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• W2388120531 abstract "It is believed that to study the CO_2 releasing or absorbing processes of the Karst water corresponding to the dissolution or formation of carbonate in various environments is the precondition and base for studying carbon cycling effect caused by the dissolution or formation of carbonate.By using Gibbs free energy thermodynamic theory,162 batches of data for waters sampled from rivers,streams,lakes,springs,underground rivers etc.in different Karst regions were collected for thermodynamic study.Our results have revealed that,1) The waters in rivers,streams,lakes,and dripping waters in caves could release CO_2 to atmosphere due to the deposition of calcite.They could be potential sources for CO_2 in atmosphere;2) The underground waters could absorb CO_2 due to the dissolution of carbonate.They could be sinks of CO_2 indirectly;3) The spring waters could not only absorb CO_2 due to carbonate dissolution but also release CO_2 due to carbonate deposition.They could be sinks or sources of CO_2 indirectly;4) the variation of hydrochemical characters of spring waters in flooding period does not change their original properties as sinks or sources of CO_2 dramatically.It is indicated that all river waters and spring waters are releasing CO_2 into atmosphere,based on 162 batches of data.The results show that the Gibbs free energy thermodynamic theory could be used to study if the water in Karst areas could be the potential sources or sinks of CO_2 in atmosphere without any limitation." @default.
• W2388120531 created "2016-06-24" @default.
• W2388120531 creator A5052596963 @default.
• W2388120531 date "2006-01-01" @default.
• W2388120531 modified "2023-09-25" @default.
• W2388120531 title "Geochemistry of Water System in Karst Regions and the Atmospheric CO_2 :Thermodynamic Studies" @default.
• W2388120531 hasPublicationYear "2006" @default.
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