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Rates of carbon dioxide outgassing and calcite precipitation in travertine-depositing streams

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6459505

The authors studied Falling Spring Creek, Virginia, over the course of a year to quantify rates of calcite precipitation resulting from CO/sub 2/ outgassing in the subsurface and at the surface of the earth. The creek begins in Warm River Cave and is formed by the mixing of a warm stream, fed by a thermal spring, and a cold stream, fed by shallow groundwater. The mixed water emerges at the surface as several springs and forms the surface stream that is characterized by travertine deposition, especially in the vicinity of riffles and falls. The authors used computerized geochemical models to calculate aqueous speciation, saturation states, and PCO/sub 2/ values. They also calculated masses of calcite and CO/sub 2/ transferred out of solution between pairs of sequential samples collected along the 5 km of flow path studied. Using measured stream velocity, they determined rates of CO/sub 2/ outgassing and calcite precipitation for comparison to values predicted by published rate models. In the summer and fall, the stream water is supersaturated with respect to calcite all along the flow path; in the high flow conditions the initial length of the stream is undersaturated. The water reaches a high degree of supersaturation before calcite precipitates. The relatively high concentrations of Mg and SO/sub 4/ in solution may act as kinetic inhibitors of calcite precipitation.

Research Organization:
Univ. of Virginia, Charlottesville (USA)
OSTI ID:
6459505
Report Number(s):
CONF-8510489-
Journal Information:
Geol. Soc. Am., Abstr. Programs; (United States), Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Vol. 17; ISSN GAAPB
Country of Publication:
United States
Language:
English