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CO_(2)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 sute of Shaanxi an examples,by analyzing the temporal change and the difference in soul CO;content,the relationship between soil CO_(2)and karst process in South and North China 1 expounded.Combined with the climaue data(temperature and precipi-tetion)etc..the reason for the difference in karst development in South and North Chins 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IGCP379项目、国家自然科学基金项目(49632100、49703047)
地矿部“九五”重大项目(9501104)
地矿部岩溶动力学开放研究实验联合资助。
