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土壤碳作为湿润亚热带表层岩溶作用的动力机制:系统碳库及碳转移特征
引用本文:潘根兴,曹建华,何师意,陶于祥,孙玉华,滕永忠.土壤碳作为湿润亚热带表层岩溶作用的动力机制:系统碳库及碳转移特征[J].南京农业大学学报,1999,22(3):1.
作者姓名:潘根兴  曹建华  何师意  陶于祥  孙玉华  滕永忠
作者单位:1. 南京农业大学资源与环境科学学院,南京,210095
2. 桂林岩溶地质研究所及岩溶动力学开放实验室,桂林,541004
基金项目:国家自然科学基金,岩溶动力学开放实验室资助
摘    要:以桂林丫吉村岩溶实验场为例, 分析了表层带岩溶系统中碳库组成, 测定了各碳库的碳稳定性同位素丰度, 表明土壤碳是系统中最大的碳库, 生物的 C O2 吸收同化与土壤有机质分解导致的土壤 C O2 释放是系统中主导的碳流通过程, 系统活动态碳组分主要由土壤碳贡献, 从而揭示了土壤碳对表层岩溶作用的动力机制。

关 键 词:表层岩溶系统  碳库  碳转移  碳稳定性同位素  土壤碳
修稿时间:1998-11-23

Soil carbon as dynamic mechanism for epikarstification in humid subtropical region: Evidence of carbon reservoirs and transfer in the system
Pan Genxing,Cao Jianhua,He Shiyi,Tao Yuxiang,Shun Yuhua,Teng Yongzhong.Soil carbon as dynamic mechanism for epikarstification in humid subtropical region: Evidence of carbon reservoirs and transfer in the system[J].Journal of Nanjing Agricultural University,1999,22(3):1.
Authors:Pan Genxing  Cao Jianhua  He Shiyi  Tao Yuxiang  Shun Yuhua  Teng Yongzhong
Abstract: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.
Keywords:carbon reservoir  carbon stable isotope  carbon transfer  epikarst system  soil carbon
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