The result shows that the variation of hydraulic conductivity with the changes of groundwater head in observation wells in Pingtung Plain is of fuzzy properties.
由分析可知，屏东平原各地下水位观测站井之水力传导系数随地下水位变化具模糊关系。
The result shows that the variation of hydraulic conductivity with the changes of groundwater head in observation wells in Pingtung Plain is of fuzzy properties.
由分析可知，屏东平原各地下水位观测站井之水力传导系数随地下水位变化具模糊关系。
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