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Origin of the Chemical Compositions of Some Springs and Lakes
Abstract
The spring waters of the Sierra Nevada result from the attack of high CO 2 soil waters on typical igneous rocks and hence can be regarded as nearly ideal samples of a major water type. Their compositions are consistent with a model in which the primary rock-forming silicates are altered in a closed system to soil minerals plus a solution in steady-state equilibrium with these minerals. Isolation of Sierra waters from the solid alteration products followed by isothermal evaporation in equilibrium with the earth's atmosphere should produce a highly alkaline Na-HCO 3- CO 3 water; a soda lake with calcium carbonate, magnesium hydroxysilicate, and amorphous silica as precipitates.
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Citations
Cited by
Nesbitt, H. W., & Young, G. M. (1984) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(84)90408-3 · Cited by 2,368
Chemical processes affecting alkalis and alkaline earths during continental weathering
Nesbitt, H. W., Markovics, G., & price, R. C. (1980) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(80)90218-5 · Cited by 1,050
Chemical Weathering, Atmospheric CO2, and Climate
Kump, L. R., Brantley, S. L., & Arthur, M. A. (2000) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev.earth.28.1.611 · Cited by 874
Middelburg, J. J., van der Weijden, C. H., & Woittiez, J. R. W. (1988) · Chemical Geology · doi:10.1016/0009-2541(88)90025-3 · Cited by 614
The origin of brines and salts in Chilean salars: a hydrochemical review
Risacher, F., Alonso, H., & Salazar, C. (2003) · Earth-Science Reviews · doi:10.1016/s0012-8252(03)00037-0 · Cited by 325
Metadata
- Authors
- GARRELS, R. M., & MACKENZIE, F. T.
- Venue
- Advances in Chemistry
- Publisher
- AMERICAN CHEMICAL SOCIETY
- Published
- 1967-01-01
- Pages
- 222-242
- ISSN
- 0065-2393 (ISSN-L)
- OpenAlex
- W2485646210
- Cited by
- 793
- References
- 0
- FWCI
- 10.00
- Type
- book chapter
- Language
- en
- Open access
- closed
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