摘要
作者以桂林岩溶试验场和陕西鱼洞河两个观测站为例，分析了我国南、北方土壤ＣＯ２的动态、差异及其对岩溶作用的驱动规律，进一步结合气候条件（气温、降水）等的分析，揭示了南、北方岩溶发育差异的根源。
Taking the guilin karst experimental site of Guangxi and the Yudonghe observation site of Shaanxi as examples, by analyzing the temporal change and the difference in soil CO 2 content, the relationship between soil CO 2 and karst process in South and North China is expounded. Combined with the climatic data (temperature and precipitation) etc., the reason for the difference in karst development in South and North China is further revealed.
出处
《水文地质工程地质》
CAS
CSCD
1998年第4期42-45,共4页
Hydrogeology & Engineering Geology
基金
国际地质对比计划
国家自然科学基金
地矿部"九五"重大项目
地矿部岩溶动力学开放研究实验联合资助
