CHEMICAL WEATHERING, ATMOSPHERIC CO2, AND CLIMATE

dc.contributor.authorKump L.R.
dc.contributor.authorBrantley S.L.
dc.contributor.authorArthur M.A.
dc.date.accessioned2021-01-29T07:14:08Z
dc.date.available2021-01-29T07:14:08Z
dc.date.issued2000
dc.description.abstractThere has been considerable controversy concerning the role of chem-ical weathering in the regulation of the atmospheric partial pressure of carbon dioxide, and thus the strength of the greenhouse effect and global climate. Arguments center on the sensitivity of chemical weathering to climatic factors, especially temperature. Laboratory studies reveal a strong dependence of mineral dissolution on temperature, but the expression of this dependence in the field is often obscured by other environ-mental factors that co-vary with temperature. In the field, the clearest correlation is between chemical erosion rates and runoff, indicating an important dependence on the intensity of the hydrological cycle. Numerical models and interpretation of the geologic record reveal that chemical weathering has played a substantial role in both maintaining climatic stability over the eons as well as driving climatic swings in response to tectonic and paleogeographic factors.
dc.identifierhttps://elibrary.ru/item.asp?id=13827107
dc.identifier.citationAnnual Review of Earth and Planetary Sciences, 2000, 28, , 611-667
dc.identifier.issn0084-6597
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/24027
dc.titleCHEMICAL WEATHERING, ATMOSPHERIC CO2, AND CLIMATE
dc.typeСтатья

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