Coupled dissolution and precipitation at mineral-fluid interfaces

被引：320

作者：

Ruiz-Agudo, E. ^{[1
]}

Putnis, C. V. ^{[2
]}

Putnis, A. ^{[2
]}

机构：

[1] Univ Granada, Dept Mineral & Petr, E-18071 Granada, Spain

[2] Univ Munster, Inst Mineral, D-48149 Munster, Germany

来源：

CHEMICAL GEOLOGY | 2014年 / 383卷

关键词：

Replacement; Coupled dissolution-precipitation; Mineral-water interface; ATOMIC-FORCE MICROSCOPY; AQUEOUS SOLUTION SYSTEMS; REPLACEMENT REACTIONS; SILICATE MINERALS; ALKALI FELDSPARS; HYDROTHERMAL CONDITIONS; LABRADORITE FELDSPAR; MOLECULAR-DYNAMICS; CALCITE SURFACES; CATION-EXCHANGE;

D O I：

10.1016/j.chemgeo.2014.06.007

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

Reactions occurring at mineral-fluid interfaces are important in all geochemical processes and essential for the cycling of elements within the Earth. Understanding the mechanism of the transformation of one solid phase to another and the role of fluids is fundamental to many natural and industrial processes. Problems such as the interaction of minerals with CO2-saturated water, the durability of nuclear waste materials, the remediation of polluted water, and mineral reactions that can destroy our stone-based cultural heritage, are related by the common feature that a mineral assemblage in contact with a fluid may be replaced by a more stable assemblage. (C) 2014 Published by Elsevier B.V.

引用

页码：132 / 146

页数：15

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