Science: v.1-v.219Moses King, 1967 |
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Стр. 1228
... sulfate indicates that oceanic sulfate is not in oxygen isotope equilibrium with ocean water . Preliminary experiments suggest that the turnover of sulfate in the sulfur cycle is too rapid to allow equilibrium to be established . If ...
... sulfate indicates that oceanic sulfate is not in oxygen isotope equilibrium with ocean water . Preliminary experiments suggest that the turnover of sulfate in the sulfur cycle is too rapid to allow equilibrium to be established . If ...
Стр. 1229
... sulfate Marine evaporating pans Nonmarine sulfates S018 WATER Fig . 3. Variations in 801 of dissolved sulfate compared to the 8018 of the water from various natural waters . Locations of samples are given in Table 1 . Fig . 4 ...
... sulfate Marine evaporating pans Nonmarine sulfates S018 WATER Fig . 3. Variations in 801 of dissolved sulfate compared to the 8018 of the water from various natural waters . Locations of samples are given in Table 1 . Fig . 4 ...
Стр. 1230
... sulfate is more negative than the predicted equilibrium value we cannot call on bacterial reduction as the primary con- trolling factor for its isotopic composi- tion . The second element of the cycle , the oxidation of reduced sulfur ...
... sulfate is more negative than the predicted equilibrium value we cannot call on bacterial reduction as the primary con- trolling factor for its isotopic composi- tion . The second element of the cycle , the oxidation of reduced sulfur ...
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