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Volume 30 Issue 4
Dec.  2011
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Zhang Cheng. Time-scale of karst processes and the carbon sink stability[J]. CARSOLOGICA SINICA, 2011, 30(4): 368-371. doi: 10.3969/j.issn.1001-4810.2011.04.003
Citation: Zhang Cheng. Time-scale of karst processes and the carbon sink stability[J]. CARSOLOGICA SINICA, 2011, 30(4): 368-371. doi: 10.3969/j.issn.1001-4810.2011.04.003

Time-scale of karst processes and the carbon sink stability

doi: 10.3969/j.issn.1001-4810.2011.04.003
  • Received Date: 2011-10-08
  • Publish Date: 2011-12-25
  • This paper discussed the time scale of karst processes and the carbon sink stability from fast kinetics of carbonate dissolution, open property of karst dynamic system and its environmental sensitivity and the involvement of organisms. It showed that karst processes may be particular geologic processes that involved in global carbon cycle over various time scales. Influenced by aquatic vegetation and land-use change, carbon sink resulted from carbonate rock dissolution is remarkable and quite stable, and is significant to the reduction of atmospheric CO2 nowadays. More high resolution data-log monitoring sites should be established for better estimation of carbon sink. It also indicated that the impact of allogenic water in the catchment, aquatic vegetation and land-use change must be taken into account for the estimating method improvement.

     

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