Carbon Sinks Flux Mechanism Analysis in Different Geological Background

Liang Li; Fen Huang; Jian Hua Cao; Pei Wang; Yi Liang

doi:10.4028/www.scientific.net/AMR.616-618.1528

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HomeAdvanced Materials ResearchAdvanced Materials Research Vols. 616-618Carbon Sinks Flux Mechanism Analysis in Different...

Carbon Sinks Flux Mechanism Analysis in Different Geological Background

Abstract:

According to the global carbon balance, the lost carbon is called missing carbon sinks were taken up by geological. In order to describe carbon sinks mechanism, Maocun watershed was selected as a study area, and choose four sites in different geological background, where the electrical conductivity (Ec), bicarbonate, temperature and PH value are monitored, the results show that: (1) The amount of bicarbonate in sandstone water is less than any karst water, the order of bicarbonate is that: (HCO3-)_XiaolongbeiBianyanMaocunchukouBeidiping, and with exogenous water which contain low concentration of bicarbonate flow into the karst area along the water canal, bicarbonate increase step by step until stable; (2)Temperature, hydrophyte photosynthesis are the main impact factors affect on the carbon sinks flux; (3) Exogenous water can aggravate the carbon sinks flux.

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Periodical:

Advanced Materials Research (Volumes 616-618)

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1528-1531

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https://doi.org/10.4028/www.scientific.net/AMR.616-618.1528

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December 2012

Authors:

Liang Li, Fen Huang, Jian Hua Cao, Pei Wang, Yi Liang

Keywords:

Carbon Sinks Flux, Different Geological Background, Mechanism Analysis

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