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- W2389032173 abstract "We had high resolution monitor on the HCO-3and Flux in response to the rainfall of Maocun subterranean river in Guilin on June 13～17,2010.Measured the precipitation,water level,water temperature,pH,EC(electrical conductivity) and HCO-3(bicarbonate) by CTDP300,Based on the SIc(saturation index) and pCO2(carbon dioxide partial pressure),analyzed the dynamic behaviors of karst carbon sink in rainfall.Relevant data shows that the water stage,flow and water temperature change with the rainfall.HCO-3,pH,SIc and pCO2 are in response to rainfall quickly.Karst carbon sink increased after rainfall and changed with the rainfall intensity.Furthermore,according to the contrast result of carbon sink between March 7,2010 and June 13,2010 of Maocun subterranean river,we find that carbon sink increased approximately two times after rainfall,carbon sink changes with different seasons,generally,rainy season's carbon sink is more than dry season,the results present that karst areas have a potential carbon sequestration." @default.
- W2389032173 created "2016-06-24" @default.
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- W2389032173 date "2011-01-01" @default.
- W2389032173 modified "2023-09-28" @default.
- W2389032173 title "Response of karst carbon sink dynamic behaviors to rainfall——a case study in Maocun Subterranean river of Guilin" @default.
- W2389032173 hasPublicationYear "2011" @default.
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