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The ‘Anthropogenic Influences ’ section of this volume on Environmental Mineralogy is concerned with controls on mineral-environment interactions that are in some way influenced by human activity. Mineral-environment interactions include all types of mineral growth and decomposition, with associated chemical and isotopic signatures, and all other chemical reactions such as ion exchange and adsorption. The controls on these interactions are the physical, chemical and biological conditions that exist in the immediate vicinity of the mineral.

Many mineral-environment interactions occur naturally in response to natural processes of change, and the significance of an anthropogenic influence may simply be in the rate or the scale of change. Thus, for example, pyrite oxidation resulting in the liberation of protons (pH decrease), has occurred wherever pyritiferous rocks have been exposed to the atmosphere or to oxygenated waters (Keith and Vaughan, chapter 7). But it is often only where humans have opened new conduits in rocks, or have spatially concentrated gangue sulphides in heaps of high-porosity mine waste, that the scale of interactions has become significant to the wider environment. Alternatively, the significance of an anthropogenic influence may be in the combining of substances that would not normally be found together in nature, or it may be in the creation of reactive conditions.

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