The distribution of gold colloids in kaolinite and the interaction between gold and kaolinite surface were investigated by transmission electron microscopy (TEM) and X-ray photoelectron spectroscopy (XPS). There is strong interaction between the gold particles and the edge surfaces of kaolinite,in low pH solution,the edge surface of kaolinite is positively charged and electrostatic attractive force between colloide gold particles and the positive edge surface of kaolinite would facilitate the adsorption of colloidal gold particles onto the suface. TEM observation shows that the aggregate morphology of gold particles was dominated by particle-particle interaction and gold particles were adsorbed on the edge surface of kaolinite crystals, resulting from the electrostatic attractive force between colloidal gold particles and the positive surfaces of kaolinite. XPS data show that in Au4f electron spectra there are four energy peaks related to gold, 83.8 eV, 85.7 eV, 87.5 eV, and 89.4 eV, respectively, which suggests that in chemical states there are metallic gold and Au bonded to O, similar to the form of Au2O3, and composite Au2O3 is formed between the edge surface of kaolinite and colloidal gold surface.
参考文献
[1] | Thompson D W;Macmillan J J;Wyatt D A .Electron Microscope Studies of the Surface Microstructures of Layer-lattice Silicates[J].Journal of Colloid and Interface Science,1981,82:362-372. |
[2] | Foster R L .Gold Deposits at Slate Creek,Northern Nye County,Nevada[J].Economic Geology,1970,66:965-966. |
[3] | Andrade W O;Machesky M L;Rose A W .Gold Distribution and Mobility in the Surficial Environment,Carajas Region,Brazil[J].Journal of Geochemical Exploration,1991,40:95-114. |
[4] | Boyle R W .The Geochemistry of Gold and Its Deposits[J].Geological Survey of Canada Bulletin,1979,280:91-140. |
[5] | Seeley J B;Senden T J .Alluvial Gold in Kalimantan,Indenesia:A Colloidal Origin?[J].Journal of Geochemical Exploration,1994,50:457-478. |
[6] | Hong H L;Wang Q Y;Chang J P et al.Occurrence and Distribution of Invisible Gold in the Shewushan Supergene Gold Deposit China[J].The Canadian Mineralogist,1999,38:1525-1531. |
[7] | 闵新民,HONG Han-lie,AN Ji-ming.Quantum Chemistry Calculations on the Interaction Between Kaolinite and Gold[J].武汉理工大学学报(材料科学版)英,2001(04):57-61. |
[8] | Qian D F;Diao S Q .Occurrence of Gold in an "Invisible gold" Deposit[J].Geochimica,1986,13(01):58-64. |
[9] | Sutheimer S H;Maurice P A;Zhou Q .Dissolution of Well and Poorly Crystallized Kaolinites:Al Speciation and Effects of Surface Characteristics[J].American Mineralogist,1999,84:620-628. |
[10] | Aita C R;Tran N C .Core Level and Valence Band x-ray Photoelectron Spectroscopy of Gold Oxide[J].Journal of Vacuum Science and Technology A-Vacuum Surfaces and Films,1991,9(03):1498-1500. |
[11] | van Olphen H.A Guide to the Chemistry of Clay Colloids[M].北京:科学出版社,1982:88-92. |
[12] | Verwey E J W;Overbeek J Th G.Theory of the Stability of Lyophobic Colloids[M].Amsterdam:Elseveir,1948 |
[13] | Thompson D W;Collins I R .Electrolyte-induced Aggregation of Gold Particles on Solid Surfaces[J].Journal of Colloid and Interface Science,1978,65:79-87. |
[14] | Williams D J A;Williams K P .Electrophoresis and Zeta Potential of Kaolinite[J].Journal of Colloid and Interface Science,1994,163:347-354. |
[15] | Sposito G.The Surface Chemistry of Soils[M].New York:Oxford University Press,1984 |
[16] | Hong H L;Min X M;Fu Z Y .Study on Adsorption of Submicrometer Gold on Kaolinite by Quantum Chemistry Calculations[J].American Mineralogist,2002,87(01):1-4. |
[17] | Mcintosh D;Ozin G A .Direct Synthesis Using Gold Atoms,Monodioxygen Gold,Au(O2)[J].Inorganic Chemistry,1976,15(11):2869-2871. |
[18] | Pyykko P;Desclaux J P.Relativity and the Periodic System of Elements[J].Accounts of Chemical Research,1979(12):276-281. |
[19] | Herzberg G.Spectra of Diatomic Molecules[M].New York:Van Nostrand,1950 |
[20] | Seidel S;Seppelt K .Xenon as a Complex Ligand:The Tetra Xenono Gold (Ⅱ) Cation in AuXe42+(Sb2F-11)2[J].Science,2000,290(06):117-118. |
- 下载量()
- 访问量()
- 您的评分:
-
10%
-
20%
-
30%
-
40%
-
50%