在裂隙岩溶水水源地，由于地下水系统的存储与调蓄作用，地下水水位时间上的自相关性显著。

Due to the larger volume of storage and regulation in karstic water fi eld, the time-autocorrelation of groundwater level is outstanding.

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在此基础上，建立了裂隙岩溶水数学模型，同时用有限单元法对地下水资源进行了进一步评价，得出了较为满意的结果。

The mathematical model of karst fissure water is established on this basis, and further evaluation of groundwater resources is made by using finite element method. The result is satisfactory.

youdao

在此基础上，建立了裂隙岩溶水数学模型，同时用有限单元法对地下水资源进行了进一步评价，得出了较为满意的结果。

The mathematical model of karst fissure water is established on this basis, and further evaluation of groundwater resources is made by using finite element method…

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