The karst process is carbon sequestration for atmosphere CO2. Karst carbon sequestration (KCS) value depends on the discharge of karst catchment and inorganic carbon concentration of water body.

岩溶作用对大气co 2起到汇的作用，其量级的大小受岩溶水的排泄量及由岩溶作用产生的无机碳浓度两方面的影响。

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There are many factors that affect the low flow in a karst basin, such as climate, catchment area, lithology, soil, landform and so on, most of which are uncertain.

喀斯特流域枯水径流特征值的影响因素很多，如气候、流域面积、岩性、土壤、地貌等等，而能够确知的信息不多。

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The karst groundwater system in Ordos basin consists of 22 sub-systems with various catchment sizes.

鄂尔多斯盆地周边岩溶分布区由22个汇水面积不等的岩溶地下水子系统组成。

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