黄铁矿吸附-还原金络合物的实验研究进展
Progress in Experimental Investigations on the Adsorption-reduction of Gold Complexes by Pyrite
查看参考文献77篇
文摘
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金的吸附成矿作用是表生和低温条件下的一种重要成矿机制。本文综述了黄铁矿吸附-还原金络合物的实验研究方法,探讨了黄铁矿吸附-还原不同金络合物的反应机制和影响因素。黄铁矿对Au-S络合物的吸附作用主要是黄铁矿与Au-S络合物之间的静电吸附以及表面络合,由于吸附的Au-S络合物的还原反应相当缓慢,随着周围环境的变化很容易发生解吸附作用;而黄铁矿对Au-Cl络合物的吸附作用实质上是黄铁矿表面金络合物迅速的还原反应,通过还原作用形成自然金而使得解吸附率极低。As掺杂形成的p型黄铁矿以及和n型黄铁矿构成p-n结是导致金络合物在黄铁矿表面发生电化学沉淀的驱动因素。目前有关金的吸附实验都是在温度小于90℃的表生条件下进行的,开展一定温度和压力条件下的吸附成矿实验,尤其是利用电化学方法原位研究高温高压下黄铁矿-金络合物溶液之间的界面反应以及原电池效应对金络合物还原作用的影响,是今后研究的重点。 |
其他语种文摘
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Gold adsorption metallogenesis is an important metallogenic mechanism at supergene and low temperature conditions. We summarized the experimental investigation methods of gold adsorption-reduction by pyrite and discussed the gold reduction mechanism on pyrite surface in different gold complexes solutions.The adsorption of Au-S complexes on pyrite surface is mainly the processes of electrostatic adsorption and surface complexation.Because the reduction reaction rate of the adsorption of Au-S complexes on pyrite surface is quite low,desorption will occurs once the conditions are changed.However,the adsorbed Au-Cl complexes on pyrite surface are rapidly reduced,and natural gold particles are produced through it,therefore,aprocess of desorption hardly occurs.p-type pyrite doped by arsenic is apt to form p-n junctions with n-type pyrite,which is the driving factors to result in electrochemical precipitation of gold complexes on pyrite surface.Gold adsorption experiments are currently conducted at conditions of supergene with temperatures<90℃.Therefore,in the future,we should carry out adsorption metallogenic experiments at higher temperature and pressure conditions,especially combining with in-situ electrochemical approaches to investigate the influence of interface reaction between pyrite and gold complexes and galvanic effect on gold complexes reduction. |
来源
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地球与环境
,2013,41(2):185-192 【核心库】
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关键词
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吸附成矿
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黄铁矿
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金沉淀
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电化学反应
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原电池效应
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地址
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中国科学院地球化学研究所, 中国科学院地球内部物质高温高压实验室, 贵阳, 550002
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语种
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中文 |
文献类型
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综述型 |
ISSN
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1672-9250 |
学科
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地质学 |
基金
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国家自然科学基金
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中国科学院地球化学研究所“135”项目
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中国科学院重大科研装备研制项目
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文献收藏号
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CSCD:4800284
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参考文献 共
77
共4页
|
1.
毛华海. 热液中金的沉淀机理研究综述.
地质地球化学,1997,2(2):89-92
|
CSCD被引
10
次
|
|
|
|
2.
Muntean J L. Magmatic-hydrothermal origin of Nevada's Carlin-type gold deposits.
Nature Geoscience,2011,4(2):122-127
|
CSCD被引
69
次
|
|
|
|
3.
Sung Y H. Invisible gold in arsenian pyrite and arsenopyrite from a multistage Archaean gold deposit:Sunrise Dam,Eastern Goldfields Province,Western Australia.
Mineralium Deposita,2009,44(7):765-791
|
CSCD被引
24
次
|
|
|
|
4.
Williams-Jones A E. Gold in solution.
Elements,2009,5(5):281-287
|
CSCD被引
71
次
|
|
|
|
5.
Zhu Y F. Geochemistry of hydrothermal gold deposits:A review.
Geosciences Frontiers,2011,2(3):367-374
|
CSCD被引
14
次
|
|
|
|
6.
Maddox L M. Invisible gold comparison of Au deposition on pyrite and arsenopyrite.
American Mineralogist,1998,83(11/12Part1):1240-1245
|
CSCD被引
10
次
|
|
|
|
7.
Mikhlin Y L. Gold deposition on pyrite and the common sulfide minerals:An STM/STS and SR-XPS study of surface reactions and Au nanoparticles.
Geochimica et Cosmochimica Acta,2007,71(24):5985-6001
|
CSCD被引
7
次
|
|
|
|
8.
Mikhlin Y L. Understanding the initial stages of precious metals precipitation: Nanoscale metallic and sulfidic species of gold and silver on pyrite surfaces.
Ore Geology Reviews,2011,42(1):47-54
|
CSCD被引
10
次
|
|
|
|
9.
Mycroft J R. Spontaneous deposition of gold on pyrite from solutions containing Au (III)and Au(I)chlorides.Part I:A surface study.
Geochimica et Cosmochimica Acta,1995,59(16):3351-3365
|
CSCD被引
5
次
|
|
|
|
10.
Bancroft G M. Gold deposition at low temperature on sulphide minerals.
Nature,1982,298(5876):730-731
|
CSCD被引
2
次
|
|
|
|
11.
Widler A M. The adsorption of gold(I)hydrosulphide complexes by iron sulphide surfaces.
Geochimica et Cosmochimica Acta,2002,66(3):384-402
|
CSCD被引
34
次
|
|
|
|
12.
涂光炽.
低温地球化学,1998
|
CSCD被引
26
次
|
|
|
|
13.
朱笑青. 银和金的选择吸附实验研究及意义.
矿床地质,2005,24(4):445-450
|
CSCD被引
4
次
|
|
|
|
14.
Zotov A V. Thermodynamic properties of aurochloride solute complex AuCl-2 at temperature of 350-500℃ and pressure of 500-1500bars.
Sciences Geologiques Bulletin,1989,42:335-342
|
CSCD被引
1
次
|
|
|
|
15.
Pokrovski G S. An in situ X-ray absorption spectroscopy study of gold-chloride complexing in hydrothermal fluids.
Chemical Geology,2009,259(1):17-29
|
CSCD被引
8
次
|
|
|
|
16.
Stefansson A. Stability of chloridogold(I)complexes in aqueous solutions from 300to 600℃and from 500 to 1800bar.
Geochimica et Cosmochimica Acta,2003,67(23):4559-4576
|
CSCD被引
11
次
|
|
|
|
17.
郁云妹. 金沉淀的一个可能机理——歧化反应.
中国科学:D辑,1997,27(5):419-424
|
CSCD被引
3
次
|
|
|
|
18.
Seward T M. Thio complexes of gold and the transport of gold in hydrothermal ore solutions.
Geochimica et Cosmochimica Acta,1973,37(3):379-399
|
CSCD被引
71
次
|
|
|
|
19.
Hayashi K. Solubility of gold in NaCl-and H_2S-bearing aqueous solutions at 250-350℃.
Geochimica et Cosmochimica Acta,1991,55(8):2111-2126
|
CSCD被引
45
次
|
|
|
|
20.
Pokrovski G S. A new view on gold speciation in sulfur-bearing hydrothermal fluids from in situ X-ray absorption spectroscopy and quantum-chemical modeling.
Geochimica et Cosmochimica Acta,2009,73(18):5406-5427
|
CSCD被引
22
次
|
|
|
|
|