The effect of climate on the chemistry of carbonate groundwater.

Citation

Material Information

Title:
The effect of climate on the chemistry of carbonate groundwater.
Series Title:
Water Resources Research
Creator:
Drake, John J.
Wigley, T.M.L.
Publisher:
American Geophysical Union.
Publication Date:
Language:
English

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Genre:
serial ( sobekcm )

Notes

Abstract:
The temperature coefficient of the log Pco2‐temperature relationship for springwater from carbonate terrains in North America is approximately 0.07/°C. Consideration of a simple model of soil air behavior and various published data suggests that the temperature coefficient of the same relationship for soil air is of the order of 0.04/°C. A model where the soil zone is the source of carbon dioxide for water entering a groundwater system and where the subsequent chemical evolution of the water occurs under closed system conditions is consistent with these relationships.
Original Version:
Water Resources Research, Vol. 11, no. 6 (1975-12).

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Source Institution:
University of South Florida Library
Holding Location:
University of South Florida
Rights Management:
This object is protected by copyright, and is made available here for research and educational purposes. Permission to reuse, publish, or reproduce the object beyond the bounds of Fair Use or other exemptions to copyright law must be obtained from the copyright holder.

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