# Selection of Optimal Threshold of Generalised Rock Quality Designation Based on Modified Blockiness Index

Authors: Qingfa Chen; Tingchang Yin; Hangyu Jia
Journal: Advances in Civil Engineering
 (2019)

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## Abstract

Rock quality designation (RQD) is a critical index for quantifying the degree of rock mass jointing; it is widely used for evaluating the qualities and stabilities of engineering rock masses. However, the use of traditional RQD may yield inaccurate assessments because only core pieces longer than 100 mm are counted. To enhance the utility of RQD, generalised RQD was introduced. Based on the modified blockiness index (MBi), the determination of the optimal threshold of generalised RQD was performed. In this work, 35 types of hypothetical three-dimensional joint network models were constructed, and their generalised RQD values (with different thresholds) and MBi values were measured. The correlation between the standard ratings of MBi and RQD was assessed; based on this correlation, the theoretical RQD values of the 35 models were derived. The reasonable thresholds of the generalised RQD were determined according to the theoretical RQD values, and the optimal threshold of generalised RQD was obtained using the variation coefficient and anisotropy index of the jointing degree. The discrepancy between the results produced using traditional and generalised RQDs was discussed. Finally, an actual case study was conducted, and the results indicate that the generalised RQD associated with the optimal threshold determined in this study can properly quantify the degree of jointing of a given rock mass.


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## Body

## 1. Introduction

A rock mass is a natural substance that is composed of different compositions and complex structures produced by geologic processes. It varies with the evolution of the geological environment. Owing to the complicacy and invisibility of the rock mass structure, engineers cannot deeply understand the mechanical behaviour of jointed rock mass. Rock mass is separated into blocks because of the presence of joints; therefore, the mechanical properties and stabilities of engineering rock masses are deteriorated significantly [1].Rock quality designation (RQD) [2] is a critical index to quantify the degree of jointing and is typically applied in various rock engineering worldwide, including hydraulic engineering, underground and surface mining, and rock tunnel; furthermore, RQD has been used for over 50 years. RQD is defined as a percentage of the drill core in lengths of 100 mm or greater. Although the RQD is routinely used in practices, this concept has several inherent limitations; for example, the RQD index only considers core pieces longer than 100 mm and may result in a final RQD value that does not agree with the practice [3].To improve the utility of the RQD, some investigations were undertaken; for example, Sen and Elssa [4] proposed the concept of volumetric RQD and evaluated the correlations between RQDs with different thresholds, volumetric joint count (Jv), and block size; they outlined that the relations between the RQD values with different thresholds and the Jv values should be nonlinear, and such relations vary with the shapes of the blocks. Harrison [5] reported that, with an optimal threshold, the variation in RQD values in different directions is maximal; that is, the anisotropy of the rock mass structure is highlighted maximally; additionally, through theoretical derivation, he provided a determination equation of the optimal threshold in conjunction with the maximum and minimum joint frequencies. Xu et al. [6] investigated the correlation between the fractal dimensions of joints and RQD values based on the discrete fracture network (DFN) technique. They also reported that when the rock masses are sparsely jointed, the use of traditional RQD cannot sufficiently differentiate the rock mass structures; however, when the slopes of the curve (fractal dimensions vs. RQDs with different thresholds) attain a maximum value, the associated threshold can be deemed an optimal value. Zhang et al. [7, 8] developed a determination method of the optimal RQD threshold based on a three-dimensional joint network model and setting virtual scanlines; they also claimed that the variation in RQD values can be maximised with an optimal threshold.The reviewed literatures reported that when the RQD values are accompanied by an optimal threshold in a given rock mass, the anisotropy of the rock mass structure can be fully reflected; that is, the difference between the maximum RQD value (RQDmax) and the minimum RQD value (RQDmin) is maximised. However, from the perspective of engineering practicability, the RQD values accompanied by an optimal threshold should exactly quantify the degree of jointing to lay the groundwork for the subsequent tasks, e.g., rock mass quality classification and rock mass stability assessment.Recently, the modified blockiness index (MBi) [9, 10] was developed as a three-dimensional measurement for the degree of rock mass jointing; using this index, the implications of blocks of different sizes on the rock mass jointing can be considered. However, the typical practice in rock engineering applications is to use RQD to quantify the degree of jointing; meanwhile, knowing the RQD value is crucial in many rock mass quality classifications and stability assessment systems, such as the rock mass rating system [11], Q-system [12], and Qslope-system [13, 14]; furthermore, the associated empirical relation with the determination of support schemes has been well developed. Therefore, we do not attempt to replace the RQD with MBi but to enhance the utility of RQD. In this study, referring to the MBi, the determination of the optimal threshold of RQD was investigated based on the three-dimensional joint network modelling suggested by Zhang et al. [8], which can avoid the high uncertainty of the determination of RQD values. The goal of this study is to obtain an RQD value with the optimal threshold to quantify the degree of jointing more properly. Additionally, this work may provide an appropriate reference for determining a proper RQD value in other rock engineering projects.


## 2. Modified Blockiness Index (MBi)

The block percentage (B) [9] is defined as the ratio of the volume of blocks fully enclosed by joints to the total rock mass volume, which ranges from 0 to 100%, and can be expressed as(1)B=∑i=1nviV,where vi is the volume of block i, n is the number of blocks, and V is the total rock mass volume.When the block percentage is used to quantify the degree of jointing, the effect of block size may be ignored. To address this problem, Chen et al. [10] developed the MBi, in which the rock blocks are grouped into five categories according to block volume: 0–0.008 m3, 0.008–0.03 m3, 0.03–0.2 m3, 0.2–1.0 m3, and >1.0 m3, and the percentages of blocks in different categories are assigned different weights, i.e., the coefficients of rock block scale effect [15, 16]. The MBi value can be calculated by(2)MBi=B1+12B2+13B3+14B4+15B5,where B1, B2, B3, B4, and B5 are the block percentages of the volumes in the five intervals (0–0.008 m3, 0.008–0.03 m3, 0.03–0.2 m3, 0.2–1.0 m3, and >1.0 m3, respectively). Apparently, with an increase in the degree of jointing, the MBi value increases and the number of small blocks inside the rock mass increases, and vice versa. The calculation of MBi is based entirely on the three-dimensional joint network model, and this kind of model can be created by probabilistic and/or deterministic joints.In this study, the block percentages and MBi values were determined using the GeneralBlock program [9], in the following steps: (1) construct a three-dimensional joint network model, (2) calculate the volumes of the rock blocks that are separated by joints, and (3) determine the block percentages and MBi values based on Eqs. (1) and (2).


## 3. Traditional and Generalised RQDs

### 3.1. Traditional RQD

Traditional RQD was pioneered by Deere in 1967 [2] and is defined by a percentage of the drill core in lengths of 100 mm or greater. The RQD concept is widely used worldwide; however, it suffers from critiques [17, 18], including the following: (i) the RQD value is anisotropic and orientation dependent and (ii) the RQD concept only considers core pieces longer than 100 mm; that is, the block scale effect is ignored.


### 3.2. Generalised RQD

The concept of generalised RQD (RQDt) was introduced in [7, 8]. Using this concept, the threshold can be varied. Far less work has been performed on investigating RQDt; however, the RQDt is important in the investigation of the anisotropy of the rock mass structure; that is, a specified threshold can enhance the variation in RQDt values. When the joint density is extremely high, the calculated RQDt values in all directions are always close to 100% if the selected threshold is small; if the threshold is large, the RQDt values will be approximately 0% regardless of the directions of the scanlines. The RQDt value is influenced by the threshold t, and the core pieces should be counted if their lengths are equal to or greater than t. The RQDt can be calculated by(3)RQDt=100L∑i=1nxi%,where xi is the length of the core piece longer than t and L is the total length of the scanline. Given various t values, a series of RQDt values can be obtained and subsequently used to describe the degree of jointing.According to the recommendation from Zhang et al. [8], a calculation model of RQDt termed “Model A-A-S” was employed, which can be expressed as follows:(4)RQDt=l1+l2+ltl×100%,l1+l2<t,ltl×100%,l1+l2>t,where l1 and l2 are the lengths of the core pieces at the start and end of the scanline, respectively, and lt is the total length of the inner core pieces that is greater than the given threshold t.


## 3.1. Traditional RQD

Traditional RQD was pioneered by Deere in 1967 [2] and is defined by a percentage of the drill core in lengths of 100 mm or greater. The RQD concept is widely used worldwide; however, it suffers from critiques [17, 18], including the following: (i) the RQD value is anisotropic and orientation dependent and (ii) the RQD concept only considers core pieces longer than 100 mm; that is, the block scale effect is ignored.


## 3.2. Generalised RQD

The concept of generalised RQD (RQDt) was introduced in [7, 8]. Using this concept, the threshold can be varied. Far less work has been performed on investigating RQDt; however, the RQDt is important in the investigation of the anisotropy of the rock mass structure; that is, a specified threshold can enhance the variation in RQDt values. When the joint density is extremely high, the calculated RQDt values in all directions are always close to 100% if the selected threshold is small; if the threshold is large, the RQDt values will be approximately 0% regardless of the directions of the scanlines. The RQDt value is influenced by the threshold t, and the core pieces should be counted if their lengths are equal to or greater than t. The RQDt can be calculated by(3)RQDt=100L∑i=1nxi%,where xi is the length of the core piece longer than t and L is the total length of the scanline. Given various t values, a series of RQDt values can be obtained and subsequently used to describe the degree of jointing.According to the recommendation from Zhang et al. [8], a calculation model of RQDt termed “Model A-A-S” was employed, which can be expressed as follows:(4)RQDt=l1+l2+ltl×100%,l1+l2<t,ltl×100%,l1+l2>t,where l1 and l2 are the lengths of the core pieces at the start and end of the scanline, respectively, and lt is the total length of the inner core pieces that is greater than the given threshold t.


## 4. Development of 35 Three-Dimensional Joint Network Models and Their MBi and RQD Values

### 4.1. Establishment of the Hypothetical Three-Dimensional Joint Network Models

According to the standard classification of rock joints suggested by the International Society for Rock Mechanics [19], five representative joint persistence values and seven representative joint spacing values were selected, as shown in Table 1. Additionally, the Baecher disc model [20] was applied to create the joints; it can be generated by the following parameters: the centre coordinate (x0, y0, z0), diameter d, dip direction α, and dip angle β (Figure 1). A Baecher disc model can be represented as follows:(5)Ax−x0+By−y0+Cz−z0=0,(6)x−x02+y−y02+z−z02=r=d2,where A = sin α sin β, B = sin α cos β, and C = cos α. Therefore, the normal vector of the disc joint n is (A, B, C).Table 1
Selected representative values of joint spacing and persistence.
Joint spacing classification
Extremely wide
Very wide
Wide
Moderate
Close
Very close
Extremely close
Selected value (m)
6
4
1.3
0.4
0.13
0.04
0.02
Joint persistence classification
Very high
High
Medium
Low
Very low
Selected value (m)
40
20
10
3
1Figure 1
Disc model of the joint.n is the normal vector of the disc joint.The orientations of the joints were assumed to exhibit a Fisher distribution:(7)fα,β=fβfα=12πκsinα2sinhκeκcosα,where κ is the Fisher coefficient. In addition, the three-dimensional density of a set of joints can be determined by(8)d3=4d1πED2En⋅i,where i is the vector along the scanline l and ED2 is the mean value of the squared joint diameter.When the number of joint sets is constant, the joint density/frequency/spacing affects the degree of rock mass jointing the most, followed by joint persistence [11, 21]; meanwhile, other geometrical parameters, such as joint orientation and distribution type, have negligible influences on such a degree [22]. The number of joint sets was fixed to three in this study, and other geometrical parameters of joints (with the exceptions of joint spacing and persistence) were also unchanged (Table 2), because (1) blocks form inside the rock mass as three sets of joints exist and (2) the computing time is always dissatisfactory if the number of joint sets is larger than three. The selected five representative joint persistence values and seven representative joint spacing values were cross-joined; hence, 35 pairs of “persistence-spacing” were obtained. Additionally, based on Eq. (8) and Table 2, the three-dimensional joint density of each pair was calculated, as shown in Table 3.Table 2
Distribution parameters of the joint parameters of the theoretical DFN model.
Joint set no.
Set 1
Set 2
Set 3
Distribution type of joint persistence
Uniform
Uniform
Uniform
Distribution type of joint orientation
Uniform
Uniform
Uniform
Fisher’s coefficientκ
0
0
0
Average dip direction/dip angle (°)
0/90
90/0
90/90Table 3
Three-dimensional joint densities of 35 pairs of “persistence-spacing.”
Joint persistence (m)
Joint spacing (m)
Extremely wide
Very wide
Wide
Moderate
Close
Very close
Extremely close
0.02
0.04
0.13
0.4
1.3
4
6
40
Very high
0.0398
0.0199
0.0061
0.0020
0.0006
0.0002
0.0001
20
High
0.1592
0.0796
0.0245
0.0080
0.0024
0.0008
0.0005
10
Medium
0.6369
0.3185
0.9799
0.0318
0.0098
0.0032
0.0021
3
Low
7.0771
3.5386
1.0888
0.3539
0.1089
0.0354
0.0236
1
Very low
63.6620
31.8310
9.7942
3.1831
0.9794
0.3183
0.2122The flow chart to show the process of generating the network model is shown in Figure2. Based on Tables 2 and 3, 35 types of hypothetical three-dimensional joint network models were constructed, as shown in Figure 3. It is noteworthy that the sizes of all models arrive at the geometrical representative elementary volume of rock mass [23].Figure 2
Flow chart of the generation of a three-dimensional joint network model.Figure 3
Thirty-five types of three-dimensional joint network models with different combinations of joint spacing and persistence. Each model’s number is stated below the model; the first number indicates joint persistence, the second indicates joint spacing, and the third represents the side length of the model.


### 4.2. MBi Values of All Models

The blocks inside the 35 models and their volumes were identified; after removing the blocks formed by a combination of the boundary surfaces and joints, the MBi values of all models were measured using Eq. (2); these values are presented in Table 4. The table shows that the wider the joint spacing is, the smaller the MBi value is; also, the higher the joint persistence is, the larger the MBi value is.Table 4
MBi values (%) of the 35 types of hypothetical models and the corresponding ratings.
Joint persistence (m)
Joint spacing (m)
Extremely wide
Very wide
Wide
Moderate
Close
Very close
Extremely close
0.02
0.04
0.13
0.4
1.3
4
6
40
Very high
93.7571
91.4286
61.2567
27.5231
17.5350
10.5002
0.3650
20
High
91.0728
87.5613
44.6782
23.9566
13.5002
0.3186
0.0307
10
Medium
90.2910
87.2045
44.0021
20.9621
4.6818
0.0573
0.0012
3
Low
88.9321
86.0180
43.8025
7.9657
0.1070
1.20E-8
1.78E-10
1
Very low
87.9759
84.3504
18.2843
0.1110
5.13E-5
1.03E-7
1.74E-9


### 4.3. Measurement of RQDt Values

Referring to the associated definition, the RQDt values of a three-dimensional joint network model were measured by setting the scanlines. Three cross sections were extracted along the plane at 1/2Lx, 1/2Ly, and 1/2Lz (Lx, Ly, and Lz mean the lengths of the sides in the X, Y, and Z directions, respectively), and scanlines were established through the geometrical centre of the cross sections every 10°, as illustrated in Figure 4. Hence, a total of 18 or 54 scanlines were set in the cross section or on the model.Figure 4
Illustration of setting scanlines in a model.When the cross section is extracted at 1/2Lx, the scanline can be expressed as(9)xs=12Lx,zs=ys⋅tanπ2−βs,where βs is the plunge of a scanline.From Eqs. (5), (6), and (9), an equation of the intersection of the joint and scanline can be established; if the solution of this equation is a real number, the intersection point between the joint and scanline exists, and vice versa. After the coordinates of the intersection points are determined, the length of the core piece along the scanline can be calculated.Using the aforementioned measurement of the core piece length, a total of 54 RQDt values can be determined in the model, and the mean can be regarded as the representative RQDt value of this model. When the investigation of the optimal t value of RQDt is implemented, a series of g RQDt values can be calculated with the variation in the t value.


## 4.1. Establishment of the Hypothetical Three-Dimensional Joint Network Models

According to the standard classification of rock joints suggested by the International Society for Rock Mechanics [19], five representative joint persistence values and seven representative joint spacing values were selected, as shown in Table 1. Additionally, the Baecher disc model [20] was applied to create the joints; it can be generated by the following parameters: the centre coordinate (x0, y0, z0), diameter d, dip direction α, and dip angle β (Figure 1). A Baecher disc model can be represented as follows:(5)Ax−x0+By−y0+Cz−z0=0,(6)x−x02+y−y02+z−z02=r=d2,where A = sin α sin β, B = sin α cos β, and C = cos α. Therefore, the normal vector of the disc joint n is (A, B, C).Table 1
Selected representative values of joint spacing and persistence.
Joint spacing classification
Extremely wide
Very wide
Wide
Moderate
Close
Very close
Extremely close
Selected value (m)
6
4
1.3
0.4
0.13
0.04
0.02
Joint persistence classification
Very high
High
Medium
Low
Very low
Selected value (m)
40
20
10
3
1Figure 1
Disc model of the joint.n is the normal vector of the disc joint.The orientations of the joints were assumed to exhibit a Fisher distribution:(7)fα,β=fβfα=12πκsinα2sinhκeκcosα,where κ is the Fisher coefficient. In addition, the three-dimensional density of a set of joints can be determined by(8)d3=4d1πED2En⋅i,where i is the vector along the scanline l and ED2 is the mean value of the squared joint diameter.When the number of joint sets is constant, the joint density/frequency/spacing affects the degree of rock mass jointing the most, followed by joint persistence [11, 21]; meanwhile, other geometrical parameters, such as joint orientation and distribution type, have negligible influences on such a degree [22]. The number of joint sets was fixed to three in this study, and other geometrical parameters of joints (with the exceptions of joint spacing and persistence) were also unchanged (Table 2), because (1) blocks form inside the rock mass as three sets of joints exist and (2) the computing time is always dissatisfactory if the number of joint sets is larger than three. The selected five representative joint persistence values and seven representative joint spacing values were cross-joined; hence, 35 pairs of “persistence-spacing” were obtained. Additionally, based on Eq. (8) and Table 2, the three-dimensional joint density of each pair was calculated, as shown in Table 3.Table 2
Distribution parameters of the joint parameters of the theoretical DFN model.
Joint set no.
Set 1
Set 2
Set 3
Distribution type of joint persistence
Uniform
Uniform
Uniform
Distribution type of joint orientation
Uniform
Uniform
Uniform
Fisher’s coefficientκ
0
0
0
Average dip direction/dip angle (°)
0/90
90/0
90/90Table 3
Three-dimensional joint densities of 35 pairs of “persistence-spacing.”
Joint persistence (m)
Joint spacing (m)
Extremely wide
Very wide
Wide
Moderate
Close
Very close
Extremely close
0.02
0.04
0.13
0.4
1.3
4
6
40
Very high
0.0398
0.0199
0.0061
0.0020
0.0006
0.0002
0.0001
20
High
0.1592
0.0796
0.0245
0.0080
0.0024
0.0008
0.0005
10
Medium
0.6369
0.3185
0.9799
0.0318
0.0098
0.0032
0.0021
3
Low
7.0771
3.5386
1.0888
0.3539
0.1089
0.0354
0.0236
1
Very low
63.6620
31.8310
9.7942
3.1831
0.9794
0.3183
0.2122The flow chart to show the process of generating the network model is shown in Figure2. Based on Tables 2 and 3, 35 types of hypothetical three-dimensional joint network models were constructed, as shown in Figure 3. It is noteworthy that the sizes of all models arrive at the geometrical representative elementary volume of rock mass [23].Figure 2
Flow chart of the generation of a three-dimensional joint network model.Figure 3
Thirty-five types of three-dimensional joint network models with different combinations of joint spacing and persistence. Each model’s number is stated below the model; the first number indicates joint persistence, the second indicates joint spacing, and the third represents the side length of the model.


## 4.2. MBi Values of All Models

The blocks inside the 35 models and their volumes were identified; after removing the blocks formed by a combination of the boundary surfaces and joints, the MBi values of all models were measured using Eq. (2); these values are presented in Table 4. The table shows that the wider the joint spacing is, the smaller the MBi value is; also, the higher the joint persistence is, the larger the MBi value is.Table 4
MBi values (%) of the 35 types of hypothetical models and the corresponding ratings.
Joint persistence (m)
Joint spacing (m)
Extremely wide
Very wide
Wide
Moderate
Close
Very close
Extremely close
0.02
0.04
0.13
0.4
1.3
4
6
40
Very high
93.7571
91.4286
61.2567
27.5231
17.5350
10.5002
0.3650
20
High
91.0728
87.5613
44.6782
23.9566
13.5002
0.3186
0.0307
10
Medium
90.2910
87.2045
44.0021
20.9621
4.6818
0.0573
0.0012
3
Low
88.9321
86.0180
43.8025
7.9657
0.1070
1.20E-8
1.78E-10
1
Very low
87.9759
84.3504
18.2843
0.1110
5.13E-5
1.03E-7
1.74E-9


## 4.3. Measurement of RQDt Values

Referring to the associated definition, the RQDt values of a three-dimensional joint network model were measured by setting the scanlines. Three cross sections were extracted along the plane at 1/2Lx, 1/2Ly, and 1/2Lz (Lx, Ly, and Lz mean the lengths of the sides in the X, Y, and Z directions, respectively), and scanlines were established through the geometrical centre of the cross sections every 10°, as illustrated in Figure 4. Hence, a total of 18 or 54 scanlines were set in the cross section or on the model.Figure 4
Illustration of setting scanlines in a model.When the cross section is extracted at 1/2Lx, the scanline can be expressed as(9)xs=12Lx,zs=ys⋅tanπ2−βs,where βs is the plunge of a scanline.From Eqs. (5), (6), and (9), an equation of the intersection of the joint and scanline can be established; if the solution of this equation is a real number, the intersection point between the joint and scanline exists, and vice versa. After the coordinates of the intersection points are determined, the length of the core piece along the scanline can be calculated.Using the aforementioned measurement of the core piece length, a total of 54 RQDt values can be determined in the model, and the mean can be regarded as the representative RQDt value of this model. When the investigation of the optimal t value of RQDt is implemented, a series of g RQDt values can be calculated with the variation in the t value.


## 5. Investigation of Selecting an Optimal Threshold of RQDt

### 5.1. Correlation between the Standard Ratings of MBi and RQD

The MBi and RQD indices can be used to quantify the degree of rock mass jointing, and both of them divide such a degree into five categories, as shown in Tables 5 and 6. The correlation between standard ratings of MBi and RQD was assessed; this is shown in Figure 5. From this figure, a good linear relation was found between the standard ratings of MBi and RQD, which is expressed as(10)RQD=100−0.92MBi.Table 5
Standard ratings of MBi.
MBi
<7
7–27
27–55
55–85
≥85
Rating
I
II
III
IV
V
Description
Integrated
Relatively integrated
Poorly integrated
Relatively fractured
FracturedTable 6
Standard ratings of RQD.
RQD
90–100
75–90
50–75
25–50
<25
Rating
I
II
III
IV
V
Description
Very good
Good
Fair
Poor
Very poorFigure 5
Correlation between the standard ratings of MBi and RQD.The determination coefficient is 0.99, indicating a high fitting degree. Based on Eq. (10), theoretical RQD values can be derived.


### 5.2. Theoretical RQD Values

From Table4 and Eq. (10), the theoretical RQD values of the 35 models were determined, as shown in Table 7. The theoretical RQD value can be defined as an RQD value derived by the MBi, which is more compatible with the actual degree of rock mass jointing.Table 7
Theoretical RQD values (%) of all hypothetical models.
Joint persistence (m)
Joint spacing (m)
Extremely wide
Very wide
Wide
Moderate
Close
Very close
Extremely close
0.02
0.04
0.13
0.4
1.3
4
6
40
Very high
11.50
13.69
42.03
73.71
83.08
89.69
99.21
20
High
14.03
17.32
57.59
77.05
86.87
99.25
99.52
10
Medium
14.76
17.66
58.23
79.87
95.16
99.55
99.55
3
Low
16.04
18.78
58.42
92.07
99.45
99.55
99.55
1
Very low
16.94
20.34
82.39
99.45
99.55
99.55
99.55


### 5.3. Selection of Optimal Threshold of RQDt

The three-dimensional joint network model with a joint persistence of 20 m and joint spacing of 1.3 m was used as an example to demonstrate the procedure for selecting an optimal threshold of the RQDt. Based on the measurement described in Section 4.3, the (representative) RQDt values of different thresholds were calculated, as shown in Figure 6. The figure indicates that (1) when the threshold is 100 mm, the RQDt value is close to 100%, and when the threshold is 1000 mm, the RQDt value is approximately 70%, and (2) with the increase in t value, the RQDt values tend to be reduced.Figure 6
Generalised RQD values with different thresholds of the exampled model.As shown in Table4, the MBi value of this example model is 13.50%, which belongs to Class II (“relatively integrated” category). The corresponding rating of the theoretical RQD value also belongs to Class II (“good” category); that is, when the measured RQDt values are in the interval of 75% to 90%, the RQDt values can be regarded as reasonable, and the corresponding t values can be termed as reasonable thresholds.Figure6 shows that the reasonable thresholds are 600 mm, 700 mm, 800 mm, and 900 mm, and an optimal t value should be further selected. Owing to the anisotropy of the rock mass structure, the RQDt values in different directions are varied. To reflect the anisotropy of rock mass clearly, the variation in the RQDt values with an optimal t value should be maximised. Therefore, the variation coefficient (Cv-RQD) and anisotropy index of jointing degree (AIjd) [24] were introduced to measure the dispersion of the RQDt values with the same threshold but at different directions. The Cv-RQD and AIjd are two different indices that share a common feature in that when the RQDt values in different directions are dispersed, both the Cv-RQD and AIjd values are relatively large, and vice versa. The Cv-RQD can be calculated by(11)Cv−RQD=σRQDμRQD,where σRQD and μRQD are the standard deviation and mean of the measured RQDt values in a model, respectively. The AIjd can be expressed as(12)AIjd=RQDtmaxRQD−tmaxRQDtmin100,where RQDtmax and RQDtmin are the maximum and minimum RQDt values, respectively.For the three-dimensional joint network model exampled in this section, the reasonablet values are 600 mm, 700 mm, 800 mm, and 900 mm. To select the optimal threshold, the Cv-RQD and AIjd of RQDt values with the four thresholds were calculated, as shown in Figure 7. The figure presents a tendency that the Cv-RQD and AIjd increase with the increasing threshold. Meanwhile, all the Cv-RQD values are greater than 0.1, indicating strong variation degrees. As the threshold is 900 mm, the Cv-RQD and AIjd values are the highest, implying that the RQDt values with a threshold of 900 mm can fully reflect the anisotropy of the rock mass structure. Thus, the optimal threshold is 900 mm.Figure 7
C
v-RQD and AIjd of the RQDt values with reasonable thresholds.The optimal thresholds of all models were determined, as shown in Table8. A review of Table 8 indicates that when the joint persistence is 3 m or more, the optimal t values first increase and subsequently decrease with the increase in joint spacing; for example, when the joint persistence remains unaltered as 40 m, the optimal t value increases from 200 mm to 800 mm and subsequently decreases to 100 mm. This can be attributed to two factors: (1) the wider the joint spacing is, the more integrated the rock mass is and the smaller the variation in the RQDt values is, and (2) with the increasing joint spacing, the variation in the RQDt values tends to be increasingly smaller regardless of the change in t value; particularly, when joint persistence is very wide or extremely wide, the RQDt values change little or not at all because all the corresponding Cv-RQD and AIjd values are extremely low. Hence, the RQDt values with a t value of 100 mm are enough to accurately describe those rock masses sparsely jointed or integrated. Additionally, when the joint spacing is unchanged, the change in joint persistence appears to have minor effects on the determination of the optimal t value; for example, when the joint spacing is fixed at 0.4 m, the optimal t values vary irregularly, and when the joint spacing is fixed as 6 m, the optimal t values do not change. It can be concluded that the major determinant factor for selecting the optimal t value is joint spacing.Table 8
Optimal thresholds of all hypothetical models.
Joint persistence (m)
Joint spacing (m)
Extremely wide
Very wide
Wide
Moderate
Close
Very close
Extremely close
0.02
0.04
0.13
0.4
1.3
4
6
40
Very high
200
200
300
500
800
100
100
20
High
100
300
200
200
900
100
100
10
Medium
100
100
100
300
100
100
100
3
Low
100
200
200
300
100
100
100
1
Very low
100
100
100
100
100
100
100


## 5.1. Correlation between the Standard Ratings of MBi and RQD

The MBi and RQD indices can be used to quantify the degree of rock mass jointing, and both of them divide such a degree into five categories, as shown in Tables 5 and 6. The correlation between standard ratings of MBi and RQD was assessed; this is shown in Figure 5. From this figure, a good linear relation was found between the standard ratings of MBi and RQD, which is expressed as(10)RQD=100−0.92MBi.Table 5
Standard ratings of MBi.
MBi
<7
7–27
27–55
55–85
≥85
Rating
I
II
III
IV
V
Description
Integrated
Relatively integrated
Poorly integrated
Relatively fractured
FracturedTable 6
Standard ratings of RQD.
RQD
90–100
75–90
50–75
25–50
<25
Rating
I
II
III
IV
V
Description
Very good
Good
Fair
Poor
Very poorFigure 5
Correlation between the standard ratings of MBi and RQD.The determination coefficient is 0.99, indicating a high fitting degree. Based on Eq. (10), theoretical RQD values can be derived.


## 5.2. Theoretical RQD Values

From Table4 and Eq. (10), the theoretical RQD values of the 35 models were determined, as shown in Table 7. The theoretical RQD value can be defined as an RQD value derived by the MBi, which is more compatible with the actual degree of rock mass jointing.Table 7
Theoretical RQD values (%) of all hypothetical models.
Joint persistence (m)
Joint spacing (m)
Extremely wide
Very wide
Wide
Moderate
Close
Very close
Extremely close
0.02
0.04
0.13
0.4
1.3
4
6
40
Very high
11.50
13.69
42.03
73.71
83.08
89.69
99.21
20
High
14.03
17.32
57.59
77.05
86.87
99.25
99.52
10
Medium
14.76
17.66
58.23
79.87
95.16
99.55
99.55
3
Low
16.04
18.78
58.42
92.07
99.45
99.55
99.55
1
Very low
16.94
20.34
82.39
99.45
99.55
99.55
99.55


## 5.3. Selection of Optimal Threshold of RQDt

The three-dimensional joint network model with a joint persistence of 20 m and joint spacing of 1.3 m was used as an example to demonstrate the procedure for selecting an optimal threshold of the RQDt. Based on the measurement described in Section 4.3, the (representative) RQDt values of different thresholds were calculated, as shown in Figure 6. The figure indicates that (1) when the threshold is 100 mm, the RQDt value is close to 100%, and when the threshold is 1000 mm, the RQDt value is approximately 70%, and (2) with the increase in t value, the RQDt values tend to be reduced.Figure 6
Generalised RQD values with different thresholds of the exampled model.As shown in Table4, the MBi value of this example model is 13.50%, which belongs to Class II (“relatively integrated” category). The corresponding rating of the theoretical RQD value also belongs to Class II (“good” category); that is, when the measured RQDt values are in the interval of 75% to 90%, the RQDt values can be regarded as reasonable, and the corresponding t values can be termed as reasonable thresholds.Figure6 shows that the reasonable thresholds are 600 mm, 700 mm, 800 mm, and 900 mm, and an optimal t value should be further selected. Owing to the anisotropy of the rock mass structure, the RQDt values in different directions are varied. To reflect the anisotropy of rock mass clearly, the variation in the RQDt values with an optimal t value should be maximised. Therefore, the variation coefficient (Cv-RQD) and anisotropy index of jointing degree (AIjd) [24] were introduced to measure the dispersion of the RQDt values with the same threshold but at different directions. The Cv-RQD and AIjd are two different indices that share a common feature in that when the RQDt values in different directions are dispersed, both the Cv-RQD and AIjd values are relatively large, and vice versa. The Cv-RQD can be calculated by(11)Cv−RQD=σRQDμRQD,where σRQD and μRQD are the standard deviation and mean of the measured RQDt values in a model, respectively. The AIjd can be expressed as(12)AIjd=RQDtmaxRQD−tmaxRQDtmin100,where RQDtmax and RQDtmin are the maximum and minimum RQDt values, respectively.For the three-dimensional joint network model exampled in this section, the reasonablet values are 600 mm, 700 mm, 800 mm, and 900 mm. To select the optimal threshold, the Cv-RQD and AIjd of RQDt values with the four thresholds were calculated, as shown in Figure 7. The figure presents a tendency that the Cv-RQD and AIjd increase with the increasing threshold. Meanwhile, all the Cv-RQD values are greater than 0.1, indicating strong variation degrees. As the threshold is 900 mm, the Cv-RQD and AIjd values are the highest, implying that the RQDt values with a threshold of 900 mm can fully reflect the anisotropy of the rock mass structure. Thus, the optimal threshold is 900 mm.Figure 7
C
v-RQD and AIjd of the RQDt values with reasonable thresholds.The optimal thresholds of all models were determined, as shown in Table8. A review of Table 8 indicates that when the joint persistence is 3 m or more, the optimal t values first increase and subsequently decrease with the increase in joint spacing; for example, when the joint persistence remains unaltered as 40 m, the optimal t value increases from 200 mm to 800 mm and subsequently decreases to 100 mm. This can be attributed to two factors: (1) the wider the joint spacing is, the more integrated the rock mass is and the smaller the variation in the RQDt values is, and (2) with the increasing joint spacing, the variation in the RQDt values tends to be increasingly smaller regardless of the change in t value; particularly, when joint persistence is very wide or extremely wide, the RQDt values change little or not at all because all the corresponding Cv-RQD and AIjd values are extremely low. Hence, the RQDt values with a t value of 100 mm are enough to accurately describe those rock masses sparsely jointed or integrated. Additionally, when the joint spacing is unchanged, the change in joint persistence appears to have minor effects on the determination of the optimal t value; for example, when the joint spacing is fixed at 0.4 m, the optimal t values vary irregularly, and when the joint spacing is fixed as 6 m, the optimal t values do not change. It can be concluded that the major determinant factor for selecting the optimal t value is joint spacing.Table 8
Optimal thresholds of all hypothetical models.
Joint persistence (m)
Joint spacing (m)
Extremely wide
Very wide
Wide
Moderate
Close
Very close
Extremely close
0.02
0.04
0.13
0.4
1.3
4
6
40
Very high
200
200
300
500
800
100
100
20
High
100
300
200
200
900
100
100
10
Medium
100
100
100
300
100
100
100
3
Low
100
200
200
300
100
100
100
1
Very low
100
100
100
100
100
100
100


## 6. Comparative Analysis of Traditional and Generalised RQDs

To evaluate the difference between traditional and generalised RQDs, the scatter plots of traditional and generalised RQDs and MBi values are shown in Figure 8, and the corresponding cumulative frequency curves are presented in Figure 9.Figure 8
Scatter plot of traditional and generalised RQDs and MBi values.Figure 9
Comparison between the cumulative frequency curves of traditional and generalised RQDs.As shown in Figure8, when the rock mass is integrated (i.e., the MBi value ranges from 0 to 7%), the generalised RQD values are almost consistent with the traditional RQD values. However, when the rock mass is in Class II (“relatively integrated” category) or lower, significant discrepancies between traditional and generalised RQD values appear, and the general tendency is that the generalised RQD values are less than the traditional RQD values. A model of y = 100 − x was adopted to fit the two kinds of data points in Figure 8; as shown, the fitting degree of the data points in generalised RQD vs. MBi is better than that of the data points in traditional RQD vs. MBi; especially in the MBi interval of 85% to 100%, it indicates fractured rock masses, but the traditional RQD values range from Classes III to V (“fair” to “very poor” category). This suggests that the traditional RQD values may mismatch with the MBi values that are three-dimensional quantifications of the rock mass jointing degree. Obviously, the generalised RQD values with optimal thresholds perform better in this aspect because the fitting degree of the generalised RQD and MBi values is rather high, and the RQD’s ability to differentiate rock mass structures is similar to that of the MBi.In Figure9, the cumulative frequency curve of the generalised RQD is below that of the traditional RQD; that is, the curve of the generalised RQD attains 100% later, implying that the ability of the generalised RQD to distinguish rock mass structures is superior, as shown in Figure 8: the data points (generalised RQD vs. MBi) distribute evenly on both sides of the fitting line of y = 100 − x. However, for the three-dimensional joint network models with similar MBi values, the acquired traditional RQD values range widely, as shown in Figure 8.


## 7. Engineering Practice

The investigation of the optimal threshold of generalised RQD was performed based on the joint data gathered on the dam rock mass in the Zipingpu hydropower station (Figure10), Sichuan, China. The analysis of the joint data identifies three joint sets, and their probabilistic distribution parameters are presented in Table 9. Based on Table 9, a three-dimensional joint network model of the dam rock mass was constructed, as shown in Figure 11. Using the procedure for determining the RQDt values described in Section 4.3, the generalised RQD values with different thresholds and directions were measured (Figure 12), and their means were calculated (Table 10). Table 10 shows that the traditional RQD value is 96.95%, which is in Class I (“good” category). The blocks inside the three-dimensional joint network model and their volumes were identified, and the MBi value of this model was determined to be 17%, which belongs to Class II (“relatively integrated” category).Figure 10
Zipingpu hydropower station in Sichuan, China.Table 9
Joint data of the dam rock mass.
Joint set no.
Joint number
Joint orientation
Trace length
d
3 (m−3)
Dip direction (°)
Dip angle (°)
Fisher’s coefficientκ
Distribution type
Average trace length
1
20
75
64
7.38
Lognormal
10
0.024
2
10
5
85
5.95
Lognormal
7
0.012
3
20
33
49
5.73
Lognormal
7
0.025Figure 11
Three-dimensional joint network model of the dam rock mass.Figure 12
Generalised RQD values (in different directions) with various thresholds of the dam rock mass.Table 10
Average generalised RQD values with different thresholds of the dam rock mass.
t (mm)
100
200
300
400
500
600
700
800
900
1000
RQDt
96.96
75.45
50.32
31.95
20.81
12.86
7.30
3.55
2.40
0.00As shown in Figure11, the traditional RQD values (in different directions) are almost in proximity to 100%, which cannot highlight the anisotropy of the rock mass structure; however, the increase in threshold resulted in an improvement; that is, in the polar coordinate (Figure 12), the contours that indicate the RQDt values with the same threshold but different directions are elliptical or bow-tie-shaped if the threshold is equal to or greater than 200 mm.Additionally, Table10 presents the average RQDt values with different thresholds; clearly, the traditional RQD value is slightly unreasonable and cannot correspond to the MBi value. Based on the method described in Section 5, the reasonable t value was determined to be 200 mm; therefore, an optimal threshold of 200 mm was obtained directly. Therefore, as shown in Table 10, the corresponding generalised RQD value is 75.45%, which is in Class II (“good” category) and consistent with the measured MBi value.


## 8. Conclusions

(1)
A total of 35 types of hypothetical three-dimensional joint network models were established, their generalised RQD values with different thresholds were measured, and a procedure for determining the optimal threshold of RQD was developed. This procedure was based on the MBi: if the measured generalised RQD values are consistent with the MBi with respect to the rating of the rock mass jointing degree, the corresponding thresholds are regarded as reasonable thresholds; subsequently, using the Cv-RQD and AIjd, an optimal threshold was determined.
(2)
The comparison between the traditional RQD values and the generalised RQD values with optimal thresholds indicated that (1) when the rock masses were integrated (rated in MBi), the measured traditional RQD values were similar to the generalised RQD values; (2) when the degrees of rock mass jointing were in Class II (“relatively integrated” category in MBi) or poorer, significant differences were found between the measured traditional and generalised RQD values; and (3) the traditional RQD may fail to differentiate rock masses possessing various structures, and the generalised RQD was superior (as shown in Figures 8 and 9).
(3)
The investigation of selecting an optimal threshold of RQDt was conducted based on an actual jointed rock mass, and the result indicated that the generalised RQD value with an optimal threshold could properly quantify the jointing degree of a real rock mass compared to MBi, when using the procedure developed in this study.



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*Source: 1340549-2019-01-10.xml*