Dynamics and stable isotope composition of gaseous and dissolved oxygen
The vadose zone and ground water environments are a sink for atmospheric O(2). The pathways and rates of O(2) consumption are primarily related to the availability and rate of oxidation of key reductants (e.g., organics, sulfides), through a combination of biological or abiotic reactions. The range...
Veröffentlicht in: | Ground water. - 1979. - 45(2007), 4 vom: 01. Juli, Seite 447-60 |
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Format: | Aufsatz |
Sprache: | English |
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2007
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Zugriff auf das übergeordnete Werk: | Ground water |
Schlagworte: | Journal Article Research Support, Non-U.S. Gov't Oxygen Isotopes Oxygen S88TT14065 |