水均衡分析法原理是根据岩溶系统径流反推补给面积，进而确定地下水分水岭的位置。
The principle for water balance analysis is to reversely derive the area of water supply according to runoff amount in the karst system, further to determine the position of the groundwater divide.
通过与层次分析法(ahp)的比较表明，ANP方法得出的指标权趋向均衡化，增加了指标权重的可行性和合理性。
Made a comparison between the results of ANP and AHP, which showed that the index weights of ANP were inclined to be more balanced thereby enhanced the feasibility and reasonability of index weights.
采用非均衡数据的单因素方差分析法，评价不同疗法的优劣，并结合多重比较图，得到最佳的疗法。
Adopting ANOVA of unbalanced data, evaluating the effect of different treatment, the best treatment through the multiple comparison graph is got.
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