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Cited by 625

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Geochemical Processes at Mineral Surfaces

·1987·ACS Symposium Series

Abstract

The phase discontinuity that occurs at the mineral-water interface greatly influences the geochemical cycles of many elements. The composition of natural waters and the flux of material through the hydrosphere are largely controlled by the weathering of minerals and the precipitation of new phases -- processes in which the mineral - water interface plays a fundamental role. In addition, mineral surfaces may act as catalysts for chemical or biological transformations that occur within the hydrosphere. Reactions at the mineral-water interface are of interest in the study of ore genesis, geochemical exploration, mineral separation processes such as flotation and sedimentation, transport of adsorbed nutrients or pollutants in rivers and lakes, scavenging of trace elements in the oceans, and the transport of nuclear or other hazardous waste materials in groundwaters.

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Metadata

Venue
ACS Symposium Series
Published
1987-11-13
ISSN
  • 0097-6156 (ISSN-L)
  • 1947-5918
OpenAlex
W1512962418
Cited by
625
References
0
FWCI
31.33
Type
conference paper
Language
en
Open access
closed

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CoChat. (2026). Citation check: Geochemical Processes at Mineral Surfaces. https://app.cochat.ai/papers/10.1021/bk-1987-0323
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Geochemical Processes at Mineral Surfaces. (1987). ACS Symposium Series. https://doi.org/10.1021/bk-1987-0323

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Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.