# Nanodeserts: A Conjecture in Nanotechnology to Enhance Quasi-Photosynthetic CO2 Absorption

Authors: Wenfeng Wang; Xi Chen; Yifan Zhang; Jianjun Yu; Tianyi Ma; Zhihan Lv; Jing Zhang; Fanyu Zeng; Hui Zou
Journal: International Journal of Polymer Science
 (2016)

---

## Abstract

This paper advances “nanodeserts” as a conjecture on the possibility of developing the hierarchical structured polymeric nanomaterials for enhancing abiotic CO2 fixation in the soil-groundwater system beneath deserts (termed as quasi-photosynthetic CO2 absorption). Arid and semiarid deserts ecosystems approximately characterize one-third of the Earth’s land surface but play an unsung role in the carbon cycling, considering the huge potentials of such CO2 absorption to expand insights to the long-sought missing CO2 sink and the naturally unneglectable turbulence in temperature sensitivities of soil respiration it produced. “Nanodeserts” as a reconciled concept not only indicate a conjecture in nanotechnology to enhance quasi-photosynthetic CO2 absorption, but also aim to present to the desert researchers a better understanding of the footprints of abiotic CO2 transport, conversion, and assignment in the soil-groundwater system beneath deserts. Meanwhile, nanodeserts allow a stable temperature sensitivity of soil respiration in deserts by largely reducing the CO2 release above the deserts surface and highlighting the abiotic CO2 fixation beneath deserts. This may be no longer a novelty in the future.


---

## Body

## 1. Introduction

Attempts to account for the global atmospheric CO2 fluxes by quantifying CO2 sources and sinks have provided evidence of an unneglectable missing CO2 sink [1–3]. There are numerous studies that claimed to find the “missing sink,” but none of those claims has been widely accepted [4, 5]. Recently, the reports of carbon uptake by arid and semiarid desert ecosystems revealed rates of carbon uptake in many forests (i.e., the CO2 absorption rate is up to the photosynthetic absorption level) and focused research attention on arid and semiarid deserts ecosystems as the location of the long-sought “missing CO2 sink” [6–13], which was termed as quasi-photosynthetic CO2 absorption [6]. There is strong evidence suggesting that absorbed CO2 significantly contributes to the total soil CO2 flux [7–10]. Arid and semiarid deserts ecosystems approximately characterize one-third of the Earth’s land surface and play unsung role in the carbon cycling [9]. But where the absorbed CO2 has gone remains undetermined [11, 12]. A latest publication claimed that such absorption can be attributed to geochemical CO2 dissolution in saline aquifers beneath deserts [9], but the intensity of CO2 dissolution and absorption and the extent to which it modulates the global C balance are still a matter of controversy [9, 13, 14].Differential, difference, and dynamic equations are used for quantitative analysis in the engineering and natural sciences [15–18]. This suggests us trying to develop some differential equations to describe the dynamics of CO2 dissolution and absorption beneath deserts. Since absorbed CO2 is largely dissolved in saline aquifers [9, 10], the dynamic equations for groundwater dissolved in CO2 (DIC) are representative for both dissolution and absorption. Before this modeling work, the possible difficulties and uncertainties must be theoretically analyzed. Particularly, the quasi-photosynthetic CO2 absorption as a component of soil respiration in deserts is abound to produce turbulence in temperature sensitivities of soil respiration. The first estimate of the absorption intensity is very promising [12], but a subsequent challenge is how to reduce the CO2 release above the deserts surface and enhance the abiotic CO2 fixation beneath deserts. Otherwise, the abiotic CO2 fixation cannot be utilized [19–22]. Hierarchical structured polymeric materials, benefitting from nanotechnology enhancement, exhibited superior adsorption selectivity, high adsorption capacity, water tolerance, and low energy consumption with respect to physisorption, holding great promise for CO2 capture, and the capture can consequently, maybe, employed in the future utilization and enhancement of quasi-photosynthetic CO2 absorption beneath deserts. Considering the rapid development of nanotechnology and the wide applications hierarchical structured polymeric materials [23, 24], it can be conjectured that there are opportunities for the innovative design of self-assembling polymeric materials for the separation of aboveground CO2 release and underground CO2 fixation.This paper hypothesizes that in the future it is possible to develop some hierarchical structured polymeric materials to enhance quasi-photosynthetic CO2 absorption in deserts and advance “nanodeserts” as a conjecture in nanotechnology for modulating abiotic CO2 fixation in the soil-groundwater system. To illustrate the necessity for introducing this concept, the influences of quasi-photosynthetic CO2 absorption on temperature sensitivities of soil respiration are explicitly analyzed. A perspective Riccati Equation for the quasi-photosynthetic CO2 absorption in the soil-groundwater system is established, providing that the hierarchical structured polymeric materials physically reduce the soil surface CO2 release and enhance the abiotic CO2 fixation beneath nanodeserts and allow a stable temperature sensitivity of soil respiration in deserts and a reliable quantification of CO2 absorption intensity on regional and global nanodeserts.


## 2. Materials and Methods

### 2.1. Data Sources

“Nanodeserts” are a conjecture on the possibility of developing hierarchical structured polymeric materials to enhance abiotic CO2 fixation in the soil-groundwater system, where nanoporous materials are supposed to be able to largely reduce the CO2 release from the surface of the soil-groundwater system and enhance the quasi-photosynthetic CO2 absorption beneath nanodeserts. As a particular example, the higher-resolution SEM images of polyethylenimine nanofibers (Figures 1, 2, and 3; loading with BiOCl nanoparticles) were collected. The morphology was evaluated via scanning electron microscopy (SEM, Model SU8010, Hitachi Co., Ltd.).Figure 1
SEM image of polyethylenimine (PEI) nanofibers, loading with BiOCl nanoparticles.Figure 2
SEM image of polyethylenimine (PEI) nanofibers, loading with BiOCl nanoparticles.Figure 3
The SEM image of polyethylenimine (PEI) nanofibers.To highlight the necessity for this conjecture, the potential influences of the quasi-photosynthetic CO2 absorption on the temperature sensitivities (Q
10) of soil respiration (R
s) are basically analyzed. This work is based on the R
s values (both positive and negative values) and the corresponding θ
s, T
a, and T
s values collected from some previous publications, with the analysis of Q
10 of R
s to soil temperature at 5 cm depths (T
s) and air temperatures at 10 cm above the soil surface (T
a) at typical ecosystems along a gradient of soil alkalinity at 5 cm depths within the Manas River Basin [6, 12, 25].The Manas River Basin is located at the southern periphery of the Gurbantunggut Desert and in the hinterland of the Eurasian continent. Soils in this inland river basin bear typical physical and chemical characteristics, which are resulting from the soil water and soil salt transport during regional hydrological processes [26]. Almost 10 × 106 km2 of the hinterland of the Eurasian continent is arid and semiarid deserts ecosystems. The inland rivers carried large quantities of salt into the Eurasian continent, resulting in strong, complicated ecological responses and forming the world largest desert-oasis compound system, which allows us to carry experiments at typical saline desert sites and typical cropped farmland sites, respectively.


### 2.2. Calculation and Modeling

The size of the nanoparticles was statistically analyzed utilizing the DLS measurement (Figure2). Q
10 values used in the analysis were calculated using the following formula (for consistence, the negative values of R
s were not included in calculations of Q
10), using the simple model of R
s (the derivative of the exponential chemical reaction-temperature equation originally developed by Van’t Hoff) [27]:(1)
R
s
T
R
s
T
0
=
Q
10
T
-
T
0
/
10
,where R
s
T and R
s
T
0 are the R
s rates (μmol CO2m−2 s−1) at T and T
0, respectively.Developing hierarchical structured polymeric materials to enhance quasi-photosynthetic CO2 absorption beneath nanodeserts is very urgent and might draw much attention in the future. Hypothesizing that such nanoporous carbon materials were finally synthesized, the performance of CO2 absorption, conversion, and assignment beneath nanodeserts would be further studied. Therefore, it is also necessary to present a preliminary discussion of the coming modeling work when this interesting and innovative conjecture was demonstrated [28]. Riccati Equation is traditionally serving for the theory of transonic gas-dynamic flows and is hence employed in the present study to illustrate how to model CO2 footprints beneath nanodeserts.


## 2.1. Data Sources

“Nanodeserts” are a conjecture on the possibility of developing hierarchical structured polymeric materials to enhance abiotic CO2 fixation in the soil-groundwater system, where nanoporous materials are supposed to be able to largely reduce the CO2 release from the surface of the soil-groundwater system and enhance the quasi-photosynthetic CO2 absorption beneath nanodeserts. As a particular example, the higher-resolution SEM images of polyethylenimine nanofibers (Figures 1, 2, and 3; loading with BiOCl nanoparticles) were collected. The morphology was evaluated via scanning electron microscopy (SEM, Model SU8010, Hitachi Co., Ltd.).Figure 1
SEM image of polyethylenimine (PEI) nanofibers, loading with BiOCl nanoparticles.Figure 2
SEM image of polyethylenimine (PEI) nanofibers, loading with BiOCl nanoparticles.Figure 3
The SEM image of polyethylenimine (PEI) nanofibers.To highlight the necessity for this conjecture, the potential influences of the quasi-photosynthetic CO2 absorption on the temperature sensitivities (Q
10) of soil respiration (R
s) are basically analyzed. This work is based on the R
s values (both positive and negative values) and the corresponding θ
s, T
a, and T
s values collected from some previous publications, with the analysis of Q
10 of R
s to soil temperature at 5 cm depths (T
s) and air temperatures at 10 cm above the soil surface (T
a) at typical ecosystems along a gradient of soil alkalinity at 5 cm depths within the Manas River Basin [6, 12, 25].The Manas River Basin is located at the southern periphery of the Gurbantunggut Desert and in the hinterland of the Eurasian continent. Soils in this inland river basin bear typical physical and chemical characteristics, which are resulting from the soil water and soil salt transport during regional hydrological processes [26]. Almost 10 × 106 km2 of the hinterland of the Eurasian continent is arid and semiarid deserts ecosystems. The inland rivers carried large quantities of salt into the Eurasian continent, resulting in strong, complicated ecological responses and forming the world largest desert-oasis compound system, which allows us to carry experiments at typical saline desert sites and typical cropped farmland sites, respectively.


## 2.2. Calculation and Modeling

The size of the nanoparticles was statistically analyzed utilizing the DLS measurement (Figure2). Q
10 values used in the analysis were calculated using the following formula (for consistence, the negative values of R
s were not included in calculations of Q
10), using the simple model of R
s (the derivative of the exponential chemical reaction-temperature equation originally developed by Van’t Hoff) [27]:(1)
R
s
T
R
s
T
0
=
Q
10
T
-
T
0
/
10
,where R
s
T and R
s
T
0 are the R
s rates (μmol CO2m−2 s−1) at T and T
0, respectively.Developing hierarchical structured polymeric materials to enhance quasi-photosynthetic CO2 absorption beneath nanodeserts is very urgent and might draw much attention in the future. Hypothesizing that such nanoporous carbon materials were finally synthesized, the performance of CO2 absorption, conversion, and assignment beneath nanodeserts would be further studied. Therefore, it is also necessary to present a preliminary discussion of the coming modeling work when this interesting and innovative conjecture was demonstrated [28]. Riccati Equation is traditionally serving for the theory of transonic gas-dynamic flows and is hence employed in the present study to illustrate how to model CO2 footprints beneath nanodeserts.


## 3. The Major Results

### 3.1. Necessity to Introduce “Nanodeserts”

The necessity to introduce “nanodeserts” depends on whether wide utilization of quasi-photosynthetic CO2 absorption is feasible and reliable quantification of its overall importance is possible. Since it has been demonstrated that the current soil-groundwater system in arid and semiarid deserts ecosystems contributes both positive and negative CO2 fluxes and the magnitudes of these two fluxes components are almost the same [9–13], wide utilization of quasi-photosynthetic CO2 absorption is infeasible unless nanodeserts are introduced. Considering the rapid development of nanotechnology and its applications in CO2 capture and storage technology [29–36], nanodeserts as an emerging technology may be no longer a novelty in the future since deserts are attracting more and more interest in the increasingly urbanized world [37–40]. Because the wide range of nanomaterials and the particle sizes provides optional sizes of nanoparticles in the fabrication of nanomaterials (Figure 1), we can conjecture that there is an optimal size of nanoparticles to largely reduce CO2 release and meanwhile enhance the abiotic CO2 dissolution and fixation beneath nanodeserts.The turbulence inQ
10 values is evident. Quasi-photosynthetic CO2 absorption was demonstrated to have significant influences on temperature sensitivities (Q
10) of soil respiration (R
s), which highlight the necessity to introduce “nanodeserts.” Using positive R
s values, Q
10 was calculated by the relative change in R
s with each 10°C increase of T
s in the saline desert and cropped farmland largely fell into [
1
,
2
] and [
1
,
3
], respectively, while calculated Q
10 by the relative change in R
s with 10°C increases of T
a largely fell into [
3
,
13
] and [
2
,
4
], respectively. The mean Q
10 value of R
s to T
a (Q
10 = 4.88) was almost three times the mean Q
10 value of R
s to T
s (Q
10 = 1.66), implying that R
s in the alkaline land was much more sensitive to T
a than to T
s. The mean Q
10 value of R
s to T
a in the desert (Q
10 = 6.83) was more than the mean Q
10 value of R
s to T
a in the farmland (Q
10 = 2.95), implying that R
s in the desert was more sensitive to T
a than R
s in the farmland. However, R
s in the desert was less sensitive to T
s (with the mean Q
10 = 1.33) than R
s in the farmland (with the mean Q
10 = 1.98). Although those negative R
s were excluded and only the positive values were used in the calculations of Q
10, their significant influences on the response of R
s to T
s still existed. Additionally, the calculated Q
10 uniformly decreased with temperature (T = T
s or T
a) at both sites. This indicated that the variations of Q
10 with temperature in alkaline lands were not different from that in other terrestrial ecosystems (Figure 4).Figure 4
Responses of the temperature sensitivity (Q
10) to soil temperature at 5 cm depth (T
s) and air temperature 10 cm above the soil surface (T
a) in saline desert (a, c) and cropped farmland (b, d) and the responses of Q
10 to T
s and T
a when taking the saline desert and cropped farmland data together (e, f).
(a)
(b)
(c)
(d)
(e)
(f)Such turbulence inQ
10 values majorly resulted from the alternatively appearing positive and negative R
s. It is therefore essentially necessary to introduce “nanodeserts” as a conjecture on the possibility of developing hierarchical structured polymeric materials to largely reduce the CO2 release from the surface of the soil-groundwater system and enhance the quasi-photosynthetic CO2 absorption beneath nanodeserts by nanoporous modulation of the abiotic CO2 fixation in the soil-groundwater system. A series of polymers are suitable for nanodeserts working in the future and the chemical structure of polymer specially used for illustration here. The chemisorption of CO2 via amine-based materials is an efficient approach to reduce the greenhouse gas emission. In particular, polyethylenimine (PEI) impregnated materials exhibit superior adsorption selectivity, high adsorption capacity, water tolerance, and low energy consumption with respect to physisorption, holding great promise for CO2 capture (Figure 5).Figure 5
The chemical structure of polyethylenimine (PEI).


### 3.2. CO2 Footprints beneath Nanodeserts

Nanodeserts equipped with hierarchical structured polymeric materials can largely reduce the CO2 release from the surface of the soil-groundwater system and enhance the quasi-photosynthetic CO2 absorption beneath nanodeserts by nanoporous modulation of the abiotic CO2 fixation in the soil-groundwater system, which not only allows a stable temperature sensitivity (Q
10) beneath CO2 absorption and dissolution in the soil-groundwater system, but also makes it easy for deserts researchers to predict the CO2 footprints beneath nanodeserts. Despite the wide applications of hierarchical structured polymers [41–46], they are slightly associated to modulate the carbon cycle in deserts and so it is difficult to provide the quantification data of polymer used for CO2 absorption and the efficiency of CO2 fixation beneath deserts. This is really a challenge. At current stage, we can only present a first approach to quantification data of polymer used for CO2 absorption and the efficiency of CO2 fixation beneath deserts based on the parameter of CO2 content, power of visible-light for photocatalysis they used for calculation and modeling. Here is a specific example to explain how to carry out and evaluate the CO2 capture on polyethylenimine in future investigations. As an illustrating example, the CO2 adsorption-desorption isotherms were measured at 298 K and 308 K at low pressure (1 bar) using a Model Belsorp Max instrument (BEL Japan, Inc.). A volumetric measurement method was used to obtain the CO2 adsorption capacity. Before measurement, the samples were degassed for 10 h at 200°C until the residual pressure fell below 0.01 kPa and then cooled to room temperature. Photocatalytic activities of the as-prepared samples were estimated by the degradation rate of RhB under a Solar Simulator (Sun 2000, ABET) with a 440 nm cutoff filter (Figures 6 and 7).Figure 6
Effect of CO2 capture of impregnated-graphite oxide by polyethylenimine.Figure 7
A conceptual mechanism about the graphene oxide/BiOCl heterostructured nanofibers (the specified example in this study) for visible-light photocatalytic enhancements of CO2 fixation.To predict CO2 footprints beneath “nanodeserts,” first we establish a mathematical equation to describe the dynamics of CO2 in the groundwater-soil system beneath hypothetically built “nanodeserts.” Suppose that CO2 absorption per square-meter alkaline soils was finally dissolved in the groundwater of volume V. Let D
0 be the initial amount of DIC at t
0 and the growth rate of DIC is r. Ignoring groundwater flows and the restricting effect of current DIC, it is straight that (2)
d
D
1
t
d
t
=
D
0
·
r
t
-
t
0
,where D
1
t represents the one-dimension groundwater DIC dynamics.Noting thatD
1
0
=
D
0, the analytic solution of (2) is D
1
t
=
D
0
·
e
r
t
-
t
0.Now take into account groundwater flows. It is natural to provide that outflow = inflow, with volumeQ. Because such flows are very slow, assume that groundwater flows out after the inflow is uniformly mixed with the groundwater unit V. The quality conversation law implies(3)
D
2
t
+
Δ
t
-
D
2
t
=
Q
p
Δ
t
+
∫
t
t
+
Δ
t
r
D
2
t
-
Q
D
2
t
V
+
Q
d
t
,where p is DIC proportion in the inflows (hypothesized as a constant).Simplifying and taking the limitΔ
t
→
0, it implies(4)
d
D
2
t
d
t
=
Q
p
-
Q
V
+
Q
-
r
D
2
t
.Noting thatD
2
(
0
)
=
D
0, the analytic solution of (2) is(5)
D
2
t
=
Q
p
V
+
Q
Q
-
r
V
+
Q
-
D
0
-
Q
p
V
+
Q
Q
-
r
V
+
Q
e
r
-
Q
/
V
+
Q
t
,where D
2
t represents the two-dimension groundwater DIC dynamics.Finally take into account both the groundwater flows and the restricting effect of current DIC. The quality conversation law implies(6)
D
3
t
+
Δ
t
-
D
3
t
=
Q
p
Δ
t
+
∫
t
t
+
Δ
t
r
R
-
λ
D
3
t
D
3
t
-
Q
D
3
t
V
+
Q
d
t
,where R
-
λ
D
3
(
t
) determines the restricting effect of current DIC on r.Simplifying and taking the limitΔ
t
→
0, it implies (7)
d
D
3
t
d
t
=
Q
p
+
r
R
V
+
Q
-
Q
V
+
Q
D
3
t
-
λ
r
D
3
t
2
,where D
3
t represents the three-dimension groundwater DIC dynamics.Equation (7) is the famous Riccati Equation, where the parameters p, Q, r, R, and V are allowed to be changing with t [15–18]. Equations (2) and (4) are both simple forms of (7) and hence are also special forms of the famous Riccati Equation. Generally the Riccati Equation has no analytic solutions unless some assumptions are imposed. And it is better to provide a specific example to prove analytic solutions in certain conditions, which help to understand the full story of CO2 footprint and make chances for the subsequent quantitative analysis of quasi-photosynthetic CO2 absorption and fixation beneath nanodeserts (Figure 8).Figure 8
Hypothetical CO2 footprints beneath nanodeserts and the C sink kinetics in CO2 explosion.Suppose its analytic solutions by discussing that root of(8)
Q
p
+
r
R
V
+
Q
-
Q
V
+
Q
D
3
t
-
λ
r
D
3
t
2
=
0is zero; that is, 4
λ
r
p
Q
2
+
4
λ
r
p
V
+
r
R
-
1
Q
+
r
R
V is zero; then (8) has two same real roots, say d, and (7) is simplified as(9)
d
D
3
t
D
3
t
-
d
2
=
λ
r
d
t
,where the analytic solution can be obtained by D
3
0
=
D
0 and(10)
D
3
t
=
d
-
λ
r
t
+
c
,
c
is arbitrary constant
.CO2 footprints beneath nanodeserts can be therefore theoretically characterized. First, to note the auxiliary role of soil-groundwater metal ions in the CO2 footprints beneath nanodeserts is significant, which prepare chemical condition for the quasi-photosynthetic CO2 absorption beneath deserts (Figure 8). This is a key point of the whole story. Those metal ions come from the dissolution of soil salt during the discharge and recharge of groundwater. The percentages of those metal ions beneath deserts can be very different in different sites and the local extremes amount to 80 mg/L [47–56]. Second, the CO2 movements in the soil-groundwater system beneath nanodeserts are usually accompanied by the movements and sequestration of these metal ions. Finally, such accompanied movements present advantageous conditions for geochemical processes and therefore reconstruct CO2 footprints beneath nanodeserts. The above assumption and analytic solution (10) indicate that the quasi-photosynthetic CO2 absorption beneath deserts significantly contributed to the dynamic of the soil-groundwater CO2 concentration beneath deserts. In other words, the subterranean C pool and CO2 footprints would be reconstructed in next centuries when/if the quasi-photosynthetic CO2 absorption becoming the predominant processes was beneath “nanodeserts.”


## 3.1. Necessity to Introduce “Nanodeserts”

The necessity to introduce “nanodeserts” depends on whether wide utilization of quasi-photosynthetic CO2 absorption is feasible and reliable quantification of its overall importance is possible. Since it has been demonstrated that the current soil-groundwater system in arid and semiarid deserts ecosystems contributes both positive and negative CO2 fluxes and the magnitudes of these two fluxes components are almost the same [9–13], wide utilization of quasi-photosynthetic CO2 absorption is infeasible unless nanodeserts are introduced. Considering the rapid development of nanotechnology and its applications in CO2 capture and storage technology [29–36], nanodeserts as an emerging technology may be no longer a novelty in the future since deserts are attracting more and more interest in the increasingly urbanized world [37–40]. Because the wide range of nanomaterials and the particle sizes provides optional sizes of nanoparticles in the fabrication of nanomaterials (Figure 1), we can conjecture that there is an optimal size of nanoparticles to largely reduce CO2 release and meanwhile enhance the abiotic CO2 dissolution and fixation beneath nanodeserts.The turbulence inQ
10 values is evident. Quasi-photosynthetic CO2 absorption was demonstrated to have significant influences on temperature sensitivities (Q
10) of soil respiration (R
s), which highlight the necessity to introduce “nanodeserts.” Using positive R
s values, Q
10 was calculated by the relative change in R
s with each 10°C increase of T
s in the saline desert and cropped farmland largely fell into [
1
,
2
] and [
1
,
3
], respectively, while calculated Q
10 by the relative change in R
s with 10°C increases of T
a largely fell into [
3
,
13
] and [
2
,
4
], respectively. The mean Q
10 value of R
s to T
a (Q
10 = 4.88) was almost three times the mean Q
10 value of R
s to T
s (Q
10 = 1.66), implying that R
s in the alkaline land was much more sensitive to T
a than to T
s. The mean Q
10 value of R
s to T
a in the desert (Q
10 = 6.83) was more than the mean Q
10 value of R
s to T
a in the farmland (Q
10 = 2.95), implying that R
s in the desert was more sensitive to T
a than R
s in the farmland. However, R
s in the desert was less sensitive to T
s (with the mean Q
10 = 1.33) than R
s in the farmland (with the mean Q
10 = 1.98). Although those negative R
s were excluded and only the positive values were used in the calculations of Q
10, their significant influences on the response of R
s to T
s still existed. Additionally, the calculated Q
10 uniformly decreased with temperature (T = T
s or T
a) at both sites. This indicated that the variations of Q
10 with temperature in alkaline lands were not different from that in other terrestrial ecosystems (Figure 4).Figure 4
Responses of the temperature sensitivity (Q
10) to soil temperature at 5 cm depth (T
s) and air temperature 10 cm above the soil surface (T
a) in saline desert (a, c) and cropped farmland (b, d) and the responses of Q
10 to T
s and T
a when taking the saline desert and cropped farmland data together (e, f).
(a)
(b)
(c)
(d)
(e)
(f)Such turbulence inQ
10 values majorly resulted from the alternatively appearing positive and negative R
s. It is therefore essentially necessary to introduce “nanodeserts” as a conjecture on the possibility of developing hierarchical structured polymeric materials to largely reduce the CO2 release from the surface of the soil-groundwater system and enhance the quasi-photosynthetic CO2 absorption beneath nanodeserts by nanoporous modulation of the abiotic CO2 fixation in the soil-groundwater system. A series of polymers are suitable for nanodeserts working in the future and the chemical structure of polymer specially used for illustration here. The chemisorption of CO2 via amine-based materials is an efficient approach to reduce the greenhouse gas emission. In particular, polyethylenimine (PEI) impregnated materials exhibit superior adsorption selectivity, high adsorption capacity, water tolerance, and low energy consumption with respect to physisorption, holding great promise for CO2 capture (Figure 5).Figure 5
The chemical structure of polyethylenimine (PEI).


## 3.2. CO2 Footprints beneath Nanodeserts

Nanodeserts equipped with hierarchical structured polymeric materials can largely reduce the CO2 release from the surface of the soil-groundwater system and enhance the quasi-photosynthetic CO2 absorption beneath nanodeserts by nanoporous modulation of the abiotic CO2 fixation in the soil-groundwater system, which not only allows a stable temperature sensitivity (Q
10) beneath CO2 absorption and dissolution in the soil-groundwater system, but also makes it easy for deserts researchers to predict the CO2 footprints beneath nanodeserts. Despite the wide applications of hierarchical structured polymers [41–46], they are slightly associated to modulate the carbon cycle in deserts and so it is difficult to provide the quantification data of polymer used for CO2 absorption and the efficiency of CO2 fixation beneath deserts. This is really a challenge. At current stage, we can only present a first approach to quantification data of polymer used for CO2 absorption and the efficiency of CO2 fixation beneath deserts based on the parameter of CO2 content, power of visible-light for photocatalysis they used for calculation and modeling. Here is a specific example to explain how to carry out and evaluate the CO2 capture on polyethylenimine in future investigations. As an illustrating example, the CO2 adsorption-desorption isotherms were measured at 298 K and 308 K at low pressure (1 bar) using a Model Belsorp Max instrument (BEL Japan, Inc.). A volumetric measurement method was used to obtain the CO2 adsorption capacity. Before measurement, the samples were degassed for 10 h at 200°C until the residual pressure fell below 0.01 kPa and then cooled to room temperature. Photocatalytic activities of the as-prepared samples were estimated by the degradation rate of RhB under a Solar Simulator (Sun 2000, ABET) with a 440 nm cutoff filter (Figures 6 and 7).Figure 6
Effect of CO2 capture of impregnated-graphite oxide by polyethylenimine.Figure 7
A conceptual mechanism about the graphene oxide/BiOCl heterostructured nanofibers (the specified example in this study) for visible-light photocatalytic enhancements of CO2 fixation.To predict CO2 footprints beneath “nanodeserts,” first we establish a mathematical equation to describe the dynamics of CO2 in the groundwater-soil system beneath hypothetically built “nanodeserts.” Suppose that CO2 absorption per square-meter alkaline soils was finally dissolved in the groundwater of volume V. Let D
0 be the initial amount of DIC at t
0 and the growth rate of DIC is r. Ignoring groundwater flows and the restricting effect of current DIC, it is straight that (2)
d
D
1
t
d
t
=
D
0
·
r
t
-
t
0
,where D
1
t represents the one-dimension groundwater DIC dynamics.Noting thatD
1
0
=
D
0, the analytic solution of (2) is D
1
t
=
D
0
·
e
r
t
-
t
0.Now take into account groundwater flows. It is natural to provide that outflow = inflow, with volumeQ. Because such flows are very slow, assume that groundwater flows out after the inflow is uniformly mixed with the groundwater unit V. The quality conversation law implies(3)
D
2
t
+
Δ
t
-
D
2
t
=
Q
p
Δ
t
+
∫
t
t
+
Δ
t
r
D
2
t
-
Q
D
2
t
V
+
Q
d
t
,where p is DIC proportion in the inflows (hypothesized as a constant).Simplifying and taking the limitΔ
t
→
0, it implies(4)
d
D
2
t
d
t
=
Q
p
-
Q
V
+
Q
-
r
D
2
t
.Noting thatD
2
(
0
)
=
D
0, the analytic solution of (2) is(5)
D
2
t
=
Q
p
V
+
Q
Q
-
r
V
+
Q
-
D
0
-
Q
p
V
+
Q
Q
-
r
V
+
Q
e
r
-
Q
/
V
+
Q
t
,where D
2
t represents the two-dimension groundwater DIC dynamics.Finally take into account both the groundwater flows and the restricting effect of current DIC. The quality conversation law implies(6)
D
3
t
+
Δ
t
-
D
3
t
=
Q
p
Δ
t
+
∫
t
t
+
Δ
t
r
R
-
λ
D
3
t
D
3
t
-
Q
D
3
t
V
+
Q
d
t
,where R
-
λ
D
3
(
t
) determines the restricting effect of current DIC on r.Simplifying and taking the limitΔ
t
→
0, it implies (7)
d
D
3
t
d
t
=
Q
p
+
r
R
V
+
Q
-
Q
V
+
Q
D
3
t
-
λ
r
D
3
t
2
,where D
3
t represents the three-dimension groundwater DIC dynamics.Equation (7) is the famous Riccati Equation, where the parameters p, Q, r, R, and V are allowed to be changing with t [15–18]. Equations (2) and (4) are both simple forms of (7) and hence are also special forms of the famous Riccati Equation. Generally the Riccati Equation has no analytic solutions unless some assumptions are imposed. And it is better to provide a specific example to prove analytic solutions in certain conditions, which help to understand the full story of CO2 footprint and make chances for the subsequent quantitative analysis of quasi-photosynthetic CO2 absorption and fixation beneath nanodeserts (Figure 8).Figure 8
Hypothetical CO2 footprints beneath nanodeserts and the C sink kinetics in CO2 explosion.Suppose its analytic solutions by discussing that root of(8)
Q
p
+
r
R
V
+
Q
-
Q
V
+
Q
D
3
t
-
λ
r
D
3
t
2
=
0is zero; that is, 4
λ
r
p
Q
2
+
4
λ
r
p
V
+
r
R
-
1
Q
+
r
R
V is zero; then (8) has two same real roots, say d, and (7) is simplified as(9)
d
D
3
t
D
3
t
-
d
2
=
λ
r
d
t
,where the analytic solution can be obtained by D
3
0
=
D
0 and(10)
D
3
t
=
d
-
λ
r
t
+
c
,
c
is arbitrary constant
.CO2 footprints beneath nanodeserts can be therefore theoretically characterized. First, to note the auxiliary role of soil-groundwater metal ions in the CO2 footprints beneath nanodeserts is significant, which prepare chemical condition for the quasi-photosynthetic CO2 absorption beneath deserts (Figure 8). This is a key point of the whole story. Those metal ions come from the dissolution of soil salt during the discharge and recharge of groundwater. The percentages of those metal ions beneath deserts can be very different in different sites and the local extremes amount to 80 mg/L [47–56]. Second, the CO2 movements in the soil-groundwater system beneath nanodeserts are usually accompanied by the movements and sequestration of these metal ions. Finally, such accompanied movements present advantageous conditions for geochemical processes and therefore reconstruct CO2 footprints beneath nanodeserts. The above assumption and analytic solution (10) indicate that the quasi-photosynthetic CO2 absorption beneath deserts significantly contributed to the dynamic of the soil-groundwater CO2 concentration beneath deserts. In other words, the subterranean C pool and CO2 footprints would be reconstructed in next centuries when/if the quasi-photosynthetic CO2 absorption becoming the predominant processes was beneath “nanodeserts.”


## 4. Discussion

In subsequent studies, the diverse kinds of hierarchical structured nanoporous materials should be synthesized as a set of microporous nanomaterials with small pore size and their CO2 sorption performance should be mechanically analyzed. The performance of CO2 absorption by the hierarchical structured polymeric nanomaterials needs to be systematically investigated to find the critical pore size to enhance the CO2 uptake according to the arithmetic method proposed in subsequent studies. Moreover, the exact mechanisms about the heterostructured nanofibers for visible-light photocatalytic enhancements and full utilization of the solar thermal sources above nanodeserts are also worthy of further investigations [57–60].In the present study it is indicated that it is the micropores with pore size smaller than a necessary pore size for soil CO2 release that play a crucial role in such abiotic CO2 adsorption. Such efforts are practical considering the wide applications of the hierarchical structured polymers and the nanomaterials. The pore structure and surface chemical properties of these prepared nanomaterials should be symmetrically studied by using different kinds of testing methods. Additionally, the DLS was used to measure the size of the nanoparticles in the present study since the size of the nanoparticles had been decorated on the PEI fibers. Considering the size of the particles is important for photocatalytic performance [61], it is very important to employ the DLS to measure the size distribution of the nanoparticles. Nevertheless, when measuring the diameter or the length of the PEI nanofiber, other suitable methods must be additionally employed since it is not appropriate to use DLS to measure such size of the fiber.At the current stage it is impossible to obtain a reliable quantification of the CO2 adsorption capacity, but a preliminary approach can be concluded from Figures 6 and 7. One can get detailed information from Figures 6 and 7, respectively. In Figure 6, it is highlighted that chemisorption of CO2 via amine-based solid adsorbents is another efficient approach to reduce the greenhouse gas emission [62]. In particular, polyethylenimine (PEI) impregnated materials exhibit superior adsorption selectivity, high adsorption capacity, water tolerance, and low energy consumption with respect to physisorption, holding great promise for CO2 capture [63]. Nevertheless, the low thermal conductivity of PEI coupled with high adsorption heat (Δ
H) of chemisorption commonly generates overheating of these adsorbents during the CO2 capture. This unavoidably leads to partial degradation of PEI, poor cycle stability, and even safety problems. Therefore, the development of a suitable material with high CO2 adsorption capacity, superior adsorption selectivity, and excellent cycle performance remains a major challenge. In Figure 6, the GO sheets can serve as an efficient carrier support for PEI via a nanocasting technology. Such features are favorable for the efficient diffusion and adsorption of CO2 as well as the rapid thermal transfer. As for Figure 7, PEI nanofibers were prepared by electrospinning so that the graphene oxide/BiOCl heterostructured PEI nanofibers can be synthesized through in situ method. As well known, harmful chemical compounds have become the main cause of water pollution. For instance, organic dyes are often discharged with wastewater into the local environment without adequate treatment. Although the preparation of graphene-based composite hydrogels for photocatalyst has been previously reported [64, 65], recovering the photocatalyst after waste water purification has been a challenging issue. Thus, polymer-based photocatalyst nanocomposites have been attracting more interest due to their advantages for photocatalyst recovery. Exactly, the formation of graphene oxide/BiOCl heterostructured PEI nanofibers using an in situ reduction approach has been stated in the present study. Interestingly, this composite hydrogel matrix can be further utilized as highly efficient catalyst for wastewater treatment.Furthermore, the Riccati Equation presented in the present studies demands further investigations by the mathematicians who are interested in this conjecture and are able to make contributions. Therefore, the analysis of qualitative properties of solutions to Riccati Equation is crucial for understanding the CO2 absorption, offering some cautionary notes for interpretations based on first principles for CO2 capture at ecosystem level and large-scale applications, which is also a future research priority.


## 5. Conclusion

“Nanodeserts” as a reconciled concept not only indicate a conjecture in nanotechnology to enhance quasi-photosynthetic CO2 absorption, but also aim to present to desert researchers a better understanding of the footprints of abiotic CO2 transport, conversion, and assignment in the soil-groundwater system beneath deserts. Meanwhile, nanodeserts allow a stable temperature sensitivity of soil respiration in deserts by largely reducing the CO2 release above the deserts surface and highlight the abiotic CO2 fixation beneath deserts. When/if the dream is realized, it is not difficult then to widely utilize the quasi-photosynthetic CO2 absorption in the soil-groundwater system and present further explicit modeling results towards a reliable quantification of the quasi-photosynthetic CO2 absorption beneath nanodeserts. This may be no longer a novelty in the future since deserts are attracting more and more interest in the increasingly urbanized world.



---

*Source: 5027879-2016-07-26.xml*