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First-principles calculation of adsorption of shale gas on CaCO3 (100) surfaces

Abstract

Background

To demonstrate the adsorption strength of shale gas to calcium carbonate in shale matrix, the adsorption of shale gas on CaCO3 (100) surfaces was studied using the first-principles method, which is based on the density functional theory (DFT).

Methods

The structures and electronic properties of CH4, C2H6, CO2 and N2 molecules were calculated by the generalized gradient approximation (GGA), for a coverage of 1 monolayer (ML). Under the same conditions, the density of states (DOS) of CaCO3 (100) surfaces before and after the adsorption of shale gas molecules at high-symmetry adsorption sites were compared.

Results

The results showed that the adsorption energies of CH4, C2H6, CO2 and N2 on CaCO3 (100) surfaces were between 0.2683 eV and -0.7388 eV. When a CH4 molecule was adsorbed at a hollow site and its 2 hydrogen atoms were parallel to the long diagonal (H3) on the CaCO3 (100) surface, it had the most stable adsorption, and the adsorption energy was only -0.4160 eV. The change of adsorption energy of CH4 was no more than 0.0535 eV. Compared with the DOS distribution of CH4 before adsorption, it shifted to the left overall after adsorption. At the same time, the partial density of states (PDOS) curves of CaCO3 (100) surfaces before and after adsorption basically overlapped.

Conclusions

This work showed that the adsorption effect of shale gas on calcium carbonate is very weak, and the adsorption is physisorption at the molecular level.

J Appl Biomater Funct Mater 2017; 15(Suppl. 1): e45 - e51

Article Type: ORIGINAL RESEARCH ARTICLE

DOI:10.5301/jabfm.5000352

OPEN ACCESS ARTICLE

Authors

Qiang Luo, Yikun Pan, Ping Guo, Zhouhua Wang, Na Wei, Pengfei Sun, Yuxiao Liu

Article History

Disclosures

Financial support: This work was supported by the Young Scientists Fund of the National Natural Science Foundation of China (grant no. 51204141), the Major Program of the National Natural Science Foundation of China (grant no. 51374179), the Southwest Petroleum University Foundation (grant no. 2014QHS009, 2015JXYJ-07) and the Open Research Fund of the Computational Physics Key Laboratory of Sichuan Province (grant no. JSWL2014KF03).
Conflict of interest: The authors declare they have no conflicts of interest.

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Introduction

Shale gas, as one of the global unconventional natural gases, has received extensive attention around the world. The United States and Canada have achieved commercial exploitation of shale gas with good results. China has done a lot of work with respect to shale gas research status, reservoiring mechanisms and favorable-area evaluation, but the study of the adsorption of shale gas was only just initiated in recent years (1, 2). The development from conventional oil and gas fields to shale gas fields actually reflects the scale transition from micron to nanometer, and macroscopic breakthroughs have become increasingly dependent on microscopic studies. Therefore, it becomes particularly important to improve our microscopic understanding by using new theories and methods (3). Moreover, the study of shale gas molecule adsorption on shale substrate surfaces helps to understand the occurrence of shale gas, to assess the gas adsorption capacity quantitatively, to explore the correlation of adsorption properties and mineral composition and to evaluate the quantity of shale gas as a natural resource.

Shale gas is generally dry and mainly consists of CH4, C2H6, CO2, N2 and other components, with the content of CH4 up to more than 95% (4, 5). The adsorption of shale gas and shale has been investigated through a large number of experimental and theoretical studies (6-7-8-9-10-11-12). Most of the theoretical studies show that shale gas is mainly absorbed on the surface of the kerogen and clay minerals, and is almost not adsorbed at all on the surface of calcium carbonate (13-14-15-16). Ji et al (5) studied methane adsorption on clay minerals of different sources and origins by isothermal adsorption experiment. The results showed that different types of clay minerals had evidently different gas adsorption capacities. However, there is no direct evidence of very weak gas adsorption on the surface of calcium carbonate.

At the same time, the first-principles method is used to study the adsorption of gas molecules on material surface (17-18-19-20-21-22-23-24-25-26), but there are few reports about the adsorption of gas molecules on the surface of calcium carbonate. Based on density functional theory with solid-state nuclear magnetic resonance (SS-NMR) calculations, Bevilaqua et al (27) simulated the adsorption of hydrocarbon molecules on calcite surface (CaCO3(10Ī4)), but the adsorption of shale gas was not studied. In this paper, we adopted the first-principles method based on density functional theory (DFT) to study the adsorption stability of shale gas and its components at different high-symmetry positions on CaCO3 (100) surfaces. By analyzing the adsorption results, such as the adsorption energy of gas molecules and the structure and electronic properties of CaCO3 (100) surfaces, we uncovered the microscopic mechanisms of shale gas adsorption on CaCO3 surfaces.

Methods

Computational methods

Based on the first-principle method of DFT (28, 29), the ground state geometries and electronic properties of CH4, C2H6, CO2 and N2 molecules adsorbed on CaCO3 (100) were calculated using the Cambridge Sequential Total Energy Package (CASTEP) module in Materials Studio. Within the generalized gradient approximation (GGA), Perdew-Burke-Ernzerhof (PBE) (30) exchange correlation functionals combined with ultrasoft pseudopotentials were used in the calculations. The value of plane wave cutoff energy was 300 eV. The K point grid (31) size was 3 × 1 × 1. Self-consistent field calculations were performed with a convergence criterion of 2.0 × 10-6 eV on single atom energy. The convergence of parameters was tested for each supercell. The Broyden-Fletcher-Goldfarb-Shanno (BFGS) optimization algorithm proposed by Broyden, was used in the structure optimization (32-33-34-35).

Structural models

In this paper, the P (1 × 1) periodic supercell is used as the initial surface. Under the coverage of 1 monolayer (ML), the adsorption of CH4, C2H6, CO2 and N2 on the surface was theoretically studied for each. First, an optimized CaCO3 unit cell (Fig. 1) was cleaved for a (100) surface. Then a vacuum layer of 2-nm thickness was constructed to simulate the CaCO3 (100) surface (Fig. 2). Finally, the CaCO3 (100) structure was optimized. We focused on shale gas molecule adsorption on CaCO3 (100) surfaces. Therefore, in the structural optimization computation, the position of oxygen atoms was kept on the surface layer, and the number of adsorbed of shale gas molecules was variable, whereas the atoms of the non–surface layer were immobilized. We adopted such a setting to simulate the adsorption of CaCO3 on shale gas molecules in order to reduce the number of calculations and to exclude the effect of substrate thickness. The initial lattice constant of calcium carbonate was an experimental value for, a = 0.499 nm, c = 1.7061 nm (36). After optimization, the lattice constant was a = 0.499 nm, c = 1.7060 nm. The gas molecules were added on the CaCO3 (100) surface to a height of 0.5 nm.

Structural model of an optimized CaCO3 cell with oxygen atoms (red), calcium atoms (green) and carbon atoms (gray).

Structural model of a CaCO3 (100) surface supercell with vacuum layer.

In the structural model of CaCO3 (100) surface supercell, there were 3 possible high-symmetry adsorption sites, the top (T), the bridge (B) and the hollow (H) part, in a parallelogram consisting of 4 oxygen atoms of surface (Fig. 3). The bridges included the short-side bridge (B1) and the long-side bridge (B2).

High-symmetry adsorption site on p (1 × 1) CaCO3 (100) surface: top (T), short-side bridge (B1), long-side bridge (B2) and hollow (H).

Due to the nature of parallelogram geometry, each gas molecule had 4 types of adsorption forms in the CaCO3 (100) surface H site. As shown in Figure 4 H1 was parallel to the short edge of the parallelogram, H2 was parallel to the short diagonal, H3 was parallel to the long diagonal and H4 was parallel to the long edge. Similarly, T-type sites were denoted by T1, T2, T3 and T4, and B-type sites were mainly related to the situation in which the adsorption of gas molecules was parallel to the short edge or long edge, and were designated as B11, B14, B21 and B24. Therefore, taking all of the possibilities into account, each gas species of CH4, C2H6, CO2 and N2 had 12 adsorption modes on the CaCO3 (100) surface.

Adsorption directions of H site.

To analyze the adsorption stability of shale gas molecules on CaCO3 (100) surfaces, the adsorption energy of gas molecules on CaCO3 (100) surfaces was calculated. The total energy of the system before adsorption was obtained by calculating the energy of CaCO3 (100) surfaces and gas molecules. Then in the same way, the total energy of the system was calculated after adsorption. The equation to calculate the adsorption energy is given by

Δ E a d = E g a s + C a C O 3 ( E C a C O 3 +    E g a s )           Eq. [1]

where Egas+CaCO3 is the total energy of the system after gas adsorption, ECaCO3 is the energy of pure CaCO3 without the gas molecule, and Egas is the energy of the isolated shale gas molecule. The value of ∆Ead reflects the stability of the adsorption system. ∆Ead < 0 means that the energy of the system decreases after adsorption, and the gas molecules are adsorbed. The adsorption process is exothermic. ∆Ead > 0 means that the energy of the system increases, and the gas molecules cannot be adsorbed (37). A smaller value of ∆Ead indicates better stability of the adsorption system.

Results and discussion

Analysis of adsorption energy

Table I lists the adsorption energy of CH4, C2H6, CO2 and N2 molecules on CaCO3 (100) surfaces in the 12 adsorption modes. CH4, C2H6 and N2 molecules had negative ∆Ead, and the lowest adsorption energy was -0.4160 eV, -0.7388 eV and -0.1567 eV, respectively. The adsorption capacity of 3 kinds of gases on the surface of calcium carbonate follows the order of C2H6 > CH4 > N2. However, the ∆Ead of CO2 was positive, which means that CO2 molecule cannot be adsorbed on the surface of calcium carbonate. Therefore, the adsorption of CO2 is not discussed in the following.

Adsorption energy of CH4, C2H6, CO2 and N2 molecules on 12 types of adsorption sites on CaCO3 (100) surfaces

High-symmetry sites Adsorption energy (eV)
CH4 C2H6 CO2 N2
T1 = on the top site and parallel to the short edge of the parallelogram; T2 = on the top site and parallel to the short diagonal; T3 = on the top site and parallel to the long diagonal; T4 = on the top site and parallel to the long edge; B11 = on the short side bridge site and parallel to the short edge; B14 = on the short-side bridge site and parallel to the long edge; B21 = on the long-side bridge site and parallel to the short edge; B24 = on the long-side bridge site and parallel to the long edge; H1 = on the hollow site and parallel to the short edge of the parallelogram; H2 = on the hollow site and parallel to the short diagonal; H3 = on the hollow site and parallel to the long diagonal; H4 = on the hollow site and parallel to the long edge.
T1 -0.3886 -0.7087 0.1872 -0.0855
T2 -0.3625 -0.6933 0.1463 -0.1567
T3 -0.3676 -0.7260 0.1619 -0.1505
T4 -0.3855 -0.7022 0.1871 -0.1032
B11 -0.3967 -0.7382 0.1672 -0.0903
B14 -0.3721 -0.7388 0.2044 -0.1279
B21 -0.4034 -0.6370 0.1679 -0.0805
B24 -0.4085 -0.6211 0.2683 -0.1243
H1 -0.4080 -0.6214 0.1361 -0.0971
H2 -0.4107 -0.6849 0.1521 -0.1363
H3 -0.4160 -0.6592 0.1127 -0.1312
H4 -0.4137 -0.6286 0.2033 -0.1195

Since the percentage of CH4 is dominant in shale gas, the adsorption energy of CH4 molecular was compared for different adsorption sites to analyze the stability of shale gas molecules adsorbed on CaCO3 (100) surfaces, as shown in Figure 5. It can be seen that CH4 molecules had the lowest ∆Ead at the H3 site.

Bar chart of adsorption energy of CH4 at various adsorption sites on the CaCO3 (100) surface.

From the point of view of the quantity of adsorption energy, CH4 molecules had a minimum adsorption energy of -0.4160 eV on H3, which was the most stable adsorption structure among the 12 high-symmetry sites (Fig. 6). Therefore, it is relatively easier for CH4 molecules to be adsorbed on H3. When adsorbed on T2, CH4 molecules had a maximum energy of -0.3625 eV, which means that it was most difficult for T2 to adsorb CH4 molecules. Similarly, C2H6 molecules had their minimum adsorption energy and most stable adsorption structure at B14, which was the position for easiest adsorption. B24 had the maximum energy and the most unstable adsorption structure. At T2, N2 molecules had their minimum adsorption energy, and could be easily adsorbed at T2. B21 was the most difficult position to adsorb N2 molecules. The small absolute values of adsorption energy indicate very weak adsorption of CH4, C2H6 and N2 molecules on CaCO3 (100) surfaces.

Structural model of CH4 molecule adsorbed at H3 site on CaCO3 (100) surface.

In terms of the range of adsorption energies, the adsorption energy of CH4 at different sites ranged from -0.3625 eV to -0.4160 eV, with the largest difference being only 0.0535 eV. Besides, the largest differences of the adsorption energy ranges for C2H6 and N2 molecules were only 0.1177 eV and 0.0762 eV, respectively. The range of adsorption energies was very small, which indicates that the adsorption of each gas molecule at the high-symmetry sites on CaCO3 (100) surfaces was very similar, and the gas molecules tended to move on the calcium carbonate surfaces. By comparison, it is known that the mobility of CH4 is the strongest.

Analysis of physical structure

In Table II we can see that after CH4 molecules were adsorbed at H3 sites, the C-H bond length became 0.1097 nm, which is in good agreement with the experimentally spectroscopic data of 0.1086 ± 0.0001 nm (38). Compared with the value before adsorption, the bond length changed by 0.091%, and bond angle changed by 0.779%.

Changes of bond length and bond angle of CH4, C2H6 and N2 molecules on CaCO3 (100) surfaces after adsorption

Gas type Before adsorption After adsorption* Relative change
Bond length (nm) Bond angle(°) Bond length (nm) Bond angle (°) Bond length Bond angle
* Situation for the most stable adsorption position.
The bond lengths were C-H for CH4, C = C for C2H6, N ≡ N for N2.
The bond angles were C-H for CH4 and C2H6, N ≡ N for N2.
CH4 0.1098 109.483 0.1097 110.336 0.091% 0.779%
C2H6 0.1547 109.471 0.1525 107.938 1.422% 1.400%
N2 0.1146 180 0.1162 180 1.396% 0

Similarly, the physical structure was analyzed for C2H6 and N2 before and after adsorption. The relative changes were 1.422% and 1.400% for C=C bond length and H-C-H bond angle of C2H6, respectively. The N≡N bond length increased by 1.396% after N2 was adsorbed. It was found that the structures of CH4, C2H6 and N2 molecules showed negligible changes, so the adsorption effect was weak on the CaCO3 (100) surface.

Analysis of density of states

The CASTEP module can analyze the band structure, electronic density of states (DOS), optical properties, phonon dispersion relations, phonon DOS and stress before and after the optimization of the physical model. Here we mainly discuss the electronic DOS changes and their effect on adsorption. According to the analysis of the DOS changes for CH4, C2H6, N2 and CaCO3 (100) surfaces before and after adsorption, the interactions between shale gas molecules and CaCO3 (100) surface can be further understood.

In Figure 7 the DOS of CH4 before and after adsorption at H3 and T2 is compared. The black curve represents the electronic DOS before adsorption, the red curve represents the electronic DOS after adsorption at H3, and the blue curve represents the electronic DOS after adsorption at T2. The vertical dashed line at 0 eV indicates the Fermi level. It can be seen that whether adsorbed at H3 or T2, the electron DOS curves of CH4 molecules shifted to the left overall after adsorption. The adsorption energy decreased, and the electronic structure became more stable, which shows that the adsorption had a significant influence on the distribution of electron DOS of CH4 molecules. Besides, the DOS curve of H3 has 2 peaks, at -12.77 eV and -5.18 eV, which move to the left about 0.3 eV compared with those of T2 at -12.47 eV and -4.88 eV. It is thus proven that the adsorption of CH4 molecules on CaCO3 (100) surface high-symmetry sites is basically from the point of view of electronic structure, and has better mobility on the surface of the calcium carbonate.

Density of states (DOS) of CH4 molecules before and after adsorption at H3 site and T2 site. The black dotted line indicates the Fermi level.

Figure 8 shows the partial density of states (PDOS) of oxygen atoms in CaCO3 (100) surface before and after the adsorption of CH4 molecules at H3 under the coverage of 1 ML. The contribution of s electronic states and p electronic states to the total density of states in energy regions is different. When the energy is greater than -10 eV, the p electronic states (red curve) play a major role in the total electron density. When the energy is less than -10 eV, the s electronic states (blue curve) play a major role in the total electron density. Before adsorption, the s electronic states energy is mainly continuously distributed in the ranges of 0 eV to -9 eV and -17 eV to -24 eV, and there are 7 peaks in the 2 intervals. While p electronic states energy is mainly continuously distributed in the ranges of 2 eV to -9 eV and -17 eV to -24 eV, and there are 9 peaks in the 2 intervals. After adsorption, the PDOS of s electronic state of oxygen atoms basically coincides with that of the state before adsorption, as does that of the p Electronic State. This suggests that there is no chemical bond formed between CH4 molecules and the oxygen atoms on CaCO3 (100) surfaces. This indicates that the adsorption of CH4 on calcium carbonate surfaces is mainly affected by the Van Der Waals force, and it is physical adsorption. To better illustrate this point, we compared the DOS of CaCO3 (100) surfaces with the different shale gas molecules adsorbed, as shown in Figure 9.

Partial density of states (PDOS) and density of states (DOS) of oxygen atoms in CaCO3 (100) surface before and after the adsorption of CH4 molecules on the H3 site. (A) Before adsorption and (B) after adsorption.

Density of states (DOS) of oxygen atoms on CaCO3 (100) surface after the adsorption of CH4, C2H6 and N2 molecules at the most stable adsorption sites.

Figure 9 presents the DOS of CH4, C2H6 and N2 adsorbed on a CaCO3 (100) surface. We can see that the adsorption of different gas molecules on the CaCO3 (100) surface has similar effects on the electronic structure of the oxygen atom on the CaCO3 (100) surface. After adsorption, the 3 DOS curves almost overlap, indicating that C2H6 and N2 molecules have similar adsorption effects on oxygen atoms on the CaCO3 (100) surface to those of the CH4 molecule, and the adsorption of the 3 kinds of gas molecules on the CaCO3 (100) surface are physical.

Conclusions

Using the first-principle method based on DFT, we established adsorption models for CH4, C2H6, CO2 and N2 on CaCO3 (100) surfaces, and calculated the corresponding adsorption energies. The adsorption abilities of CH4, C2H6 and N2 molecules on the CaCO3 (100) surface were weak. CO2 molecules could not be adsorbed. The adsorption abilities of the different molecules were different. The adsorption ability of hydrocarbon gas was stronger than that of nonhydrocarbon gas, and the adsorption ability of C2H6 was stronger than that of CH4. In addition, the adsorption energy of different gas molecules varied over the range of sites and followed the order of CH4 <N2 <C2H6. The change of CH4 was the smallest, indicating the best mobility of CH4 molecules on the surface of calcium carbonate. This may be due to the fact that the methane molecule has the smallest relative molecular mass.

We also analyzed the electronic structures of the adsorption systems. After adsorption, the changes of geometric structures of the molecules were small and the electron DOS of atoms in the CaCO3 (100) surface was basically unchanged. The findings above show that the adsorption of shale gas molecules on the surface of calcium carbonate is physical.

Acknowledgements

The authors would like to acknowledge the assistance of A.P. Li P. Chen for English correction.

Disclosures

Financial support: This work was supported by the Young Scientists Fund of the National Natural Science Foundation of China (grant no. 51204141), the Major Program of the National Natural Science Foundation of China (grant no. 51374179), the Southwest Petroleum University Foundation (grant no. 2014QHS009, 2015JXYJ-07) and the Open Research Fund of the Computational Physics Key Laboratory of Sichuan Province (grant no. JSWL2014KF03).
Conflict of interest: The authors declare they have no conflicts of interest.
References
  • 1. Kong DT Ning ZF Yang F He B Zhao TY The characteristic of adsorption on shales and influence factor. Petrochem Ind Appl 2013 32 9 1 4 Google Scholar
  • 2. Ma YL Zhang DL Research status of shale reservoir adsorption mechanism and its influencing factors. Ground Water 2014 36 6 246 249 Google Scholar
  • 3. Gao LF Wang QQ Yin S Zheng LH Wang YY Li H Research of shale gas’ absorption. Sichuan Univ Arts Sci J 2014 24 2 60 64 Google Scholar
  • 4. Zeng QS Chen WK Dai WX Zhang YF Li Y Guo X Density functional theory study of CO and O2 adsorption on NiFeB2/TiO2 surface. Chin J Catal 2010 31 4 423 428 Google Scholar
  • 5. Ji LM Qiu JL Zhang TW Xia YQ Experiments on methane adsorption of common clay minerals in shale. Earth Sci J Chin Univ Geosci 2012 37 5 1043 1050 Google Scholar
  • 6. Luo XP Wu P Zhao JH Yang N Study advances on organic pores in organic matter-rich mud shale. J Chengdu Univ Technol 2015 42 1 50 59 Google Scholar
  • 7. Zhang H Zhu YM Xia XH Hu L Chen J Comparison and explanation of the absorptivity of organic matters and clay minerals in shales. J Chin Coal Soc 2013 38 5 812 816 Google Scholar
  • 8. Zhang XF Lu CX Zhang LY Liu Q Occurrences of shale gas and their petroleum geological significance. Adv Earth Sci 2010 25 6 597 604 Google Scholar
  • 9. Huang MZ The quantitative characterization of containing gas abilities in shale with different occurrence states: a case study of Shuangyang formation in Yitong Basin. Sci Technol Eng 2015 15 20 35 41 Google Scholar
  • 10. Wang R Zhang NS Liu XJ Wu XM Yan J Research progress of mechanism of adsorption and desorption of gas in shale. Sci Technol Eng 2013 13 19 5561 5567 Google Scholar
  • 11. Qajar A Daigle H Prodanović M Methane dual-site adsorption in organic-rich shale-gas and coalbed systems. Int J Coal Geol 2015 149 1 8 Google Scholar
  • 12. Fathi E Akkutlu YI Multi-component gas transport and adsorption effects during CO2 injection and enhanced shale gas recovery. Int J Coal Geol 2014 123 52 61 Google Scholar
  • 13. Curtis JB Fractured shale-gas systems. AAPG Bull 2002 86 11 1921 1938 Google Scholar
  • 14. Montgomery SL Jarvie DM Bowker KA Pollastro RM Mississippian Barnett shale, Fort Worth basin, north-central Texas: gas-shale play with multi-trillion cubic foot potential. AAPG Bull 2005 89 2 155 175 Google Scholar
  • 15. Chalmers GRL Bustin RM The organic matter distribution and methane capacity of the Lower Cretaceous strata of Northeastern British Columbia, Canada. Int J Coal Geol 2007 70 1-3 223 239 Google Scholar
  • 16. Ross DJK Bustin RM Shale gas potential of the Lower Jurassic Gordondale Member, northeastern British Columbia, Canada. Bull Can Pet Geol 2007 55 1 51 75 Google Scholar
  • 17. Yan CX Jiang QW Effects of atmospheric species and vacancy defect on electron transfer between diamond (001) surface and adlayer. Eur Phys J Appl Phys 2012 59 1 11303 Google Scholar
  • 18. Kuang XJ Wang XQ Liu GB A density functional theory study of carbon monoxide adsorption on platinum-doped gold clusters. Eur Phys J Appl Phys 2012 60 3 31301 Google Scholar
  • 19. Luo Q Tang B Zhang Z Ran ZL First principles calculation of adsorption for H2S on Fe (100) surface. Acta Phys Sin 2013 62 7 077101 Google Scholar
  • 20. He YB Jia JF Wu HS First-principles study of stability and electronic structure of N2H4 adsorption on NiFe (111) alloy surface. Acta Phys Sin 2015 64 20 203101 Google Scholar
  • 21. Brunsvold AL Garton DJ Minton TK Troya D Schatz GC Crossed beams and theoretical studies of the dynamics of hyperthermal collisions between Ar and ethane. J Chem Phys 2004 121 23 11702 11714 Google Scholar
  • 22. Nave S Tiwari AK Jackson B Methane dissociation and adsorption on Ni(111), Pt(111), Ni(100), Pt(100), and Pt(110)-(1 × 2): energetic study. J Chem Phys 2010 132 5 054705 Google Scholar
  • 23. Li P Liu ZZ Liu HX Liu DS Ge XW Density functional theory study of methane adsorption on Ni (110). J Inner Mongolia Norm Univ 2015 44 3 389 395 Google Scholar
  • 24. Atta-Fynn R Ray AK A first principles study of the adsorption and dissociation of CO2 on the δ–Pu (111) surface. Eur Phys J B 2009 70 2 171 184 Google Scholar
  • 25. Li L Cockayne E Williamson I Espinal L Wong-Ng W First-principles studies of carbon dioxide adsorption in cryptomelane/hollandite-type manganese dioxide. Chem Phys Lett 2013 580 120 125 Google Scholar
  • 26. Jiao Y Du AJ Zhu ZH Rudolph V Simth SC Adsorption of carbon dioxide and nitrogen on single-layer aluminum nitride nanostructures studied by density functional theory. J Phys Chem C 2010 114 17 7846 7849 Google Scholar
  • 27. Bevilaqua RC Rigo VA Veríssimo-Alves M Miranda CR NMR characterization of hydrocarbon adsorption on calcite surfaces: a first principles study. J Chem Phys 2014 141 20 204705 Google Scholar
  • 28. Hohenberg P Kohn W Inhomogeneous electron gas. Phys Rev 1964 136 3B B864 B871 Google Scholar
  • 29. Kohn W Sham LJ Self-consistent equations including exchange and correlation effects. Phys Rev 1965 140 4A 1133 1138 Google Scholar
  • 30. Perdew JP Burke K Ernzerhof M Generalized gradient approximation made simple. Phys Rev Lett 1996 77 18 3865 3868 Google Scholar
  • 31. Monkhorst HJ Pack JD Special points for Brillouin-zone integrations. Phys Rev B 1976 13 12 5188 5192 Google Scholar
  • 32. Broyden CG The convergence of a class of double-rank minimization algorithms 1: general considerations. J Inst Math Appl 1970 6 1 76 90 Google Scholar
  • 33. Fletcher R A new approach to variable metric algorithms. Comput J 1970 13 3 317 322 Google Scholar
  • 34. Goldfarb D A family of variable-metric methods derived by variational means. Math Comput 1970 24 109 23 26 Google Scholar
  • 35. Shanno DF Conditioning of quasi-Newton methods for function minimization. Math Comput 1970 24 111 647 656 Google Scholar
  • 36. Graf DL Crystallographic tables for the rhombohedral carbonates. Am Mineral 1961 46 11 1283 1316 Google Scholar
  • 37. Zhang H Liu SY Zhang GY eds. Landscape painting the chemisorption of quantum mechanics. Beijing, China: Science Press; 2004 215 217 Google Scholar
  • 38. Hammer B Hansen LB Norskov JK Improved adsorption energetics within density-functional theory using revised Perdew-Burke-Ernzerhof functional. Phys Rev B 1999 59 11 7413 7421 Google Scholar

Authors

Affiliations

  • School of Science, Southwest Petroleum University, Chengdu - PR China
  • State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu - PR China

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