摘要
中国北方半干旱区存在丛山窄谷、冈山宽谷和孤山溶盆三种岩溶地貌。不同岩溶地貌区的碳酸盐岩溶蚀强度和碳循环强度不同。碳酸盐岩溶蚀量和CO2吸收量可以用化学热力学过程和化学动力学过程描述。
Three karst landforms distribute in semiarid area of North China,i.e.,cluster peak with narrow valley,gentle peak with broad valley and gentle plainhill.The strength of carbon cycle and limestone dissolution is different in various karst landforms.the carbon dioxide absorption content and limestone dissolution content can be estimated by chemical thermodynamics processes and chemical dynamics processes.
出处
《中国岩溶》
CAS
CSCD
1997年第4期296-303,共8页
Carsologica Sinica
基金
国际地质对比计划IGCP379项目
关键词
岩溶
碳循环
反应-迁移模型
数值模拟
干旱区
Karst Carbon cycle Reactiontransportation model Numerical modelling North semi-arid area