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《JOURNAL OF NANJING AGRICULTURAL UNIVERSITY》 1999-03
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Soil carbon as dynamic mechanism for epikarstification in humid subtropical region: Evidence of carbonreservoirs and transfer in the system

Pan Genxing 1,Cao Jianhua 2,He Shiyi 2,Tao Yuxiang 1,Shun Yuhua 1 and Teng Yongzhong 1 ( 1 College of Resources and Environmental Sciences,Nanjing Agric Univ,Nanjing 210095; 2 Key Lab of Karst Dynamics,Ministry of Land and Natural Resources,Gui  
Taking an example of Guilin Yaji Karst Experiment Site,carbon reservoirs and their stable isotope abundance were analysed of the epikarst system,and CO 2 concentration in air of plant system and its relation to soil respiration CO 2 emmission were monitored.The results showed that soil carbon was the biggest carbon reservoir in the system,plant CO 2 absorption from air and soil CO 2 respiration emmission were the predominant process of carbon fluxes in the system.The labile carbon forms mainly expressed as CO 2 in the system was dominantly derived from soil carbon.Consequently,the dynamic mechanism of soil carbon for epikarst system in humid subtropical karst region was revealled.
【Fund】: 国家自然科学基金;岩溶动力学开放实验室资助
【CateGory Index】: S153.1r#
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