Theoretical Studies on Defects of Kaolinite in Clays
HE Man-Chao1, FANG Zhi-Jie1, ZHANG Ping2
1State Key Laboratory of Deep Geomechanics and Underground Engineering, China University of Mining and Technology, Beijing 1000832Institute of Applied Physics and Computational Mathematics, Beijing 100088
Theoretical Studies on Defects of Kaolinite in Clays
HE Man-Chao1, FANG Zhi-Jie1, ZHANG Ping2
1State Key Laboratory of Deep Geomechanics and Underground Engineering, China University of Mining and Technology, Beijing 1000832Institute of Applied Physics and Computational Mathematics, Beijing 100088
摘要Using the first-principles methods, we study the formation energetics and charge doping properties of the extrinsic substitutional defects in kaolinite. Especially, we choose Be, Mg, Ca, Fe, Cr, Mn, Cu, Zn as extrinsic defects to substitute for Al atoms. By systematically calculating the impurity formation energies and transition energy levels, we find that all group-II defects introduce the relative shallow transition energy levels in kaolinite. Among them, MgAl has the shallowest transition energy level at 0.08eV above the valence band maximum. The transition-elemental defects FeAl, CrAl, and MnAl are found to have relative low formation energies, suggesting their easy formation in kaolinite under natural surrounding conditions. Our calculations show that the defects CuAl and ZnAl have the high formation energies and deep transition energy levels, which exclude the possibility of their formation in natural kaolinite.
Abstract:Using the first-principles methods, we study the formation energetics and charge doping properties of the extrinsic substitutional defects in kaolinite. Especially, we choose Be, Mg, Ca, Fe, Cr, Mn, Cu, Zn as extrinsic defects to substitute for Al atoms. By systematically calculating the impurity formation energies and transition energy levels, we find that all group-II defects introduce the relative shallow transition energy levels in kaolinite. Among them, MgAl has the shallowest transition energy level at 0.08eV above the valence band maximum. The transition-elemental defects FeAl, CrAl, and MnAl are found to have relative low formation energies, suggesting their easy formation in kaolinite under natural surrounding conditions. Our calculations show that the defects CuAl and ZnAl have the high formation energies and deep transition energy levels, which exclude the possibility of their formation in natural kaolinite.
HE Man-Chao;FANG Zhi-Jie; ZHANG Ping. Theoretical Studies on Defects of Kaolinite in Clays[J]. 中国物理快报, 2009, 26(5): 59101-059101.
HE Man-Chao, FANG Zhi-Jie, ZHANG Ping. Theoretical Studies on Defects of Kaolinite in Clays. Chin. Phys. Lett., 2009, 26(5): 59101-059101.
[1] He M C, Xu N and Yao A J 2000 J. Chin. Univ. Mini. 10 107 [2] He M C 1996 J. Coal. Sci. 17 10 [3] Adams J M 1983 Clays. Clay. Miner. 31 352 [4] Young R A and Hewat A W 1988 Clays. Clay. Miner. 36 225 [5] Bish D L 1993 Clays. Clay. Miner. 41 {738 [6] Giese R F and Datta P 1973 Am. Mineralogist. 58 471 [7] Giese R F 1982 Bull. Mineralogy 105 417 [8] Hess A C and Saunders V R 1992 Journal of PhysicalChemistry. 96 4367 [9] Hobbs J D, Cygan R T , Nagy K L, Schultz P A, and Sears MP 1997 American Mineralogists 82 657 [10] Benco L , Tunega D, Hafner J and Lischka H 2001 American Mineralogists 86 1057 [11] Angel B R, Jones J P E and Hall P L 1974 Clay.Miner. 10 247 [12] {Bish D L and Von D R 1989 Clays. Clay. Miner. 37 289 [13] Hohenberg P and Kohn W 1964 Phys. Rev. B 136864 Kohn W and Sham L J 1964 Phys. Rev. A 140 1133 [14] Kresse G and Furthm\"{uller J 1996 Phys. Rev. B 54 11169 Kresse G and Furthm\"{uller J 1996 Comput. Mater.Sci. 6 15 [15] Bl\"{ochl P E 1994 Phys. Rev. B 50 17953 Kresse G and Joubert J 1999 Phys. Rev. B 59 1758 [16] Monkhorst H J and Pack J D 1976 Phys. Rev. B 13 5188 [17] Pack J D and Monkhorst H J 1977 Phys. Rev. B 16 1748 [18] Zhang S B, Wei S H, Zunger A and Katayama Y H 1998 Phys. Rev. B 57 964 [19] Wei S H and Zhang S B 2002 Phys. Rev. B 66155211