# Mesoscale Assessment of CO2 Storage Potential and Geological Suitability for Target Area Selection in the Sichuan Basin

Authors: Yujie Diao; Guowei Zhu; Hong Cao; Chao Zhang; Xufeng Li; Xiaolin Jin
Journal: Geofluids
 (2017)

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## Abstract

In China, south of the Yangtze River, there are a large number of carbon sources, while the Sichuan Basin is the largest sedimentary basin; it makes sense to select the targets for CO2 geological storage (CGUS) early demonstration. For CO2 enhanced oil and gas, coal bed methane recovery (CO2-EOR, EGR, and ECBM), or storage in these depleted fields, the existing oil, gas fields, or coal seams could be the target areas in the mesoscale. This paper proposed a methodology of GIS superimposed multisource information assessment of geological suitability for CO2 enhanced water recovery (CO2-EWR) or only storage in deep saline aquifers. The potential per unit area of deep saline aquifers CO2 storage in Central Sichuan is generally greater than 50 × 104 t/km2 atP50 probability level, with Xujiahe group being the main reservoir. CO2 storage potential of depleted gas fields is 53.73 × 108 t, while it is 33.85 × 108 t by using CO2-EGR technology. This paper recommended that early implementation of CGUS could be carried out in the deep saline aquifers and depleted gas fields in the Sichuan Basin, especially that of the latter because of excellent traps, rich geological data, and well-run infrastructures.


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## Body

## 1. Introduction

The Intergovernmental Panel on Climate Change (IPCC) noted in its fifth assessment report that climate change is more serious than the original understanding, and perhaps more than 95% of it is caused by human behavior [1]. In China, south of the Yangtze River, there are a large number of carbon sources; among that about 104.58 Mt CO2 are discharged in Sichuan Province and Chongqing City mainly from cement and thermal power plants [2]. Therefore, as the largest sedimentary basins in Southern China, the Sichuan Basin covers about 20 × 104 km2, with its craton basic structure, thick marine carbonate, and clastic sedimentary strata, and has great significance in analyzing mesoscale potential and geological suitability for CO2 geological utilization and storage technologies (CGUS), including CO2 enhanced oil, gas, coal bed methane, shale gas and water recovery (CO2-EOR, EGR, ECBM, ESGR, and EWR), CO2 enhanced geothermal systems, and uranium leaching (CO2-EGS and EUL). Furthermore, CO2 geological storage technologies include depleted oil or gas fields, unmineable coal seams, and deep saline aquifers CO2 storage [3].Evaluation of CO2 storage potential is required to assess the contribution towards the reduction of CO2 emissions. The Carbon Sequestration Leadership Forum (CSLF) and US Department of Energy (USDOE) both proposed the standards and methodologies for CO2 storage capacity estimation and site selection and also the atlas [4–9], which provided the basic methodologies. Some researchers developed the methodologies or key parameters to evaluate the CO2 storage potential or site selection [10, 11], and Goodman et al. [12] provided a detailed description of the USDOE’s methodology for CO2 storage potential evaluation. In China, Zhang et al. [13] first carried out a preliminary assessment of the national scale potential of CO2 geological storage in depleted oil and gas fields, unmineable coal seams, and deep saline aquifers. Subsequently, Liu et al. [14] and Li et al. [15] carried out evaluation of the potential of CO2 geological storage in depleted natural gas fields and deep saline aquifers, respectively. Guo et al. [16] evaluated the national scale potential of CO2 geological storage in depleted oil and gas fields, unmineable coal seams, and deep saline aquifers in 417 onshore and offshore sedimentary basins supported by China Geological Survey (CGS) and evaluated the suitability for prospective selection in the macroscale. As the CGUS methodologies are paid more and more attention, Li et al. [17] preliminary evaluated CO2 geological storage potential of CO2-EOR, EGR, and ECBM. ACCA21 [3] first evaluated the national scale potential of CGUS, and Wei et al. [18] developed the methodology of potential assessment of CO2 geological utilization and storage in the macroscale in China.From the view of spatial scale and time scale, the mesoscale corresponds to target between basin and site which needs more geological survey for CCUS demonstration or industrialization in the short term, generally before 2030 according to carbon reduction target of China. Therefore, because of the large area and complicated geology different from abroad, the methodologies and parameters of potential evaluation of CGUS should be more suitable for geology in the Sichuan Basin.


## 2. Methodology

In the mesoscale, oil and gas fields and CBM fields under production could be the target areas for CO2 geological utilization or storage. However, for deep saline aquifer CO2 geological storage or CO2-EWR, the assessment of potential and geological suitability for target area selection should follow the order of candidate prospective area to target area, because of fast changing lithology and strong heterogeneity in terrestrial sedimentary formations and also the different distribution of aquifers in lateral and vertical direction. Based on the detailed studies of reservoirs and caprocks in sedimentary basins and the basic requirements for geological safety, the candidate prospective areas in the Sichuan Basin should be selected first, and then potential and geological suitability assessment could be carried out for target area selection next.


### 2.1. Method of Assessment of CO2 Geological Utilization and Storage Potential

#### 2.1.1. Depleted Oil Fields CO2 Storage and CO2-EOR

(1) Depleted Oil Fields
C
O
2
Storage. The method of assessment of CO2 storage potential of CO2-EOR is as follows [12]:(1)GCO2=OOIPρoil·B·ρCO2·Eoil,where GCO2 is CO2 geological storage potential; OOIP is the proven original oil reserves in place of existed oil and gas fields presented by Ministry of Land and Resources of China (MLR), in accordance with the research scale in this paper; ρoil is oil density at standard atmospheric pressure; B is oil volume factor; ρCO2 is CO2 density at reservoir temperature and pressure conditions (according to Berndt Wischnewski formula); Eoil is storage efficiency (or effective coefficient), recommend as 75% by Li et al. [17] based on the largest oil production rate of most depleted oil fields in China and the possible amount of CO2 could be injected.(2)
C
O
2-EOR. The method of CO2 geological storage potential assessment of CO2-EOR is as follows [19]:(2)GCO2-EOR=OOIPρoil·B·Eoil·EXTRA·PLCO2·RLCO2+PHCO2·RHCO2,(3)API=141.5Sg-131.5,where GCO2-EOR is storage potential of CO2 by using CO2-EOR technology; EXTRA is the proportion of extra recovery to OOIP (Table 1); PLCO2 is the lowest probability of oil recovery (Table 2); PHCO2 is the highest probability of oil recovery (Table 2); RLCO2 = 2.113 t/m3; RHCO2 = 3.522 t/m3; Sg is specific gravity; other parameters are the same as formula (1).Table 1
The value of EXTRA with differentAPI gravity.
EXTRA (%)
A
P
I
5.3
<31
1.3 (API—31) + 5.3
31
≤
A
P
I
≤
41
18.3
>41Table 2
Four EOR cases with different depth/pressure andAPI gravity.
Depth
A
P
I
P
L
C
O
2 (%)
P
H
C
O
2 (%)
<2000
>35
100
0
≤35
66
33
>2000
>35
33
66
≤35
0
100


#### 2.1.2. Depleted Gas Fields CO2 Storage and CO2-EGR

(1) Depleted Gas Fields
C
O
2
Storage. USDOE [12] and CSLF [5] have the same assumptions for assessments of both CO2-EGR storage potential and CO2-EOR storage potential. Therefore, the calculation formulas are basically the same:(4)GCO2=OGIPρgasstd·B·ρCO2·Egas,where OGIP is the proven original natural gas reserves in place, similar to OOIP; ρgasstd is gas density under standard atmospheric pressure; B is natural gas volume factor; Egas is storage efficiency (effective coefficient), 75% [17]; other parameters are the same as formula (1).(2)
C
O
2-EGR. Whether the feasibility of CO2-EGR technique is possible or not, we could evaluate the storage potential of CO2 using the following formula:(5)GCO2-EGR=OGIPρgasstd·B·ρCO2·Egas·C,where GCO2-EGR is CO2 geological storage potential by using CO2-EGR technology; C is reduction coefficient, compared with depleted gas storage, Li et al. recommend it as 63% [17]; other parameters are the same as formula (4).


#### 2.1.3. Unmineable Coal Seams CO2 Storage and CO2-ECBM

(1) Unmineable Coal Seams
C
O
2
Storage. The formula to calculate the storage potential is as follows: (6)GCO2=GCBM·RCO2/CH4·ρCO2std·Ecoal,where GCBM is coal bed methane reserves (there is only prospective reserves proposed by MLR, less credible than the oil and gas reserves); RCO2/CH4 is the absorption capacity ratio of CO2 and CH4 in coal seams; Ecoal is storage efficiency (effective coefficient); other parameters are the same as formula (4).The values ofRCO2/CH4 and Ecoal were proposed by USDOE (2003) and Goodman et al. [12] as shown in Tables 3 and 4.Table 3
The values ofRCO2/CH4 and C of different types of coal (USDOE, 2003).
Types of coal
R
C
O
2
/
C
H
4
C
Lignite
10
1.00
Noncaking coal
10
0.67
Weakly caking coal
10
1.00
Long flame coal
6
1.00
Gas coal
3
0.61
Fat coal
1
0.55
Coking coal
1
0.50
Lean coal
1
0.50
Meager coal
1
0.50
Anthracite
1
0.50Table 4
Storage efficiency of unmineable coal seams [12].
P
10
P
50
P
90
21%
37%
48%(2)
C
O
2-ECBM. The formula to calculate the storage potential of CO2-ECBM is as follows: (7)GCO2-ECBM=GCBM·RCO2/CH4·ρCO2std·Ecoal·C,where GCO2-ECBM is CO2 geological storage potential by using CO2-ECBM technology; C is recovery coefficient of different types of coal; other parameters are the same as formula (6).


#### 2.1.4. Deep Saline Aquifers CO2 Storage and CO2-EWR

The calculation formulas of CO2-EWR and the only geological storage in saline aquifers technology are the same as follows: (8)GCO2=A·h·φe·ρCO2·Esaline,where A is reservoir distribution area; h is reservoir thickness; φe is saline aquifer average effective porosity; Esaline is storage efficiency (effective coefficient), shown in Table 5; other parameters are defined above.Table 5
CO2 storage efficiency coefficients Esaline at regional scales [12].
Lithology
P
10
P
50
P
90
Clastics
1.2%
2.4%
4.1%
Dolomite
2.0%
2.7%
3.6%
Limestone
1.3%
2.0%
2.8%


### 2.2. Method of Suitability Assessment for Saline Aquifers Storage Target Selection

#### 2.2.1. Mathematical Model

(1) GIS Superimposed Multisource Information Assessment Technology. Superimposed multisource information assessment technology is an integrated method of processing multisource geological data. Based on the two-dimensional space determined by geographical coordinates, the unity of the geographical coordinates within the same region but with different information, that is, the so-called spatial registration, is achieved, which is performed by using geographic information software (ArcGIS or MapGIS).(2) Mathematical Model. The selected candidate prospective areas undergo the GIS spatial analysis into grids of 1000 m × 1000 m. The thematic information map prepared for each factor is screened by key veto factors. Thus, the single factor unfit to carry out CO2 geological storage is identified to abandon the unsuitable grid for deep saline aquifer CO2 storage.Then, GIS spatial analysis and evaluation are carried out using formula (9).(9)P=∑i=1nPiAii=1,2,3,…,n.Here,P is suitability scores of unit for CO2 geological storage; n is the total number of evaluation factors; Pi is given point of the factor i; Ai is index weight of the factor i.Single metric suitability rating is as follows: “good”: 9 points, “general”: 5 points, and “poor”: 1 point. The evaluation result suitability rating is as follows: “highly suitable”: value range 7 ≤P ≤ 9, “suitable”: 5 ≤P < 7, “less suitable”: 3 ≤P < 5, and “unsuitable”: 1 ≤P < 3.


#### 2.2.2. Index System for Geological Suitability Assessment

As shown in Table6, the index system for geological suitability has three hierarchies. The index weights at all levels are determined using the Analytic Hierarchy Process (AHP) [20, 21].Table 6
Index system for geological suitability assessment to select suitable targets for deep saline aquifer CO2 storage.
Level one index
Weight
Level two index
Weight
Level three index
Weight
Good
General
Poor
Key veto factor
Reservoir conditions and storage potential
0.50
Characteristic of the best reservoir
0.60
Lithology
0.07
Clastic
Mix of clastic and carbonate
Carbonate
Single layer thicknessh/m
0.11
≥80
30 ≤h < 80
10 ≤h < 30
<10
Sedimentary facies
0.36
River, delta
Turbidity, alluvial fan
Beach bar, reef
Average porosityφ/%
0.20
≥15
10 ≤φ < 15
5 ≤φ < 10
<5
Average permeabilityk/mD
0.27
≥50
10 ≤k < 50
1 ≤k < 10
<1
Storage potential
0.40
Storage potential per unit areaG (104 t/km2)
1.00
≥100
10 ≤G < 100
<10
Geological safety
0.50
Characteristic of the main caprock
0.62
Lithology
0.30
Evaporites
Argillite
Shale and dense limestone
Thicknessh/m
0.53
≥100
50 ≤h < 100
10 ≤h < 50
<10
DepthD/m
0.11
1000 ≤D ≤ 2700
<1000
>2700
Buffer caprock above the main caprock
0.06
Multiple sets
Single set
None
Hydrodynamic conditions
0.24
Hydrodynamic conditions
1.00
Groundwater high-containment area
Groundwater containment area
Groundwater semicontainment area
Groundwater open area
Seismic activity
0.14
Peak ground acceleration
0.50
<0.05 g
0.05 g, 0.10 g
0.15 g, 0.20 g, 0.30 g
≥0.40 g
Development degree of fractures
0.50
Simple
Moderate
Complex
Within 25 km of active faultsThe assessment indexes are described detailed in the following.(1) Characteristic of the Best ReservoirDepth. Only if the theoretical storage depth is more than 800 meters can CO2 enter the supercritical state, normally low than 3500 meters.Lithology. According to the existing commercial-scale CO2 geological storage projects (e.g., [22–24]), reservoir characteristics of oil and gas fields in China [25], and the engineering verification by the Shenhua CCS demonstration project in the Ordos Basin in China [26], clastic reservoirs are generally better than carbonate reservoirs.Single Layer Thickness. Because of terrestrial sedimentary facies in most formations in onshore basins of China, it is difficult to find the large thick aquifers for CO2 storage similar as Sleipner project in Norway. The minimum single layer thickness of reservoirs recommended in this paper is 10 m.Sedimentary Facies. Most Cenozoic sedimentary basins in China are terrestrial sedimentary formations. The main part of the reservoir is the deltaic sand body, followed by the turbidite sand and alluvial fan glutinite body and finally the sand beach dams and a small amount of reef.Porosity and Permeability. Low porosity and permeability is a special feature in terrestrial sedimentary oil and gas reservoirs and saline aquifers in China. Generally, for both the clastic and carbonate rock reservoirs, the porosity should be greater than or equal to 5% and permeability should be greater than or equal to 1 mD (e.g., [27–30]).(2) Characteristic of the Main CaprockLithology. The most common caprocks of oil and gas fields in China are argillite (mudstone and shale) and evaporites (gypsum and rock salt), followed by carbonate rocks (marl, argillaceous dolomite, compact limestone, and dense dolomite) and frozen genesis caps. Sometimes there are local chert layers, seams, dense volcanic rocks, and intrusive rock caps.Thickness. There are certain relationships between cap thickness and the size and height of the reservoir. With the combination of existing cap thickness grading standards [30] and considerations of the differences between CO2 and oil and gas, the reference criteria for grading the classification of CO2 geological storage cap thickness can be specified. The minimum thickness of CO2 geological storage caprocks recommended in this paper is 10 m.Burial Depth. The cap type is argillaceous rocks. The diagenesis has different effects on the performance of the caprock at different stage [31]. When the burial depth of argillaceous rocks is less than 1000 m, the diagenetic degree is poor and the sealing mainly relies on the capillary pressure. The porosity and permeability are good but with poor plasticity. At the burial depth of 1000–2700 m, the diagenesis is enhanced; mineral particles inside the argillaceous rock become more compacted; the porosity and permeability deteriorate; the plasticity increases; the capillary flow capacity declines; sealing ability improves; and there is abnormal sealing pressure. When the burial depth is greater than 2700 m, it is equivalent to the tightly compacted stage of the Argillite. The diagenesis is boosted further; the plasticity decreases and fragility increases; with the increase in the abnormal pressure, microcracks appear on the argillaceous rocks; and capillary sealing ability deteriorates.The “Buffer Cap” above the Main Caprock. When the CO2 breaks through the main cap, the “buffer cap” above the main cap has to provide a certain sealing capability to reduce or prevent the escape of CO2.(3) Geological SafetyHydrodynamic Conditions. Ye et al. [32] divided the effect of hydrogeological conditions controlling coalbed methane into three categories: hydraulic transport dissipation effect, hydraulic seal effect, and hydraulic block effect. The more closed the hydrogeological conditions are, the more favorable they are for CO2 geological storage. Basin lots with complex geological structure and powerful water alternating are not suitable CO2 geological storage candidate prospective areas due to the high degree of hydrogeology and strong groundwater activities.Peak Ground Acceleration. The GB 18306-2001 “The Peak Ground Acceleration Zoning in China” shows the Chinese seismic zonation map, its technical elements, and user provisions. It also applies to the CO2 geological storage construction project. The greater the peak ground acceleration is, the more unfavorable it is for CO2 geological storage. In general, the peak ground acceleration should be less than 0.40 g. Besides, active faults are not only CO2 leakage pathways but also cause damage to the strata continuity, resulting in CO2 leakage through the caprock. According to the GB 17741-2005 “Project site seismic safety evaluation” [33], the identification of the capable fault has to be made within a 5 km range of the first class venues and epitaxy. For seismic safety evaluation, the near-field region should be extended to a radius of 25 km range. Therefore, areas within 25 km of the active faults are inappropriate as the candidate prospective areas.Development Degree of Fractures. CO2 could leak by tectonic pathways including faults, fractures, and ground fissures (e.g., [28, 34–36]). Due to the complexity of geological structure and faults development in the Sichuan Basin, the qualitative assessment is based on the faults development and the existing seismic data. The more complex the fault system is, the more unfavorable it is for CO2 geological storage. In addition, there have been more frequent seismic activities in the Sichuan Basin in recent years.(4) Storage Potential per Unit Area. Guo (2014) evaluated the national scale potential of CO2 geological storage in deep saline aquifers of 390 onshore basins in China supported by China Geological Survey. As shown in Figure 1, the potential of CO2 geological storage in deep saline aquifers in most of the sedimentary basins is 50 × 104–100 × 104 t generally, and a small part of the basins are less than 10 × 104 t or more than 100 × 104 t.Figure 1
The statistical profile of CO2 geological storage potential per square kilometer of 390 onshore basins in China.


## 2.1. Method of Assessment of CO2 Geological Utilization and Storage Potential

### 2.1.1. Depleted Oil Fields CO2 Storage and CO2-EOR

(1) Depleted Oil Fields
C
O
2
Storage. The method of assessment of CO2 storage potential of CO2-EOR is as follows [12]:(1)GCO2=OOIPρoil·B·ρCO2·Eoil,where GCO2 is CO2 geological storage potential; OOIP is the proven original oil reserves in place of existed oil and gas fields presented by Ministry of Land and Resources of China (MLR), in accordance with the research scale in this paper; ρoil is oil density at standard atmospheric pressure; B is oil volume factor; ρCO2 is CO2 density at reservoir temperature and pressure conditions (according to Berndt Wischnewski formula); Eoil is storage efficiency (or effective coefficient), recommend as 75% by Li et al. [17] based on the largest oil production rate of most depleted oil fields in China and the possible amount of CO2 could be injected.(2)
C
O
2-EOR. The method of CO2 geological storage potential assessment of CO2-EOR is as follows [19]:(2)GCO2-EOR=OOIPρoil·B·Eoil·EXTRA·PLCO2·RLCO2+PHCO2·RHCO2,(3)API=141.5Sg-131.5,where GCO2-EOR is storage potential of CO2 by using CO2-EOR technology; EXTRA is the proportion of extra recovery to OOIP (Table 1); PLCO2 is the lowest probability of oil recovery (Table 2); PHCO2 is the highest probability of oil recovery (Table 2); RLCO2 = 2.113 t/m3; RHCO2 = 3.522 t/m3; Sg is specific gravity; other parameters are the same as formula (1).Table 1
The value of EXTRA with differentAPI gravity.
EXTRA (%)
A
P
I
5.3
<31
1.3 (API—31) + 5.3
31
≤
A
P
I
≤
41
18.3
>41Table 2
Four EOR cases with different depth/pressure andAPI gravity.
Depth
A
P
I
P
L
C
O
2 (%)
P
H
C
O
2 (%)
<2000
>35
100
0
≤35
66
33
>2000
>35
33
66
≤35
0
100


### 2.1.2. Depleted Gas Fields CO2 Storage and CO2-EGR

(1) Depleted Gas Fields
C
O
2
Storage. USDOE [12] and CSLF [5] have the same assumptions for assessments of both CO2-EGR storage potential and CO2-EOR storage potential. Therefore, the calculation formulas are basically the same:(4)GCO2=OGIPρgasstd·B·ρCO2·Egas,where OGIP is the proven original natural gas reserves in place, similar to OOIP; ρgasstd is gas density under standard atmospheric pressure; B is natural gas volume factor; Egas is storage efficiency (effective coefficient), 75% [17]; other parameters are the same as formula (1).(2)
C
O
2-EGR. Whether the feasibility of CO2-EGR technique is possible or not, we could evaluate the storage potential of CO2 using the following formula:(5)GCO2-EGR=OGIPρgasstd·B·ρCO2·Egas·C,where GCO2-EGR is CO2 geological storage potential by using CO2-EGR technology; C is reduction coefficient, compared with depleted gas storage, Li et al. recommend it as 63% [17]; other parameters are the same as formula (4).


### 2.1.3. Unmineable Coal Seams CO2 Storage and CO2-ECBM

(1) Unmineable Coal Seams
C
O
2
Storage. The formula to calculate the storage potential is as follows: (6)GCO2=GCBM·RCO2/CH4·ρCO2std·Ecoal,where GCBM is coal bed methane reserves (there is only prospective reserves proposed by MLR, less credible than the oil and gas reserves); RCO2/CH4 is the absorption capacity ratio of CO2 and CH4 in coal seams; Ecoal is storage efficiency (effective coefficient); other parameters are the same as formula (4).The values ofRCO2/CH4 and Ecoal were proposed by USDOE (2003) and Goodman et al. [12] as shown in Tables 3 and 4.Table 3
The values ofRCO2/CH4 and C of different types of coal (USDOE, 2003).
Types of coal
R
C
O
2
/
C
H
4
C
Lignite
10
1.00
Noncaking coal
10
0.67
Weakly caking coal
10
1.00
Long flame coal
6
1.00
Gas coal
3
0.61
Fat coal
1
0.55
Coking coal
1
0.50
Lean coal
1
0.50
Meager coal
1
0.50
Anthracite
1
0.50Table 4
Storage efficiency of unmineable coal seams [12].
P
10
P
50
P
90
21%
37%
48%(2)
C
O
2-ECBM. The formula to calculate the storage potential of CO2-ECBM is as follows: (7)GCO2-ECBM=GCBM·RCO2/CH4·ρCO2std·Ecoal·C,where GCO2-ECBM is CO2 geological storage potential by using CO2-ECBM technology; C is recovery coefficient of different types of coal; other parameters are the same as formula (6).


### 2.1.4. Deep Saline Aquifers CO2 Storage and CO2-EWR

The calculation formulas of CO2-EWR and the only geological storage in saline aquifers technology are the same as follows: (8)GCO2=A·h·φe·ρCO2·Esaline,where A is reservoir distribution area; h is reservoir thickness; φe is saline aquifer average effective porosity; Esaline is storage efficiency (effective coefficient), shown in Table 5; other parameters are defined above.Table 5
CO2 storage efficiency coefficients Esaline at regional scales [12].
Lithology
P
10
P
50
P
90
Clastics
1.2%
2.4%
4.1%
Dolomite
2.0%
2.7%
3.6%
Limestone
1.3%
2.0%
2.8%


## 2.1.1. Depleted Oil Fields CO2 Storage and CO2-EOR

(1) Depleted Oil Fields
C
O
2
Storage. The method of assessment of CO2 storage potential of CO2-EOR is as follows [12]:(1)GCO2=OOIPρoil·B·ρCO2·Eoil,where GCO2 is CO2 geological storage potential; OOIP is the proven original oil reserves in place of existed oil and gas fields presented by Ministry of Land and Resources of China (MLR), in accordance with the research scale in this paper; ρoil is oil density at standard atmospheric pressure; B is oil volume factor; ρCO2 is CO2 density at reservoir temperature and pressure conditions (according to Berndt Wischnewski formula); Eoil is storage efficiency (or effective coefficient), recommend as 75% by Li et al. [17] based on the largest oil production rate of most depleted oil fields in China and the possible amount of CO2 could be injected.(2)
C
O
2-EOR. The method of CO2 geological storage potential assessment of CO2-EOR is as follows [19]:(2)GCO2-EOR=OOIPρoil·B·Eoil·EXTRA·PLCO2·RLCO2+PHCO2·RHCO2,(3)API=141.5Sg-131.5,where GCO2-EOR is storage potential of CO2 by using CO2-EOR technology; EXTRA is the proportion of extra recovery to OOIP (Table 1); PLCO2 is the lowest probability of oil recovery (Table 2); PHCO2 is the highest probability of oil recovery (Table 2); RLCO2 = 2.113 t/m3; RHCO2 = 3.522 t/m3; Sg is specific gravity; other parameters are the same as formula (1).Table 1
The value of EXTRA with differentAPI gravity.
EXTRA (%)
A
P
I
5.3
<31
1.3 (API—31) + 5.3
31
≤
A
P
I
≤
41
18.3
>41Table 2
Four EOR cases with different depth/pressure andAPI gravity.
Depth
A
P
I
P
L
C
O
2 (%)
P
H
C
O
2 (%)
<2000
>35
100
0
≤35
66
33
>2000
>35
33
66
≤35
0
100


## 2.1.2. Depleted Gas Fields CO2 Storage and CO2-EGR

(1) Depleted Gas Fields
C
O
2
Storage. USDOE [12] and CSLF [5] have the same assumptions for assessments of both CO2-EGR storage potential and CO2-EOR storage potential. Therefore, the calculation formulas are basically the same:(4)GCO2=OGIPρgasstd·B·ρCO2·Egas,where OGIP is the proven original natural gas reserves in place, similar to OOIP; ρgasstd is gas density under standard atmospheric pressure; B is natural gas volume factor; Egas is storage efficiency (effective coefficient), 75% [17]; other parameters are the same as formula (1).(2)
C
O
2-EGR. Whether the feasibility of CO2-EGR technique is possible or not, we could evaluate the storage potential of CO2 using the following formula:(5)GCO2-EGR=OGIPρgasstd·B·ρCO2·Egas·C,where GCO2-EGR is CO2 geological storage potential by using CO2-EGR technology; C is reduction coefficient, compared with depleted gas storage, Li et al. recommend it as 63% [17]; other parameters are the same as formula (4).


## 2.1.3. Unmineable Coal Seams CO2 Storage and CO2-ECBM

(1) Unmineable Coal Seams
C
O
2
Storage. The formula to calculate the storage potential is as follows: (6)GCO2=GCBM·RCO2/CH4·ρCO2std·Ecoal,where GCBM is coal bed methane reserves (there is only prospective reserves proposed by MLR, less credible than the oil and gas reserves); RCO2/CH4 is the absorption capacity ratio of CO2 and CH4 in coal seams; Ecoal is storage efficiency (effective coefficient); other parameters are the same as formula (4).The values ofRCO2/CH4 and Ecoal were proposed by USDOE (2003) and Goodman et al. [12] as shown in Tables 3 and 4.Table 3
The values ofRCO2/CH4 and C of different types of coal (USDOE, 2003).
Types of coal
R
C
O
2
/
C
H
4
C
Lignite
10
1.00
Noncaking coal
10
0.67
Weakly caking coal
10
1.00
Long flame coal
6
1.00
Gas coal
3
0.61
Fat coal
1
0.55
Coking coal
1
0.50
Lean coal
1
0.50
Meager coal
1
0.50
Anthracite
1
0.50Table 4
Storage efficiency of unmineable coal seams [12].
P
10
P
50
P
90
21%
37%
48%(2)
C
O
2-ECBM. The formula to calculate the storage potential of CO2-ECBM is as follows: (7)GCO2-ECBM=GCBM·RCO2/CH4·ρCO2std·Ecoal·C,where GCO2-ECBM is CO2 geological storage potential by using CO2-ECBM technology; C is recovery coefficient of different types of coal; other parameters are the same as formula (6).


## 2.1.4. Deep Saline Aquifers CO2 Storage and CO2-EWR

The calculation formulas of CO2-EWR and the only geological storage in saline aquifers technology are the same as follows: (8)GCO2=A·h·φe·ρCO2·Esaline,where A is reservoir distribution area; h is reservoir thickness; φe is saline aquifer average effective porosity; Esaline is storage efficiency (effective coefficient), shown in Table 5; other parameters are defined above.Table 5
CO2 storage efficiency coefficients Esaline at regional scales [12].
Lithology
P
10
P
50
P
90
Clastics
1.2%
2.4%
4.1%
Dolomite
2.0%
2.7%
3.6%
Limestone
1.3%
2.0%
2.8%


## 2.2. Method of Suitability Assessment for Saline Aquifers Storage Target Selection

### 2.2.1. Mathematical Model

(1) GIS Superimposed Multisource Information Assessment Technology. Superimposed multisource information assessment technology is an integrated method of processing multisource geological data. Based on the two-dimensional space determined by geographical coordinates, the unity of the geographical coordinates within the same region but with different information, that is, the so-called spatial registration, is achieved, which is performed by using geographic information software (ArcGIS or MapGIS).(2) Mathematical Model. The selected candidate prospective areas undergo the GIS spatial analysis into grids of 1000 m × 1000 m. The thematic information map prepared for each factor is screened by key veto factors. Thus, the single factor unfit to carry out CO2 geological storage is identified to abandon the unsuitable grid for deep saline aquifer CO2 storage.Then, GIS spatial analysis and evaluation are carried out using formula (9).(9)P=∑i=1nPiAii=1,2,3,…,n.Here,P is suitability scores of unit for CO2 geological storage; n is the total number of evaluation factors; Pi is given point of the factor i; Ai is index weight of the factor i.Single metric suitability rating is as follows: “good”: 9 points, “general”: 5 points, and “poor”: 1 point. The evaluation result suitability rating is as follows: “highly suitable”: value range 7 ≤P ≤ 9, “suitable”: 5 ≤P < 7, “less suitable”: 3 ≤P < 5, and “unsuitable”: 1 ≤P < 3.


### 2.2.2. Index System for Geological Suitability Assessment

As shown in Table6, the index system for geological suitability has three hierarchies. The index weights at all levels are determined using the Analytic Hierarchy Process (AHP) [20, 21].Table 6
Index system for geological suitability assessment to select suitable targets for deep saline aquifer CO2 storage.
Level one index
Weight
Level two index
Weight
Level three index
Weight
Good
General
Poor
Key veto factor
Reservoir conditions and storage potential
0.50
Characteristic of the best reservoir
0.60
Lithology
0.07
Clastic
Mix of clastic and carbonate
Carbonate
Single layer thicknessh/m
0.11
≥80
30 ≤h < 80
10 ≤h < 30
<10
Sedimentary facies
0.36
River, delta
Turbidity, alluvial fan
Beach bar, reef
Average porosityφ/%
0.20
≥15
10 ≤φ < 15
5 ≤φ < 10
<5
Average permeabilityk/mD
0.27
≥50
10 ≤k < 50
1 ≤k < 10
<1
Storage potential
0.40
Storage potential per unit areaG (104 t/km2)
1.00
≥100
10 ≤G < 100
<10
Geological safety
0.50
Characteristic of the main caprock
0.62
Lithology
0.30
Evaporites
Argillite
Shale and dense limestone
Thicknessh/m
0.53
≥100
50 ≤h < 100
10 ≤h < 50
<10
DepthD/m
0.11
1000 ≤D ≤ 2700
<1000
>2700
Buffer caprock above the main caprock
0.06
Multiple sets
Single set
None
Hydrodynamic conditions
0.24
Hydrodynamic conditions
1.00
Groundwater high-containment area
Groundwater containment area
Groundwater semicontainment area
Groundwater open area
Seismic activity
0.14
Peak ground acceleration
0.50
<0.05 g
0.05 g, 0.10 g
0.15 g, 0.20 g, 0.30 g
≥0.40 g
Development degree of fractures
0.50
Simple
Moderate
Complex
Within 25 km of active faultsThe assessment indexes are described detailed in the following.(1) Characteristic of the Best ReservoirDepth. Only if the theoretical storage depth is more than 800 meters can CO2 enter the supercritical state, normally low than 3500 meters.Lithology. According to the existing commercial-scale CO2 geological storage projects (e.g., [22–24]), reservoir characteristics of oil and gas fields in China [25], and the engineering verification by the Shenhua CCS demonstration project in the Ordos Basin in China [26], clastic reservoirs are generally better than carbonate reservoirs.Single Layer Thickness. Because of terrestrial sedimentary facies in most formations in onshore basins of China, it is difficult to find the large thick aquifers for CO2 storage similar as Sleipner project in Norway. The minimum single layer thickness of reservoirs recommended in this paper is 10 m.Sedimentary Facies. Most Cenozoic sedimentary basins in China are terrestrial sedimentary formations. The main part of the reservoir is the deltaic sand body, followed by the turbidite sand and alluvial fan glutinite body and finally the sand beach dams and a small amount of reef.Porosity and Permeability. Low porosity and permeability is a special feature in terrestrial sedimentary oil and gas reservoirs and saline aquifers in China. Generally, for both the clastic and carbonate rock reservoirs, the porosity should be greater than or equal to 5% and permeability should be greater than or equal to 1 mD (e.g., [27–30]).(2) Characteristic of the Main CaprockLithology. The most common caprocks of oil and gas fields in China are argillite (mudstone and shale) and evaporites (gypsum and rock salt), followed by carbonate rocks (marl, argillaceous dolomite, compact limestone, and dense dolomite) and frozen genesis caps. Sometimes there are local chert layers, seams, dense volcanic rocks, and intrusive rock caps.Thickness. There are certain relationships between cap thickness and the size and height of the reservoir. With the combination of existing cap thickness grading standards [30] and considerations of the differences between CO2 and oil and gas, the reference criteria for grading the classification of CO2 geological storage cap thickness can be specified. The minimum thickness of CO2 geological storage caprocks recommended in this paper is 10 m.Burial Depth. The cap type is argillaceous rocks. The diagenesis has different effects on the performance of the caprock at different stage [31]. When the burial depth of argillaceous rocks is less than 1000 m, the diagenetic degree is poor and the sealing mainly relies on the capillary pressure. The porosity and permeability are good but with poor plasticity. At the burial depth of 1000–2700 m, the diagenesis is enhanced; mineral particles inside the argillaceous rock become more compacted; the porosity and permeability deteriorate; the plasticity increases; the capillary flow capacity declines; sealing ability improves; and there is abnormal sealing pressure. When the burial depth is greater than 2700 m, it is equivalent to the tightly compacted stage of the Argillite. The diagenesis is boosted further; the plasticity decreases and fragility increases; with the increase in the abnormal pressure, microcracks appear on the argillaceous rocks; and capillary sealing ability deteriorates.The “Buffer Cap” above the Main Caprock. When the CO2 breaks through the main cap, the “buffer cap” above the main cap has to provide a certain sealing capability to reduce or prevent the escape of CO2.(3) Geological SafetyHydrodynamic Conditions. Ye et al. [32] divided the effect of hydrogeological conditions controlling coalbed methane into three categories: hydraulic transport dissipation effect, hydraulic seal effect, and hydraulic block effect. The more closed the hydrogeological conditions are, the more favorable they are for CO2 geological storage. Basin lots with complex geological structure and powerful water alternating are not suitable CO2 geological storage candidate prospective areas due to the high degree of hydrogeology and strong groundwater activities.Peak Ground Acceleration. The GB 18306-2001 “The Peak Ground Acceleration Zoning in China” shows the Chinese seismic zonation map, its technical elements, and user provisions. It also applies to the CO2 geological storage construction project. The greater the peak ground acceleration is, the more unfavorable it is for CO2 geological storage. In general, the peak ground acceleration should be less than 0.40 g. Besides, active faults are not only CO2 leakage pathways but also cause damage to the strata continuity, resulting in CO2 leakage through the caprock. According to the GB 17741-2005 “Project site seismic safety evaluation” [33], the identification of the capable fault has to be made within a 5 km range of the first class venues and epitaxy. For seismic safety evaluation, the near-field region should be extended to a radius of 25 km range. Therefore, areas within 25 km of the active faults are inappropriate as the candidate prospective areas.Development Degree of Fractures. CO2 could leak by tectonic pathways including faults, fractures, and ground fissures (e.g., [28, 34–36]). Due to the complexity of geological structure and faults development in the Sichuan Basin, the qualitative assessment is based on the faults development and the existing seismic data. The more complex the fault system is, the more unfavorable it is for CO2 geological storage. In addition, there have been more frequent seismic activities in the Sichuan Basin in recent years.(4) Storage Potential per Unit Area. Guo (2014) evaluated the national scale potential of CO2 geological storage in deep saline aquifers of 390 onshore basins in China supported by China Geological Survey. As shown in Figure 1, the potential of CO2 geological storage in deep saline aquifers in most of the sedimentary basins is 50 × 104–100 × 104 t generally, and a small part of the basins are less than 10 × 104 t or more than 100 × 104 t.Figure 1
The statistical profile of CO2 geological storage potential per square kilometer of 390 onshore basins in China.


## 2.2.1. Mathematical Model

(1) GIS Superimposed Multisource Information Assessment Technology. Superimposed multisource information assessment technology is an integrated method of processing multisource geological data. Based on the two-dimensional space determined by geographical coordinates, the unity of the geographical coordinates within the same region but with different information, that is, the so-called spatial registration, is achieved, which is performed by using geographic information software (ArcGIS or MapGIS).(2) Mathematical Model. The selected candidate prospective areas undergo the GIS spatial analysis into grids of 1000 m × 1000 m. The thematic information map prepared for each factor is screened by key veto factors. Thus, the single factor unfit to carry out CO2 geological storage is identified to abandon the unsuitable grid for deep saline aquifer CO2 storage.Then, GIS spatial analysis and evaluation are carried out using formula (9).(9)P=∑i=1nPiAii=1,2,3,…,n.Here,P is suitability scores of unit for CO2 geological storage; n is the total number of evaluation factors; Pi is given point of the factor i; Ai is index weight of the factor i.Single metric suitability rating is as follows: “good”: 9 points, “general”: 5 points, and “poor”: 1 point. The evaluation result suitability rating is as follows: “highly suitable”: value range 7 ≤P ≤ 9, “suitable”: 5 ≤P < 7, “less suitable”: 3 ≤P < 5, and “unsuitable”: 1 ≤P < 3.


## 2.2.2. Index System for Geological Suitability Assessment

As shown in Table6, the index system for geological suitability has three hierarchies. The index weights at all levels are determined using the Analytic Hierarchy Process (AHP) [20, 21].Table 6
Index system for geological suitability assessment to select suitable targets for deep saline aquifer CO2 storage.
Level one index
Weight
Level two index
Weight
Level three index
Weight
Good
General
Poor
Key veto factor
Reservoir conditions and storage potential
0.50
Characteristic of the best reservoir
0.60
Lithology
0.07
Clastic
Mix of clastic and carbonate
Carbonate
Single layer thicknessh/m
0.11
≥80
30 ≤h < 80
10 ≤h < 30
<10
Sedimentary facies
0.36
River, delta
Turbidity, alluvial fan
Beach bar, reef
Average porosityφ/%
0.20
≥15
10 ≤φ < 15
5 ≤φ < 10
<5
Average permeabilityk/mD
0.27
≥50
10 ≤k < 50
1 ≤k < 10
<1
Storage potential
0.40
Storage potential per unit areaG (104 t/km2)
1.00
≥100
10 ≤G < 100
<10
Geological safety
0.50
Characteristic of the main caprock
0.62
Lithology
0.30
Evaporites
Argillite
Shale and dense limestone
Thicknessh/m
0.53
≥100
50 ≤h < 100
10 ≤h < 50
<10
DepthD/m
0.11
1000 ≤D ≤ 2700
<1000
>2700
Buffer caprock above the main caprock
0.06
Multiple sets
Single set
None
Hydrodynamic conditions
0.24
Hydrodynamic conditions
1.00
Groundwater high-containment area
Groundwater containment area
Groundwater semicontainment area
Groundwater open area
Seismic activity
0.14
Peak ground acceleration
0.50
<0.05 g
0.05 g, 0.10 g
0.15 g, 0.20 g, 0.30 g
≥0.40 g
Development degree of fractures
0.50
Simple
Moderate
Complex
Within 25 km of active faultsThe assessment indexes are described detailed in the following.(1) Characteristic of the Best ReservoirDepth. Only if the theoretical storage depth is more than 800 meters can CO2 enter the supercritical state, normally low than 3500 meters.Lithology. According to the existing commercial-scale CO2 geological storage projects (e.g., [22–24]), reservoir characteristics of oil and gas fields in China [25], and the engineering verification by the Shenhua CCS demonstration project in the Ordos Basin in China [26], clastic reservoirs are generally better than carbonate reservoirs.Single Layer Thickness. Because of terrestrial sedimentary facies in most formations in onshore basins of China, it is difficult to find the large thick aquifers for CO2 storage similar as Sleipner project in Norway. The minimum single layer thickness of reservoirs recommended in this paper is 10 m.Sedimentary Facies. Most Cenozoic sedimentary basins in China are terrestrial sedimentary formations. The main part of the reservoir is the deltaic sand body, followed by the turbidite sand and alluvial fan glutinite body and finally the sand beach dams and a small amount of reef.Porosity and Permeability. Low porosity and permeability is a special feature in terrestrial sedimentary oil and gas reservoirs and saline aquifers in China. Generally, for both the clastic and carbonate rock reservoirs, the porosity should be greater than or equal to 5% and permeability should be greater than or equal to 1 mD (e.g., [27–30]).(2) Characteristic of the Main CaprockLithology. The most common caprocks of oil and gas fields in China are argillite (mudstone and shale) and evaporites (gypsum and rock salt), followed by carbonate rocks (marl, argillaceous dolomite, compact limestone, and dense dolomite) and frozen genesis caps. Sometimes there are local chert layers, seams, dense volcanic rocks, and intrusive rock caps.Thickness. There are certain relationships between cap thickness and the size and height of the reservoir. With the combination of existing cap thickness grading standards [30] and considerations of the differences between CO2 and oil and gas, the reference criteria for grading the classification of CO2 geological storage cap thickness can be specified. The minimum thickness of CO2 geological storage caprocks recommended in this paper is 10 m.Burial Depth. The cap type is argillaceous rocks. The diagenesis has different effects on the performance of the caprock at different stage [31]. When the burial depth of argillaceous rocks is less than 1000 m, the diagenetic degree is poor and the sealing mainly relies on the capillary pressure. The porosity and permeability are good but with poor plasticity. At the burial depth of 1000–2700 m, the diagenesis is enhanced; mineral particles inside the argillaceous rock become more compacted; the porosity and permeability deteriorate; the plasticity increases; the capillary flow capacity declines; sealing ability improves; and there is abnormal sealing pressure. When the burial depth is greater than 2700 m, it is equivalent to the tightly compacted stage of the Argillite. The diagenesis is boosted further; the plasticity decreases and fragility increases; with the increase in the abnormal pressure, microcracks appear on the argillaceous rocks; and capillary sealing ability deteriorates.The “Buffer Cap” above the Main Caprock. When the CO2 breaks through the main cap, the “buffer cap” above the main cap has to provide a certain sealing capability to reduce or prevent the escape of CO2.(3) Geological SafetyHydrodynamic Conditions. Ye et al. [32] divided the effect of hydrogeological conditions controlling coalbed methane into three categories: hydraulic transport dissipation effect, hydraulic seal effect, and hydraulic block effect. The more closed the hydrogeological conditions are, the more favorable they are for CO2 geological storage. Basin lots with complex geological structure and powerful water alternating are not suitable CO2 geological storage candidate prospective areas due to the high degree of hydrogeology and strong groundwater activities.Peak Ground Acceleration. The GB 18306-2001 “The Peak Ground Acceleration Zoning in China” shows the Chinese seismic zonation map, its technical elements, and user provisions. It also applies to the CO2 geological storage construction project. The greater the peak ground acceleration is, the more unfavorable it is for CO2 geological storage. In general, the peak ground acceleration should be less than 0.40 g. Besides, active faults are not only CO2 leakage pathways but also cause damage to the strata continuity, resulting in CO2 leakage through the caprock. According to the GB 17741-2005 “Project site seismic safety evaluation” [33], the identification of the capable fault has to be made within a 5 km range of the first class venues and epitaxy. For seismic safety evaluation, the near-field region should be extended to a radius of 25 km range. Therefore, areas within 25 km of the active faults are inappropriate as the candidate prospective areas.Development Degree of Fractures. CO2 could leak by tectonic pathways including faults, fractures, and ground fissures (e.g., [28, 34–36]). Due to the complexity of geological structure and faults development in the Sichuan Basin, the qualitative assessment is based on the faults development and the existing seismic data. The more complex the fault system is, the more unfavorable it is for CO2 geological storage. In addition, there have been more frequent seismic activities in the Sichuan Basin in recent years.(4) Storage Potential per Unit Area. Guo (2014) evaluated the national scale potential of CO2 geological storage in deep saline aquifers of 390 onshore basins in China supported by China Geological Survey. As shown in Figure 1, the potential of CO2 geological storage in deep saline aquifers in most of the sedimentary basins is 50 × 104–100 × 104 t generally, and a small part of the basins are less than 10 × 104 t or more than 100 × 104 t.Figure 1
The statistical profile of CO2 geological storage potential per square kilometer of 390 onshore basins in China.


## 3. Candidate Prospective Areas for CO2 Geological Utilization and Storage

The fine forming conditions of the reservoir mediums for oil, gas, and CBM make them possible that the existing oil and gas fields under production are the mesoscale candidate prospective areas or target areas in the short future. Because of no official basin-scale data available, the CO2 storage potential of other CO2 geological utilization technologies is not discussed further in this paper.


### 3.1. Geology

#### 3.1.1. Geostructure

As shown in Figure2 [37], the current geostructure of the Sichuan Basin consists of the Southeast Sichuan fold belt, Central Sichuan low uplift, and Northwest Sichuan depression.Figure 2
Sichuan Basin geological structure unit zoning map. There are three first-order tectonic units in the Sichuan Basin, that is, the Southeast Sichuan fold belt, the Central Sichuan low uplift, and the Northwest Sichuan depression. The Southeast Sichuan fold belt consists of the high steep fold belt in Eastern Sichuan (I1) and the low steep bottom fold belt in Southern Sichuan (I2); the Central Sichuan low uplift is composed of the flat fold belt in Central Sichuan (II1) and the low steep fold belt in Southwestern Sichuan (II2); the Northwest Sichuan depression consists of the low-lying fold belt in Northern Sichuan (III1) and the low steep fold belt in Western Sichuan (III2).


#### 3.1.2. Stratigraphy

The Sichuan Basin sedimentary strata are complete, with a total thickness of 6000–12000 m. Only the Permian and the younger strata are considered in this paper, as follows from old to new:(1)
The Permian: Liangshan group (P1l), Qixia group (P2q), Maokou group (P2m), Longtan group (P3l), and Changxing group (P3c).(2)
The Triassic: Feixianguan group (T1f), Jialing Group (T1j), Leikoupo group (T2l), Tianjingshan group (T2t), Ma’antang group (T3m), Xiaotangzi group (T3t), and Xujiahe group.(3)
The Jurassic: Ziliujing group (J1z), Qianfoya group (J2q), Shaximiao group (J2s), Suining group (J3s), and Penglaizhen group (J3p).(4)
The Cretaceous (K) and the Quaternary (Q).


#### 3.1.3. Hydrodynamic Condition

The Sichuan Basin is essentially an artesian basin dominated by Permian and Triassic strata. The upper Jurassic and Cretaceous formations are mostly a large set of terrestrial clastic sedimentary rocks with red sandstones and mudstones throughout the basin. They are extremely thick with poor permeability, generally low in moisture, but exceedingly uneven, which could be good caprocks for the reservoirs below them. The lower upper Triassic Xujiahe consists of sandstones and shale, and the sandstone may be good aquifers for CO2 geological storage due to its huge thickness. The lower and middle Triassic and Permian carbonate rocks are the main saline aquifers, in which Triassic carbonate rocks often form alternate layers with evaporites. Therefore, an aqueous rock series based on many stacked white aquifers is formed in the Sichuan Basin (Figure 3).Figure 3
Hydrodynamic conditions in the Sichuan Basin. The groundwater activities are very strong in the peripheral target exposure area. In contrast, the groundwater activities inside the basin are relatively weak, with better hydrogeological confinement. On the edge of the mountain around the Sichuan Basin and the eastern fold belt experiencing infiltration of fresh water due to the complex structure and strong water alternating.


#### 3.1.4. Geological Safety

There are many late Quaternary active faults on the boundary of the Sichuan Basin; for example, the Longmenshan fault zone in Northwestern Sichuan has experienced more intense activity in recent years. It is the induced fracture of the “5.12” Wenchuan 8.0 earthquake. The Lushan 7.0 earthquake on April 20, 2013, is another devastating earthquake that followed the Wenchuan 8.0 earthquake nearly five years later. It is also closely linked with the Longmenshan fault belt.However, the crust in the Central and Eastern Sichuan Basin is more stable. Historical earthquakes with magnitude above 6 mainly took place in Western Sichuan and Southwestern Sichuan Basin. And the peak ground acceleration zoning according to the GB 18306-2001 “The Peak Ground Acceleration Zoning in China” is shown in Figure4.Figure 4
Seismic peak ground acceleration and large historical earthquakes in the Sichuan Basin. The peak ground acceleration is less than 0.10 g in most parts of the Sichuan Basin. Only in the western margin of the Sichuan Basin, the peak ground acceleration is larger than 0.15 g.


### 3.2. Oil and Gas Fields

The Sichuan Basin has abundant natural gas resources, mainly in Eastern Sichuan, but a relatively small amount of oil resources. The petroleum geological reserves in the Sichuan Basin amount to 4.38 × 108 t, and only 0.75 × 108 t of proven OOIP in Central and Northern Sichuan flat structure area [38].By the end of 2008, the Ministry of Land and Resources of China (MLR) announced 125 gas fields in the Sichuan Basin (Figure1), and the total amount of proven OGIP is 17225.02 × 108 m3. Among them, there are 27 medium to large-sized confirmed gas fields with OGIP exceeding 100 × 108 m3, of which the total natural gas reserves are 15092.68 × 108 m3, accounting for 87.6% of the total proven OGIP in the basin (Table 7).Table 7
Proven OGIP of 27 natural gas fields in the Sichuan Basin.
Gas fields
OGIP/108 m3
Puguang
4050.79
Guang’an
1355.58
Hecuan
1187.06
Datianchi
1067.55
Xinchang
843.02
Luojiazhai
797.36
Moxi
702.31
Wolonghe
408.86
Weiyuan
408.61
Tieshanpo
373.97
Dukouhe
359
Bajiaochang
351.07
Luodai
323.83
Qiongxi
323.25
Qilibei
282.21
Baimamiao
268.72
Dachigan
258.71
Gaofengchang
227.26
Qilixia
225.48
Hebaochang
222.12
Tieshan
187.82
Zhongba
186.3
Majing
175.58
Xindu
175.32
Chongxi
136.35
Fuchengzhai
103.3
Jiannan
100.25


### 3.3. Unmineable Coal Seams

The CBM geological reserves in the Sichuan Basin amount to 3471.40 × 108 m3 in Sichuan province and Chongqing city, 5084.57 × 108 m3 in Southern Sichuan province and Northern Guizhou province, respectively, from 1000 to 2000 meters depth [39]. Among these, the coalfields in Southern Sichuan province are the most abundant, accounting for 82% of the province’s total resources.


### 3.4. Deep Saline Aquifers

Compared with oil fields, gas fields, and unmineable coal seams, the analysis of geological conditions for saline aquifers CO2 geological storage is much more complex. The CO2 geological storage candidate prospective area for deep saline aquifers CO2 storage was selected from the map projection on the ground of all potential underground CO2 reservoirs. In addition, the hydrodynamic and geological safety conditions must be studied to delineate the candidate prospective areas.


#### 3.4.1. Candidate Prospective Area Delineation Standards

As mentioned above, this report presents the delineation standards of the CO2 geological storage candidate prospective areas shown in Table 8. Further potential and suitability assessments can be carried out for target area selection.Table 8
Veto over key factors of CO2 geological storage candidate prospective areas delineation.
Key factors
Veto
Reservoir conditions
Layer thickness
<10 m
Porosity
<5%
Permeability
<1 mD
Hydrogeological conditions
Formation water salinity
<3 g/L
Groundwater hydrodynamic condition
Groundwater zone
Geological safety conditions
Active faults
<25 km
Peak ground acceleration
≥0.40 g


#### 3.4.2. Vertical Reservoir Cap Combination and Candidate Prospective Areas Distribution

The reservoirs for deep saline aquifer CO2 storage consist of the Permian, the lower Triassic carbonates, and upper Triassic and Jurassic clastic reservoirs (Figure 5). The reservoir space includes carbonate karst pores and cracks and clastic pores and cracks. Overall, all reservoirs in the Sichuan Basin have poor physical properties, with ultra-low porosity and low permeability. Comparing with the natural gas fields in the Sichuan Basin, these reservoirs for CO2 storage have better caprock conditions too. For example, the extensive deposits of gypsum rocks in the Leikoupo phase and the widely developed dark mudstone in the Lower Jurassic can provide good sealing conditions for the underlying reservoirs.Figure 5
CO2 geological storage vertical reservoir cap combination in the Sichuan Basin. There are nine sets of reservoirs in the Sichuan Basin, and the section four of Xujiahe group is the primary reservoir with large thickness and area, which almost cover the whole basin.(1) The Permian. The reef flat facies on the top of Qixia group form a good reservoir through dolomitization, with favorable reservoir conditions (P2q) [40]. Part of them form the natural gas reservoirs, with a thickness of approximately 10 m. Similar to the Qixia group, the Maokou group (P2m) is a fracture-cave type of reservoir. Changxing group (P3c) reservoirs are pore type and fracture-pore type. The porosity is generally 2.03%–15.85%, with an average value of 5.25%; the permeability is less than 1000 mD, with an average value of 6.05 mD. The reservoir thickness is large, with a monolayer thickness of 0.5–5 m and a single well cumulative thickness of 2.5–70 m [41].(2) The Triassic. The Feixianguan group (T1f) is similar to the Changxing group. The quality and distribution of the reef beach reservoir are mainly controlled by sedimentary facies and diagenesis. The evaporative platform oolitic dolomite reservoir is mainly distributed in Northeast Sichuan, with a monolayer thickness of 1.5–15 m and total thickness of 20–50 m. The porosity ranges from 2% to 26.8%, on the average of 8.29%; and the permeability is less than 1160 mD, with an average value of 59.73 mD. The porosity of the open platform edge oolitic dolomite reservoir is 2.05%–22.62%, on the average of 8.42%, and the permeability is less than 410 mD with an average value of 17.25 mD. The reservoir monolayer thickness is generally 0.5–6 m, and the total thickness is 10–45 m typically.The favorable Jialingjiang reservoir facies are the platform interior shoal and the platform margin shoal facies. For example, section five of Jialingjiang reservoirs consists of limestone and dolomite, with a thickness of 25–30 m, of which approximately 60% is the porosity layer, and the average of the porosity is 5%, with the highest value reaching 18%.The sandstone aquifers in section two, section four, and section six of Xujiahe formation could be reservoirs for CO2 geological storage, composed of residual intergranular pore, intergranular dissolved pore, and fracture. The sand ratio of the sandstones is greater than 70% in 80% generally. In addition, the porosity of section four is higher than section two and section six, usually between 5%–10%, while the porosity of sandstones in section two and section is less than 7% generally.Figure6 shows the candidate prospective areas in the Sichuan Basin in the Sichuan Basin for deep saline aquifer CO2 storage based on geology study.Figure 6
Candidate prospective areas in the Sichuan Basin. There are eight candidate prospective areas in the Sichuan Basin for deep saline aquifer CO2 storage which cover more than 5 × 104 km2 and mainly locate in Central Sichuan Basin (districts II–V). Only district I is in Northwestern Sichuan. The candidate prospective areas (districts VI–VIII) in Eastern Sichuan are relatively small due to the effects of formation depth, geological safety, and hydrogeological conditions.


## 3.1. Geology

### 3.1.1. Geostructure

As shown in Figure2 [37], the current geostructure of the Sichuan Basin consists of the Southeast Sichuan fold belt, Central Sichuan low uplift, and Northwest Sichuan depression.Figure 2
Sichuan Basin geological structure unit zoning map. There are three first-order tectonic units in the Sichuan Basin, that is, the Southeast Sichuan fold belt, the Central Sichuan low uplift, and the Northwest Sichuan depression. The Southeast Sichuan fold belt consists of the high steep fold belt in Eastern Sichuan (I1) and the low steep bottom fold belt in Southern Sichuan (I2); the Central Sichuan low uplift is composed of the flat fold belt in Central Sichuan (II1) and the low steep fold belt in Southwestern Sichuan (II2); the Northwest Sichuan depression consists of the low-lying fold belt in Northern Sichuan (III1) and the low steep fold belt in Western Sichuan (III2).


### 3.1.2. Stratigraphy

The Sichuan Basin sedimentary strata are complete, with a total thickness of 6000–12000 m. Only the Permian and the younger strata are considered in this paper, as follows from old to new:(1)
The Permian: Liangshan group (P1l), Qixia group (P2q), Maokou group (P2m), Longtan group (P3l), and Changxing group (P3c).(2)
The Triassic: Feixianguan group (T1f), Jialing Group (T1j), Leikoupo group (T2l), Tianjingshan group (T2t), Ma’antang group (T3m), Xiaotangzi group (T3t), and Xujiahe group.(3)
The Jurassic: Ziliujing group (J1z), Qianfoya group (J2q), Shaximiao group (J2s), Suining group (J3s), and Penglaizhen group (J3p).(4)
The Cretaceous (K) and the Quaternary (Q).


### 3.1.3. Hydrodynamic Condition

The Sichuan Basin is essentially an artesian basin dominated by Permian and Triassic strata. The upper Jurassic and Cretaceous formations are mostly a large set of terrestrial clastic sedimentary rocks with red sandstones and mudstones throughout the basin. They are extremely thick with poor permeability, generally low in moisture, but exceedingly uneven, which could be good caprocks for the reservoirs below them. The lower upper Triassic Xujiahe consists of sandstones and shale, and the sandstone may be good aquifers for CO2 geological storage due to its huge thickness. The lower and middle Triassic and Permian carbonate rocks are the main saline aquifers, in which Triassic carbonate rocks often form alternate layers with evaporites. Therefore, an aqueous rock series based on many stacked white aquifers is formed in the Sichuan Basin (Figure 3).Figure 3
Hydrodynamic conditions in the Sichuan Basin. The groundwater activities are very strong in the peripheral target exposure area. In contrast, the groundwater activities inside the basin are relatively weak, with better hydrogeological confinement. On the edge of the mountain around the Sichuan Basin and the eastern fold belt experiencing infiltration of fresh water due to the complex structure and strong water alternating.


### 3.1.4. Geological Safety

There are many late Quaternary active faults on the boundary of the Sichuan Basin; for example, the Longmenshan fault zone in Northwestern Sichuan has experienced more intense activity in recent years. It is the induced fracture of the “5.12” Wenchuan 8.0 earthquake. The Lushan 7.0 earthquake on April 20, 2013, is another devastating earthquake that followed the Wenchuan 8.0 earthquake nearly five years later. It is also closely linked with the Longmenshan fault belt.However, the crust in the Central and Eastern Sichuan Basin is more stable. Historical earthquakes with magnitude above 6 mainly took place in Western Sichuan and Southwestern Sichuan Basin. And the peak ground acceleration zoning according to the GB 18306-2001 “The Peak Ground Acceleration Zoning in China” is shown in Figure4.Figure 4
Seismic peak ground acceleration and large historical earthquakes in the Sichuan Basin. The peak ground acceleration is less than 0.10 g in most parts of the Sichuan Basin. Only in the western margin of the Sichuan Basin, the peak ground acceleration is larger than 0.15 g.


## 3.1.1. Geostructure

As shown in Figure2 [37], the current geostructure of the Sichuan Basin consists of the Southeast Sichuan fold belt, Central Sichuan low uplift, and Northwest Sichuan depression.Figure 2
Sichuan Basin geological structure unit zoning map. There are three first-order tectonic units in the Sichuan Basin, that is, the Southeast Sichuan fold belt, the Central Sichuan low uplift, and the Northwest Sichuan depression. The Southeast Sichuan fold belt consists of the high steep fold belt in Eastern Sichuan (I1) and the low steep bottom fold belt in Southern Sichuan (I2); the Central Sichuan low uplift is composed of the flat fold belt in Central Sichuan (II1) and the low steep fold belt in Southwestern Sichuan (II2); the Northwest Sichuan depression consists of the low-lying fold belt in Northern Sichuan (III1) and the low steep fold belt in Western Sichuan (III2).


## 3.1.2. Stratigraphy

The Sichuan Basin sedimentary strata are complete, with a total thickness of 6000–12000 m. Only the Permian and the younger strata are considered in this paper, as follows from old to new:(1)
The Permian: Liangshan group (P1l), Qixia group (P2q), Maokou group (P2m), Longtan group (P3l), and Changxing group (P3c).(2)
The Triassic: Feixianguan group (T1f), Jialing Group (T1j), Leikoupo group (T2l), Tianjingshan group (T2t), Ma’antang group (T3m), Xiaotangzi group (T3t), and Xujiahe group.(3)
The Jurassic: Ziliujing group (J1z), Qianfoya group (J2q), Shaximiao group (J2s), Suining group (J3s), and Penglaizhen group (J3p).(4)
The Cretaceous (K) and the Quaternary (Q).


## 3.1.3. Hydrodynamic Condition

The Sichuan Basin is essentially an artesian basin dominated by Permian and Triassic strata. The upper Jurassic and Cretaceous formations are mostly a large set of terrestrial clastic sedimentary rocks with red sandstones and mudstones throughout the basin. They are extremely thick with poor permeability, generally low in moisture, but exceedingly uneven, which could be good caprocks for the reservoirs below them. The lower upper Triassic Xujiahe consists of sandstones and shale, and the sandstone may be good aquifers for CO2 geological storage due to its huge thickness. The lower and middle Triassic and Permian carbonate rocks are the main saline aquifers, in which Triassic carbonate rocks often form alternate layers with evaporites. Therefore, an aqueous rock series based on many stacked white aquifers is formed in the Sichuan Basin (Figure 3).Figure 3
Hydrodynamic conditions in the Sichuan Basin. The groundwater activities are very strong in the peripheral target exposure area. In contrast, the groundwater activities inside the basin are relatively weak, with better hydrogeological confinement. On the edge of the mountain around the Sichuan Basin and the eastern fold belt experiencing infiltration of fresh water due to the complex structure and strong water alternating.


## 3.1.4. Geological Safety

There are many late Quaternary active faults on the boundary of the Sichuan Basin; for example, the Longmenshan fault zone in Northwestern Sichuan has experienced more intense activity in recent years. It is the induced fracture of the “5.12” Wenchuan 8.0 earthquake. The Lushan 7.0 earthquake on April 20, 2013, is another devastating earthquake that followed the Wenchuan 8.0 earthquake nearly five years later. It is also closely linked with the Longmenshan fault belt.However, the crust in the Central and Eastern Sichuan Basin is more stable. Historical earthquakes with magnitude above 6 mainly took place in Western Sichuan and Southwestern Sichuan Basin. And the peak ground acceleration zoning according to the GB 18306-2001 “The Peak Ground Acceleration Zoning in China” is shown in Figure4.Figure 4
Seismic peak ground acceleration and large historical earthquakes in the Sichuan Basin. The peak ground acceleration is less than 0.10 g in most parts of the Sichuan Basin. Only in the western margin of the Sichuan Basin, the peak ground acceleration is larger than 0.15 g.


## 3.2. Oil and Gas Fields

The Sichuan Basin has abundant natural gas resources, mainly in Eastern Sichuan, but a relatively small amount of oil resources. The petroleum geological reserves in the Sichuan Basin amount to 4.38 × 108 t, and only 0.75 × 108 t of proven OOIP in Central and Northern Sichuan flat structure area [38].By the end of 2008, the Ministry of Land and Resources of China (MLR) announced 125 gas fields in the Sichuan Basin (Figure1), and the total amount of proven OGIP is 17225.02 × 108 m3. Among them, there are 27 medium to large-sized confirmed gas fields with OGIP exceeding 100 × 108 m3, of which the total natural gas reserves are 15092.68 × 108 m3, accounting for 87.6% of the total proven OGIP in the basin (Table 7).Table 7
Proven OGIP of 27 natural gas fields in the Sichuan Basin.
Gas fields
OGIP/108 m3
Puguang
4050.79
Guang’an
1355.58
Hecuan
1187.06
Datianchi
1067.55
Xinchang
843.02
Luojiazhai
797.36
Moxi
702.31
Wolonghe
408.86
Weiyuan
408.61
Tieshanpo
373.97
Dukouhe
359
Bajiaochang
351.07
Luodai
323.83
Qiongxi
323.25
Qilibei
282.21
Baimamiao
268.72
Dachigan
258.71
Gaofengchang
227.26
Qilixia
225.48
Hebaochang
222.12
Tieshan
187.82
Zhongba
186.3
Majing
175.58
Xindu
175.32
Chongxi
136.35
Fuchengzhai
103.3
Jiannan
100.25


## 3.3. Unmineable Coal Seams

The CBM geological reserves in the Sichuan Basin amount to 3471.40 × 108 m3 in Sichuan province and Chongqing city, 5084.57 × 108 m3 in Southern Sichuan province and Northern Guizhou province, respectively, from 1000 to 2000 meters depth [39]. Among these, the coalfields in Southern Sichuan province are the most abundant, accounting for 82% of the province’s total resources.


## 3.4. Deep Saline Aquifers

Compared with oil fields, gas fields, and unmineable coal seams, the analysis of geological conditions for saline aquifers CO2 geological storage is much more complex. The CO2 geological storage candidate prospective area for deep saline aquifers CO2 storage was selected from the map projection on the ground of all potential underground CO2 reservoirs. In addition, the hydrodynamic and geological safety conditions must be studied to delineate the candidate prospective areas.


### 3.4.1. Candidate Prospective Area Delineation Standards

As mentioned above, this report presents the delineation standards of the CO2 geological storage candidate prospective areas shown in Table 8. Further potential and suitability assessments can be carried out for target area selection.Table 8
Veto over key factors of CO2 geological storage candidate prospective areas delineation.
Key factors
Veto
Reservoir conditions
Layer thickness
<10 m
Porosity
<5%
Permeability
<1 mD
Hydrogeological conditions
Formation water salinity
<3 g/L
Groundwater hydrodynamic condition
Groundwater zone
Geological safety conditions
Active faults
<25 km
Peak ground acceleration
≥0.40 g


### 3.4.2. Vertical Reservoir Cap Combination and Candidate Prospective Areas Distribution

The reservoirs for deep saline aquifer CO2 storage consist of the Permian, the lower Triassic carbonates, and upper Triassic and Jurassic clastic reservoirs (Figure 5). The reservoir space includes carbonate karst pores and cracks and clastic pores and cracks. Overall, all reservoirs in the Sichuan Basin have poor physical properties, with ultra-low porosity and low permeability. Comparing with the natural gas fields in the Sichuan Basin, these reservoirs for CO2 storage have better caprock conditions too. For example, the extensive deposits of gypsum rocks in the Leikoupo phase and the widely developed dark mudstone in the Lower Jurassic can provide good sealing conditions for the underlying reservoirs.Figure 5
CO2 geological storage vertical reservoir cap combination in the Sichuan Basin. There are nine sets of reservoirs in the Sichuan Basin, and the section four of Xujiahe group is the primary reservoir with large thickness and area, which almost cover the whole basin.(1) The Permian. The reef flat facies on the top of Qixia group form a good reservoir through dolomitization, with favorable reservoir conditions (P2q) [40]. Part of them form the natural gas reservoirs, with a thickness of approximately 10 m. Similar to the Qixia group, the Maokou group (P2m) is a fracture-cave type of reservoir. Changxing group (P3c) reservoirs are pore type and fracture-pore type. The porosity is generally 2.03%–15.85%, with an average value of 5.25%; the permeability is less than 1000 mD, with an average value of 6.05 mD. The reservoir thickness is large, with a monolayer thickness of 0.5–5 m and a single well cumulative thickness of 2.5–70 m [41].(2) The Triassic. The Feixianguan group (T1f) is similar to the Changxing group. The quality and distribution of the reef beach reservoir are mainly controlled by sedimentary facies and diagenesis. The evaporative platform oolitic dolomite reservoir is mainly distributed in Northeast Sichuan, with a monolayer thickness of 1.5–15 m and total thickness of 20–50 m. The porosity ranges from 2% to 26.8%, on the average of 8.29%; and the permeability is less than 1160 mD, with an average value of 59.73 mD. The porosity of the open platform edge oolitic dolomite reservoir is 2.05%–22.62%, on the average of 8.42%, and the permeability is less than 410 mD with an average value of 17.25 mD. The reservoir monolayer thickness is generally 0.5–6 m, and the total thickness is 10–45 m typically.The favorable Jialingjiang reservoir facies are the platform interior shoal and the platform margin shoal facies. For example, section five of Jialingjiang reservoirs consists of limestone and dolomite, with a thickness of 25–30 m, of which approximately 60% is the porosity layer, and the average of the porosity is 5%, with the highest value reaching 18%.The sandstone aquifers in section two, section four, and section six of Xujiahe formation could be reservoirs for CO2 geological storage, composed of residual intergranular pore, intergranular dissolved pore, and fracture. The sand ratio of the sandstones is greater than 70% in 80% generally. In addition, the porosity of section four is higher than section two and section six, usually between 5%–10%, while the porosity of sandstones in section two and section is less than 7% generally.Figure6 shows the candidate prospective areas in the Sichuan Basin in the Sichuan Basin for deep saline aquifer CO2 storage based on geology study.Figure 6
Candidate prospective areas in the Sichuan Basin. There are eight candidate prospective areas in the Sichuan Basin for deep saline aquifer CO2 storage which cover more than 5 × 104 km2 and mainly locate in Central Sichuan Basin (districts II–V). Only district I is in Northwestern Sichuan. The candidate prospective areas (districts VI–VIII) in Eastern Sichuan are relatively small due to the effects of formation depth, geological safety, and hydrogeological conditions.


## 3.4.1. Candidate Prospective Area Delineation Standards

As mentioned above, this report presents the delineation standards of the CO2 geological storage candidate prospective areas shown in Table 8. Further potential and suitability assessments can be carried out for target area selection.Table 8
Veto over key factors of CO2 geological storage candidate prospective areas delineation.
Key factors
Veto
Reservoir conditions
Layer thickness
<10 m
Porosity
<5%
Permeability
<1 mD
Hydrogeological conditions
Formation water salinity
<3 g/L
Groundwater hydrodynamic condition
Groundwater zone
Geological safety conditions
Active faults
<25 km
Peak ground acceleration
≥0.40 g


## 3.4.2. Vertical Reservoir Cap Combination and Candidate Prospective Areas Distribution

The reservoirs for deep saline aquifer CO2 storage consist of the Permian, the lower Triassic carbonates, and upper Triassic and Jurassic clastic reservoirs (Figure 5). The reservoir space includes carbonate karst pores and cracks and clastic pores and cracks. Overall, all reservoirs in the Sichuan Basin have poor physical properties, with ultra-low porosity and low permeability. Comparing with the natural gas fields in the Sichuan Basin, these reservoirs for CO2 storage have better caprock conditions too. For example, the extensive deposits of gypsum rocks in the Leikoupo phase and the widely developed dark mudstone in the Lower Jurassic can provide good sealing conditions for the underlying reservoirs.Figure 5
CO2 geological storage vertical reservoir cap combination in the Sichuan Basin. There are nine sets of reservoirs in the Sichuan Basin, and the section four of Xujiahe group is the primary reservoir with large thickness and area, which almost cover the whole basin.(1) The Permian. The reef flat facies on the top of Qixia group form a good reservoir through dolomitization, with favorable reservoir conditions (P2q) [40]. Part of them form the natural gas reservoirs, with a thickness of approximately 10 m. Similar to the Qixia group, the Maokou group (P2m) is a fracture-cave type of reservoir. Changxing group (P3c) reservoirs are pore type and fracture-pore type. The porosity is generally 2.03%–15.85%, with an average value of 5.25%; the permeability is less than 1000 mD, with an average value of 6.05 mD. The reservoir thickness is large, with a monolayer thickness of 0.5–5 m and a single well cumulative thickness of 2.5–70 m [41].(2) The Triassic. The Feixianguan group (T1f) is similar to the Changxing group. The quality and distribution of the reef beach reservoir are mainly controlled by sedimentary facies and diagenesis. The evaporative platform oolitic dolomite reservoir is mainly distributed in Northeast Sichuan, with a monolayer thickness of 1.5–15 m and total thickness of 20–50 m. The porosity ranges from 2% to 26.8%, on the average of 8.29%; and the permeability is less than 1160 mD, with an average value of 59.73 mD. The porosity of the open platform edge oolitic dolomite reservoir is 2.05%–22.62%, on the average of 8.42%, and the permeability is less than 410 mD with an average value of 17.25 mD. The reservoir monolayer thickness is generally 0.5–6 m, and the total thickness is 10–45 m typically.The favorable Jialingjiang reservoir facies are the platform interior shoal and the platform margin shoal facies. For example, section five of Jialingjiang reservoirs consists of limestone and dolomite, with a thickness of 25–30 m, of which approximately 60% is the porosity layer, and the average of the porosity is 5%, with the highest value reaching 18%.The sandstone aquifers in section two, section four, and section six of Xujiahe formation could be reservoirs for CO2 geological storage, composed of residual intergranular pore, intergranular dissolved pore, and fracture. The sand ratio of the sandstones is greater than 70% in 80% generally. In addition, the porosity of section four is higher than section two and section six, usually between 5%–10%, while the porosity of sandstones in section two and section is less than 7% generally.Figure6 shows the candidate prospective areas in the Sichuan Basin in the Sichuan Basin for deep saline aquifer CO2 storage based on geology study.Figure 6
Candidate prospective areas in the Sichuan Basin. There are eight candidate prospective areas in the Sichuan Basin for deep saline aquifer CO2 storage which cover more than 5 × 104 km2 and mainly locate in Central Sichuan Basin (districts II–V). Only district I is in Northwestern Sichuan. The candidate prospective areas (districts VI–VIII) in Eastern Sichuan are relatively small due to the effects of formation depth, geological safety, and hydrogeological conditions.


## 4. Results

### 4.1. Potential

#### 4.1.1. Depleted Oil Fields CO2 Storage and CO2-EOR

The primary CO2-EOR prospective areas in the Sichuan Basin are located in the flat tectonic area in Central and Northern Sichuan Basin. As shown in Tables 9 and 10, the CO2 geological storage potential of storage in depleted oil fields is only 0.74 × 108 t, while the storage potential is about 0.21 × 108 t by using CO2-EOR technology.Table 9
Storage potential of CO2 geological storage in depleted oil fields.
Tectonic unit
O
O
I
P/108 t
Oil density (kg/m3)
B (—)
Reservoir pressure/Mpa
Oil temperature/°C
ρ
C
O
2 (kg/m3)
E
o
i
l
G
C
O
2/108 t
Central Sichuan flat structure area
0.58
850
1.18
21.26
64.42
712.63
0.75
0.57
Northern Sichuan flat structure area
0.17
850
1.18
21.26
64.42
712.63
0.75
0.17Table 10
CO2-EOR geological storage potential in the Sichuan Basin.
Tectonic unit
A
P
I
EXTRA (%)
P
L
C
O
2 (%)
P
H
C
O
2 (%)
E
o
i
l
G
C
O
2
-
E
O
R/108 t
Central Sichuan flat structure area
34.97
10.46
33
66
0.75
0.16
Northern Sichuan flat structure area
34.97
10.46
33
66
0.75
0.05


#### 4.1.2. Depleted Gas Fields CO2 Storage and CO2-EGR

The CO2 geological storage potential of depleted gas fields is 53.73 × 108 t. By using CO2-EGR technology, the Sichuan Basin gas fields could achieve CO2 geological storage of 33.85 × 108 t. Among that 27 large and medium gas fields have the greatest potential, with the possibility of achieving a CO2 geological storage capacity of 42.39 × 108 t in depleted gas fields, while the storage potential is about 26.70 × 108 t by using CO2-EGR technology.


#### 4.1.3. Unmineable Coal Seams CO2 Storage and CO2-ECBM

The Sichuan Basin has abundant coal bed methane resources. As shown in Table11, the total CO2 geological storage potential of unmineable coal seams can vary in the range from 3.55 × 108 t to 8.12 × 108 t (6.26 × 108 t on the average), while the storage potential of CO2-ECBM technology is half of the unmineable coal seams CO2 geological storage.Table 11
Storage potential of CO2 in unmineable coal seams and CO2-ECBM in the Sichuan Basin.
Area
G
C
B
M/108 m3
Types of coal
R
C
O
2
/
C
H
4
C
ρ
C
O
2
s
t
d (kg/m3)
G
C
O
2/108 t
G
C
O
2
-
E
C
B
M/108 t
Southern Sichuan and Northern Guizhou
5084.57
Mainly anthracite
1
0.50
1.977
3.72
1.86
Sichuan and Chongqing
3471.40
Mainly coking coal and lean coal
1
0.50
1.977
2.54
1.27However, the coal bed methane in the Sichuan Basin proposed by Ministry of Land and Resources (MLR) is just the theoretical geological reserves in place but not proven reserves, so the reliability of potential of unmineable coal seams and CO2-ECBM is much lower than depleted oil and gas fields CO2 storage and CO2-EOR and CO2-EGR.


#### 4.1.4. Deep Saline Aquifers CO2 Storage or CO2-EWR

The total CO2 geological storage potential in deep saline aquifers varies in the range of 77.81 × 108 t to 262.08 × 108 t (154.20 × 108 t on the average). However, the main CO2 geological reservoirs are sections two, four, and six of Xujiahe formation, with the storage potential of 71.98 × 108 t to 245.95 × 108 t (143.98 × 108 t on the average), that is, approximately 93.37% of the total storage potential.According to the statistics of the structural position, the total expected storage potential in Central Sichuan is the largest, reaching 89.26 × 108 t on the average. The total expected storage potentials in Western Sichuan and Eastern Sichuan are 45.68 × 108 t and 19.27 × 108 t on the average, respectively. The potential per unit area is shown in Figure 7.Figure 7
Storage potential per unit area for each prospective area. Due to the large stratigraphic thickness and many reservoir layers, the storage potential per unit area in most depressions in Northwestern Sichuan is quite large, with the largest up to 140 × 104 t/km2, atP50 probability level. The storage potential per unit area in Central Sichuan is generally greater than 50 × 104 t/km2, atP50 probability level.


### 4.2. Target Areas for Deep Saline Aquifers CO2 Storage

#### 4.2.1. Data

On the basis of systematic analysis of the deep saline aquifer CO2 geological storage cap, through the geological suitability evaluation index system, the superimposed multisource information evaluation was successively carried out using ArcGIS software. The basic information is shown in Table 12. As mentioned in Section 3.4.2, the main reservoir in the Sichuan Basin is the section four of Xujiahe formation.Table 12
Geological suitability assessment information of the main reservoir distribution area (within section four of Xujiahe formation).
Level one index
Level two index
Level three index
Distribution information of the main reservoir in Xujiahe section 4
Geological information outside of Xujiahe section 4 distribution
Reservoir conditions and storage potential
Reservoir geological characteristics
Lithology
Clastic
Mix of clastic and carbonate
Thickness/m
≥80
<30
Sedimentary facies
River, delta
Beach bar, reef
Average porosity/%
GIS partition processing
<10
Average permeability/mD
<10
<10
Storage potential
Storage potential per unit area (104 t/km2)
GIS partition processing
GIS partition processing
Geological safety
Cap geological characteristics
Lithology
Argillite
Argillite
Thickness/m
≥100
≥100
Main cap depth
1000–2700
1000–2700
Buffer cap above main cap
Multiple sets
Multiple sets
Hydrodynamic conditions
Hydrodynamic conditions
GIS partition processing
GIS partition processing
Seismic activity
Peak ground acceleration
GIS partition processing
GIS partition processing
Fracture development
GIS partition processing
GIS partition processing
The main reservoir is the section four of Xujiahe formation, and the main cap is the lower Jurassic strata. The GIS partition processing must be carried out separately for the prospective areas within and outside of section four of Xujiahe formation. The geological information outside of section four of Xujiahe formation is from the best value of other eight reservoirs.


#### 4.2.2. Target Areas

As shown in Figure8, most prospective areas are suitable for CO2 geological storage. The suitable areas could be used as the target areas for CO2 geological storage. By further ground suitability evaluation and social economic surveys, some project sites can be identified from those target areas for large-scale saline aquifers CO2 geological storage.Figure 8
Assessment results of CO2 geological storage suitability (suitable area is the “target area”). Most prospective areas in the Sichuan Basin are suitable for CO2 geological storage, which could be the “target areas” for CO2 geological storage. The main reservoirs in the Central Sichuan Basin are sections two, four, and six of Xujiahe formation with large thickness and good physical properties. They are far from the basin boundary faults, with weak hydrodynamic and good geological safety conditions.


## 4.1. Potential

### 4.1.1. Depleted Oil Fields CO2 Storage and CO2-EOR

The primary CO2-EOR prospective areas in the Sichuan Basin are located in the flat tectonic area in Central and Northern Sichuan Basin. As shown in Tables 9 and 10, the CO2 geological storage potential of storage in depleted oil fields is only 0.74 × 108 t, while the storage potential is about 0.21 × 108 t by using CO2-EOR technology.Table 9
Storage potential of CO2 geological storage in depleted oil fields.
Tectonic unit
O
O
I
P/108 t
Oil density (kg/m3)
B (—)
Reservoir pressure/Mpa
Oil temperature/°C
ρ
C
O
2 (kg/m3)
E
o
i
l
G
C
O
2/108 t
Central Sichuan flat structure area
0.58
850
1.18
21.26
64.42
712.63
0.75
0.57
Northern Sichuan flat structure area
0.17
850
1.18
21.26
64.42
712.63
0.75
0.17Table 10
CO2-EOR geological storage potential in the Sichuan Basin.
Tectonic unit
A
P
I
EXTRA (%)
P
L
C
O
2 (%)
P
H
C
O
2 (%)
E
o
i
l
G
C
O
2
-
E
O
R/108 t
Central Sichuan flat structure area
34.97
10.46
33
66
0.75
0.16
Northern Sichuan flat structure area
34.97
10.46
33
66
0.75
0.05


### 4.1.2. Depleted Gas Fields CO2 Storage and CO2-EGR

The CO2 geological storage potential of depleted gas fields is 53.73 × 108 t. By using CO2-EGR technology, the Sichuan Basin gas fields could achieve CO2 geological storage of 33.85 × 108 t. Among that 27 large and medium gas fields have the greatest potential, with the possibility of achieving a CO2 geological storage capacity of 42.39 × 108 t in depleted gas fields, while the storage potential is about 26.70 × 108 t by using CO2-EGR technology.


### 4.1.3. Unmineable Coal Seams CO2 Storage and CO2-ECBM

The Sichuan Basin has abundant coal bed methane resources. As shown in Table11, the total CO2 geological storage potential of unmineable coal seams can vary in the range from 3.55 × 108 t to 8.12 × 108 t (6.26 × 108 t on the average), while the storage potential of CO2-ECBM technology is half of the unmineable coal seams CO2 geological storage.Table 11
Storage potential of CO2 in unmineable coal seams and CO2-ECBM in the Sichuan Basin.
Area
G
C
B
M/108 m3
Types of coal
R
C
O
2
/
C
H
4
C
ρ
C
O
2
s
t
d (kg/m3)
G
C
O
2/108 t
G
C
O
2
-
E
C
B
M/108 t
Southern Sichuan and Northern Guizhou
5084.57
Mainly anthracite
1
0.50
1.977
3.72
1.86
Sichuan and Chongqing
3471.40
Mainly coking coal and lean coal
1
0.50
1.977
2.54
1.27However, the coal bed methane in the Sichuan Basin proposed by Ministry of Land and Resources (MLR) is just the theoretical geological reserves in place but not proven reserves, so the reliability of potential of unmineable coal seams and CO2-ECBM is much lower than depleted oil and gas fields CO2 storage and CO2-EOR and CO2-EGR.


### 4.1.4. Deep Saline Aquifers CO2 Storage or CO2-EWR

The total CO2 geological storage potential in deep saline aquifers varies in the range of 77.81 × 108 t to 262.08 × 108 t (154.20 × 108 t on the average). However, the main CO2 geological reservoirs are sections two, four, and six of Xujiahe formation, with the storage potential of 71.98 × 108 t to 245.95 × 108 t (143.98 × 108 t on the average), that is, approximately 93.37% of the total storage potential.According to the statistics of the structural position, the total expected storage potential in Central Sichuan is the largest, reaching 89.26 × 108 t on the average. The total expected storage potentials in Western Sichuan and Eastern Sichuan are 45.68 × 108 t and 19.27 × 108 t on the average, respectively. The potential per unit area is shown in Figure 7.Figure 7
Storage potential per unit area for each prospective area. Due to the large stratigraphic thickness and many reservoir layers, the storage potential per unit area in most depressions in Northwestern Sichuan is quite large, with the largest up to 140 × 104 t/km2, atP50 probability level. The storage potential per unit area in Central Sichuan is generally greater than 50 × 104 t/km2, atP50 probability level.


## 4.1.1. Depleted Oil Fields CO2 Storage and CO2-EOR

The primary CO2-EOR prospective areas in the Sichuan Basin are located in the flat tectonic area in Central and Northern Sichuan Basin. As shown in Tables 9 and 10, the CO2 geological storage potential of storage in depleted oil fields is only 0.74 × 108 t, while the storage potential is about 0.21 × 108 t by using CO2-EOR technology.Table 9
Storage potential of CO2 geological storage in depleted oil fields.
Tectonic unit
O
O
I
P/108 t
Oil density (kg/m3)
B (—)
Reservoir pressure/Mpa
Oil temperature/°C
ρ
C
O
2 (kg/m3)
E
o
i
l
G
C
O
2/108 t
Central Sichuan flat structure area
0.58
850
1.18
21.26
64.42
712.63
0.75
0.57
Northern Sichuan flat structure area
0.17
850
1.18
21.26
64.42
712.63
0.75
0.17Table 10
CO2-EOR geological storage potential in the Sichuan Basin.
Tectonic unit
A
P
I
EXTRA (%)
P
L
C
O
2 (%)
P
H
C
O
2 (%)
E
o
i
l
G
C
O
2
-
E
O
R/108 t
Central Sichuan flat structure area
34.97
10.46
33
66
0.75
0.16
Northern Sichuan flat structure area
34.97
10.46
33
66
0.75
0.05


## 4.1.2. Depleted Gas Fields CO2 Storage and CO2-EGR

The CO2 geological storage potential of depleted gas fields is 53.73 × 108 t. By using CO2-EGR technology, the Sichuan Basin gas fields could achieve CO2 geological storage of 33.85 × 108 t. Among that 27 large and medium gas fields have the greatest potential, with the possibility of achieving a CO2 geological storage capacity of 42.39 × 108 t in depleted gas fields, while the storage potential is about 26.70 × 108 t by using CO2-EGR technology.


## 4.1.3. Unmineable Coal Seams CO2 Storage and CO2-ECBM

The Sichuan Basin has abundant coal bed methane resources. As shown in Table11, the total CO2 geological storage potential of unmineable coal seams can vary in the range from 3.55 × 108 t to 8.12 × 108 t (6.26 × 108 t on the average), while the storage potential of CO2-ECBM technology is half of the unmineable coal seams CO2 geological storage.Table 11
Storage potential of CO2 in unmineable coal seams and CO2-ECBM in the Sichuan Basin.
Area
G
C
B
M/108 m3
Types of coal
R
C
O
2
/
C
H
4
C
ρ
C
O
2
s
t
d (kg/m3)
G
C
O
2/108 t
G
C
O
2
-
E
C
B
M/108 t
Southern Sichuan and Northern Guizhou
5084.57
Mainly anthracite
1
0.50
1.977
3.72
1.86
Sichuan and Chongqing
3471.40
Mainly coking coal and lean coal
1
0.50
1.977
2.54
1.27However, the coal bed methane in the Sichuan Basin proposed by Ministry of Land and Resources (MLR) is just the theoretical geological reserves in place but not proven reserves, so the reliability of potential of unmineable coal seams and CO2-ECBM is much lower than depleted oil and gas fields CO2 storage and CO2-EOR and CO2-EGR.


## 4.1.4. Deep Saline Aquifers CO2 Storage or CO2-EWR

The total CO2 geological storage potential in deep saline aquifers varies in the range of 77.81 × 108 t to 262.08 × 108 t (154.20 × 108 t on the average). However, the main CO2 geological reservoirs are sections two, four, and six of Xujiahe formation, with the storage potential of 71.98 × 108 t to 245.95 × 108 t (143.98 × 108 t on the average), that is, approximately 93.37% of the total storage potential.According to the statistics of the structural position, the total expected storage potential in Central Sichuan is the largest, reaching 89.26 × 108 t on the average. The total expected storage potentials in Western Sichuan and Eastern Sichuan are 45.68 × 108 t and 19.27 × 108 t on the average, respectively. The potential per unit area is shown in Figure 7.Figure 7
Storage potential per unit area for each prospective area. Due to the large stratigraphic thickness and many reservoir layers, the storage potential per unit area in most depressions in Northwestern Sichuan is quite large, with the largest up to 140 × 104 t/km2, atP50 probability level. The storage potential per unit area in Central Sichuan is generally greater than 50 × 104 t/km2, atP50 probability level.


## 4.2. Target Areas for Deep Saline Aquifers CO2 Storage

### 4.2.1. Data

On the basis of systematic analysis of the deep saline aquifer CO2 geological storage cap, through the geological suitability evaluation index system, the superimposed multisource information evaluation was successively carried out using ArcGIS software. The basic information is shown in Table 12. As mentioned in Section 3.4.2, the main reservoir in the Sichuan Basin is the section four of Xujiahe formation.Table 12
Geological suitability assessment information of the main reservoir distribution area (within section four of Xujiahe formation).
Level one index
Level two index
Level three index
Distribution information of the main reservoir in Xujiahe section 4
Geological information outside of Xujiahe section 4 distribution
Reservoir conditions and storage potential
Reservoir geological characteristics
Lithology
Clastic
Mix of clastic and carbonate
Thickness/m
≥80
<30
Sedimentary facies
River, delta
Beach bar, reef
Average porosity/%
GIS partition processing
<10
Average permeability/mD
<10
<10
Storage potential
Storage potential per unit area (104 t/km2)
GIS partition processing
GIS partition processing
Geological safety
Cap geological characteristics
Lithology
Argillite
Argillite
Thickness/m
≥100
≥100
Main cap depth
1000–2700
1000–2700
Buffer cap above main cap
Multiple sets
Multiple sets
Hydrodynamic conditions
Hydrodynamic conditions
GIS partition processing
GIS partition processing
Seismic activity
Peak ground acceleration
GIS partition processing
GIS partition processing
Fracture development
GIS partition processing
GIS partition processing
The main reservoir is the section four of Xujiahe formation, and the main cap is the lower Jurassic strata. The GIS partition processing must be carried out separately for the prospective areas within and outside of section four of Xujiahe formation. The geological information outside of section four of Xujiahe formation is from the best value of other eight reservoirs.


### 4.2.2. Target Areas

As shown in Figure8, most prospective areas are suitable for CO2 geological storage. The suitable areas could be used as the target areas for CO2 geological storage. By further ground suitability evaluation and social economic surveys, some project sites can be identified from those target areas for large-scale saline aquifers CO2 geological storage.Figure 8
Assessment results of CO2 geological storage suitability (suitable area is the “target area”). Most prospective areas in the Sichuan Basin are suitable for CO2 geological storage, which could be the “target areas” for CO2 geological storage. The main reservoirs in the Central Sichuan Basin are sections two, four, and six of Xujiahe formation with large thickness and good physical properties. They are far from the basin boundary faults, with weak hydrodynamic and good geological safety conditions.


## 4.2.1. Data

On the basis of systematic analysis of the deep saline aquifer CO2 geological storage cap, through the geological suitability evaluation index system, the superimposed multisource information evaluation was successively carried out using ArcGIS software. The basic information is shown in Table 12. As mentioned in Section 3.4.2, the main reservoir in the Sichuan Basin is the section four of Xujiahe formation.Table 12
Geological suitability assessment information of the main reservoir distribution area (within section four of Xujiahe formation).
Level one index
Level two index
Level three index
Distribution information of the main reservoir in Xujiahe section 4
Geological information outside of Xujiahe section 4 distribution
Reservoir conditions and storage potential
Reservoir geological characteristics
Lithology
Clastic
Mix of clastic and carbonate
Thickness/m
≥80
<30
Sedimentary facies
River, delta
Beach bar, reef
Average porosity/%
GIS partition processing
<10
Average permeability/mD
<10
<10
Storage potential
Storage potential per unit area (104 t/km2)
GIS partition processing
GIS partition processing
Geological safety
Cap geological characteristics
Lithology
Argillite
Argillite
Thickness/m
≥100
≥100
Main cap depth
1000–2700
1000–2700
Buffer cap above main cap
Multiple sets
Multiple sets
Hydrodynamic conditions
Hydrodynamic conditions
GIS partition processing
GIS partition processing
Seismic activity
Peak ground acceleration
GIS partition processing
GIS partition processing
Fracture development
GIS partition processing
GIS partition processing
The main reservoir is the section four of Xujiahe formation, and the main cap is the lower Jurassic strata. The GIS partition processing must be carried out separately for the prospective areas within and outside of section four of Xujiahe formation. The geological information outside of section four of Xujiahe formation is from the best value of other eight reservoirs.


## 4.2.2. Target Areas

As shown in Figure8, most prospective areas are suitable for CO2 geological storage. The suitable areas could be used as the target areas for CO2 geological storage. By further ground suitability evaluation and social economic surveys, some project sites can be identified from those target areas for large-scale saline aquifers CO2 geological storage.Figure 8
Assessment results of CO2 geological storage suitability (suitable area is the “target area”). Most prospective areas in the Sichuan Basin are suitable for CO2 geological storage, which could be the “target areas” for CO2 geological storage. The main reservoirs in the Central Sichuan Basin are sections two, four, and six of Xujiahe formation with large thickness and good physical properties. They are far from the basin boundary faults, with weak hydrodynamic and good geological safety conditions.


## 5. Discussion and Conclusions

### 5.1. Discussion

The purpose of this paper is not only to evaluate the mesoscale potential of different CCUS technologies but also select the suitable target areas for early demonstration in the Sichuan Basin. On the basis of geology study, the CO2 storage potential of CO2-EOR, CO2-EGR, CO2-ECBM, and saline aquifer CO2 storage technologies was first evaluated comprehensively. Compared with the similar studies before, the study scale in this paper is more detailed especially for CO2 storage in deep saline aquifers, which is based on further geological study of reservoirs, seals, hydrogeology, and geological safety. The basic data for potential assessment are from MLR, PetroChina, and other authorities; thus the potential results are more credible, and more in accordance with geology. Table 13 shows the storage potential results in this paper compared with studies before.Table 13
Storage potential results in this paper compared with studies before.
CCUS
Study scales
Authors
Results before (108 t)
Basic data
CO2 geological utilization
CO2-EOR
National
ACCA 21, 2014
MLR, 2010
National
Wei, 2015
Target
This paper
0.21
CO2-EGR
National
ACCA 21, 2014
MLR, 2010
National
Wei, 2015
Target
This paper
26.70
CO2-ECBM
National
ACCA 21, 2014
MLR, 2009
National
Wei, 2015
Target
This paper
3.13
CO2 geological storage
Depleted oil fields
National
Zhang, 2005
Basin
Li, 2009
0.20
Li, 2002
National
ACCA 21, 2014
MLR, 2010
Basin
Guo, 2014
Unpublished
National
Wei, 2015
Target
This paper
0.74
Depleted gas fields
National
Zhang, 2005
National
Liu, 2006
10.14
900~3500 m Recoverable reserves [25]
Basin
Li, 2009
10.50
MLR, 2010
National
ACCA 21, 2014
Basin
Guo, 2014
Unpublished
National
Wei, 2015
Target
This paper
42.39
Unmineable coal seams
National
Zhang, 2005
National
ACCA 21, 2014
MLR, 2009
Basin
Guo, 2014
Unpublished
National
Wei, 2015
Target
This paper
6.26
Deep saline aquifers
National
Zhang, 2005
National
Li, 2006
64.07
National
Li, 2009
National
ACCA 21, 2014
Basin
Guo, 2014
Unpublished
National
Wei, 2015
Target
This paper
154.20
Further geological study


### 5.2. Conclusions

Taking the low technical application levels of CO2-EWR and CO2-EGR into account, it is recommended that deep saline aquifers and depleted gas fields CO2 geological storage in the Sichuan Basin could be early demonstrated, especially that of the latter because of excellent traps, rich geological data, and well-run infrastructures.


#### 5.2.1. Deep Saline Aquifers CO2 Geological Storage

For deep saline aquifers CO2 geological storage, based on the consideration of deep saline aquifer CO2 geological storage mechanism and geology of the Sichuan Basin, this paper proposes the study order of “prospective areas” to “target areas” and a new GIS superimposed multisource information evaluation method of geological suitability for target selection. The index system of geological suitability assessment for target selection is appropriate for multiple tectonics, facies, and reservoirs, to evaluate the suitability of prospective areas to select suitable target areas. The GIS superimposed multisource information evaluation results show that most areas are suitable for CO2 geological storage, and only some local peripheral areas are not suitable for CO2 geological storage. The areas selected through geological suitability assessment can be used as target areas for CO2 geological storage.The geology in Central Sichuan provides the best conditions, and the storage potential per unit area in Central Sichuan is generally greater than 50 × 104 t/km2, atP50 probability level, with Xujiahe group is the main reservoir. However, deep saline aquifers CO2 geological storage could only be used in the future due to its lack of other economic benefits, high investment, and multiple barriers in the short term.


#### 5.2.2. Depleted Gas Fields CO2 Geological Storage

In the mesoscale, gas fields under exploration or exploitation can be used as target areas for depleted gas fields CO2 geological storage. The MLR has announced that there are 125 gas fields in the Sichuan Basin and 27 medium to large-sized confirmed gas fields among them. There are many gas reservoirs or traps becomes depleted, which provide a great chance for early demonstration first for the CO2 resources located in the Sichuan Basin. Even in the long run, the depleted gas fields could be the main reservoirs for CO2 geological storage in the Sichuan Basin.


## 5.1. Discussion

The purpose of this paper is not only to evaluate the mesoscale potential of different CCUS technologies but also select the suitable target areas for early demonstration in the Sichuan Basin. On the basis of geology study, the CO2 storage potential of CO2-EOR, CO2-EGR, CO2-ECBM, and saline aquifer CO2 storage technologies was first evaluated comprehensively. Compared with the similar studies before, the study scale in this paper is more detailed especially for CO2 storage in deep saline aquifers, which is based on further geological study of reservoirs, seals, hydrogeology, and geological safety. The basic data for potential assessment are from MLR, PetroChina, and other authorities; thus the potential results are more credible, and more in accordance with geology. Table 13 shows the storage potential results in this paper compared with studies before.Table 13
Storage potential results in this paper compared with studies before.
CCUS
Study scales
Authors
Results before (108 t)
Basic data
CO2 geological utilization
CO2-EOR
National
ACCA 21, 2014
MLR, 2010
National
Wei, 2015
Target
This paper
0.21
CO2-EGR
National
ACCA 21, 2014
MLR, 2010
National
Wei, 2015
Target
This paper
26.70
CO2-ECBM
National
ACCA 21, 2014
MLR, 2009
National
Wei, 2015
Target
This paper
3.13
CO2 geological storage
Depleted oil fields
National
Zhang, 2005
Basin
Li, 2009
0.20
Li, 2002
National
ACCA 21, 2014
MLR, 2010
Basin
Guo, 2014
Unpublished
National
Wei, 2015
Target
This paper
0.74
Depleted gas fields
National
Zhang, 2005
National
Liu, 2006
10.14
900~3500 m Recoverable reserves [25]
Basin
Li, 2009
10.50
MLR, 2010
National
ACCA 21, 2014
Basin
Guo, 2014
Unpublished
National
Wei, 2015
Target
This paper
42.39
Unmineable coal seams
National
Zhang, 2005
National
ACCA 21, 2014
MLR, 2009
Basin
Guo, 2014
Unpublished
National
Wei, 2015
Target
This paper
6.26
Deep saline aquifers
National
Zhang, 2005
National
Li, 2006
64.07
National
Li, 2009
National
ACCA 21, 2014
Basin
Guo, 2014
Unpublished
National
Wei, 2015
Target
This paper
154.20
Further geological study


## 5.2. Conclusions

Taking the low technical application levels of CO2-EWR and CO2-EGR into account, it is recommended that deep saline aquifers and depleted gas fields CO2 geological storage in the Sichuan Basin could be early demonstrated, especially that of the latter because of excellent traps, rich geological data, and well-run infrastructures.


### 5.2.1. Deep Saline Aquifers CO2 Geological Storage

For deep saline aquifers CO2 geological storage, based on the consideration of deep saline aquifer CO2 geological storage mechanism and geology of the Sichuan Basin, this paper proposes the study order of “prospective areas” to “target areas” and a new GIS superimposed multisource information evaluation method of geological suitability for target selection. The index system of geological suitability assessment for target selection is appropriate for multiple tectonics, facies, and reservoirs, to evaluate the suitability of prospective areas to select suitable target areas. The GIS superimposed multisource information evaluation results show that most areas are suitable for CO2 geological storage, and only some local peripheral areas are not suitable for CO2 geological storage. The areas selected through geological suitability assessment can be used as target areas for CO2 geological storage.The geology in Central Sichuan provides the best conditions, and the storage potential per unit area in Central Sichuan is generally greater than 50 × 104 t/km2, atP50 probability level, with Xujiahe group is the main reservoir. However, deep saline aquifers CO2 geological storage could only be used in the future due to its lack of other economic benefits, high investment, and multiple barriers in the short term.


### 5.2.2. Depleted Gas Fields CO2 Geological Storage

In the mesoscale, gas fields under exploration or exploitation can be used as target areas for depleted gas fields CO2 geological storage. The MLR has announced that there are 125 gas fields in the Sichuan Basin and 27 medium to large-sized confirmed gas fields among them. There are many gas reservoirs or traps becomes depleted, which provide a great chance for early demonstration first for the CO2 resources located in the Sichuan Basin. Even in the long run, the depleted gas fields could be the main reservoirs for CO2 geological storage in the Sichuan Basin.


## 5.2.1. Deep Saline Aquifers CO2 Geological Storage

For deep saline aquifers CO2 geological storage, based on the consideration of deep saline aquifer CO2 geological storage mechanism and geology of the Sichuan Basin, this paper proposes the study order of “prospective areas” to “target areas” and a new GIS superimposed multisource information evaluation method of geological suitability for target selection. The index system of geological suitability assessment for target selection is appropriate for multiple tectonics, facies, and reservoirs, to evaluate the suitability of prospective areas to select suitable target areas. The GIS superimposed multisource information evaluation results show that most areas are suitable for CO2 geological storage, and only some local peripheral areas are not suitable for CO2 geological storage. The areas selected through geological suitability assessment can be used as target areas for CO2 geological storage.The geology in Central Sichuan provides the best conditions, and the storage potential per unit area in Central Sichuan is generally greater than 50 × 104 t/km2, atP50 probability level, with Xujiahe group is the main reservoir. However, deep saline aquifers CO2 geological storage could only be used in the future due to its lack of other economic benefits, high investment, and multiple barriers in the short term.


## 5.2.2. Depleted Gas Fields CO2 Geological Storage

In the mesoscale, gas fields under exploration or exploitation can be used as target areas for depleted gas fields CO2 geological storage. The MLR has announced that there are 125 gas fields in the Sichuan Basin and 27 medium to large-sized confirmed gas fields among them. There are many gas reservoirs or traps becomes depleted, which provide a great chance for early demonstration first for the CO2 resources located in the Sichuan Basin. Even in the long run, the depleted gas fields could be the main reservoirs for CO2 geological storage in the Sichuan Basin.



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*Source: 9587872-2017-07-02.xml*