The mineral-water interface: Where minerals react with the environment

The reactions that occur at the mineral–water interface are central to all geochemical processes. They affect a wide range of important Earth processes, all of which involve geochemical element cycling. Examples include weathering and soil formation, nutrient availability, biomineralization, acid mi...

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Main Authors: Putnis, Christine, Ruiz-Agudo, E.
Format: Journal Article
Published: 2013
Online Access:http://hdl.handle.net/20.500.11937/46998
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author Putnis, Christine
Ruiz-Agudo, E.
author_facet Putnis, Christine
Ruiz-Agudo, E.
author_sort Putnis, Christine
building Curtin Institutional Repository
collection Online Access
description The reactions that occur at the mineral–water interface are central to all geochemical processes. They affect a wide range of important Earth processes, all of which involve geochemical element cycling. Examples include weathering and soil formation, nutrient availability, biomineralization, acid mine drainage, the fate of contaminants, nuclear waste disposal, and minor element incorporation and partitioning during mineral growth. Each of these processes, and its reaction rates, is ultimately controlled by reactions that occur at mineral surfaces. Through the development of advanced analytical methods, direct observations of mineral reactions at the nanoscale have enabled exciting new possibilities for clarifying the mechanisms governing mineral–fluid reactions.
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spelling curtin-20.500.11937-469982017-09-13T14:27:26Z The mineral-water interface: Where minerals react with the environment Putnis, Christine Ruiz-Agudo, E. The reactions that occur at the mineral–water interface are central to all geochemical processes. They affect a wide range of important Earth processes, all of which involve geochemical element cycling. Examples include weathering and soil formation, nutrient availability, biomineralization, acid mine drainage, the fate of contaminants, nuclear waste disposal, and minor element incorporation and partitioning during mineral growth. Each of these processes, and its reaction rates, is ultimately controlled by reactions that occur at mineral surfaces. Through the development of advanced analytical methods, direct observations of mineral reactions at the nanoscale have enabled exciting new possibilities for clarifying the mechanisms governing mineral–fluid reactions. 2013 Journal Article http://hdl.handle.net/20.500.11937/46998 10.2113/gselements.9.3.177 restricted
spellingShingle Putnis, Christine
Ruiz-Agudo, E.
The mineral-water interface: Where minerals react with the environment
title The mineral-water interface: Where minerals react with the environment
title_full The mineral-water interface: Where minerals react with the environment
title_fullStr The mineral-water interface: Where minerals react with the environment
title_full_unstemmed The mineral-water interface: Where minerals react with the environment
title_short The mineral-water interface: Where minerals react with the environment
title_sort mineral-water interface: where minerals react with the environment
url http://hdl.handle.net/20.500.11937/46998