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Oxidation–reduction sequences in ground water flow systems

Champ, D. R., Gulens, J., Jackson, R. E.·1979·Canadian Journal of Earth Sciences

Abstract

Hydrogeologists and ground water geochemists have observed a decline in the measured (platinum electrode) potential, E H, of ground water as it migrates from upland recharge areas to lowland discharge areas under confined conditions. Such variations in E H and variations in concentrations of elements with variable oxidation states (e.g., oxygen, nitrogen, iron, manganese, sulfur, and carbon) can be accounted for by a sequence of oxidation–reduction reactions occurring in the flow systems, the sequence being based on thermodynamic principles as outlined by Stumm and the microbial catalysis of such reactions. This sequence of reactions results in the identification of three redox zones in ground water flow systems: (1) oxygen–nitrate, (2) iron–manganese, and (3) sulfide. The mobility and concentration of most transition metal and nonmetal ions vary according to zone—a matter of considerable significance in exploration geochemistry and in ground water pollution studies.

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Metadata

Authors
Champ, D. R., Gulens, J., & Jackson, R. E.
Venue
Canadian Journal of Earth Sciences
Published
1979-01-01
Volume
16
Issue
1
Pages
12-23
ISSN
  • 0008-4077 (ISSN-L)
  • 1480-3313
OpenAlex
W1976214358
Cited by
376
References
0
FWCI
10.24
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Oxidation–reduction sequences in ground water flow systems. https://app.cochat.ai/papers/10.1139/e79-002
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Champ, D. R., Gulens, J., & Jackson, R. E. (1979). Oxidation–reduction sequences in ground water flow systems. Canadian Journal of Earth Sciences. https://doi.org/10.1139/e79-002

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