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1·The alkali saturation test show that the alkali saturated conductivity of the controlled specimen is the greatest and the conductivity of the 10% silica fume-bearing concrete is the smallest.

结果表明：基准试件的饱碱电导最大，掺10%硅灰的混凝土饱碱电导最小。

2·Effects of PAM application rate and method on saturated hydraulic conductivity were studied in laboratory through a soil column leaching experiment.

通过室内土柱淋洗试验，研究了PAM施用量和施用方式对不同碱度土壤饱和水力传导度的影响。

3·Sensitivity analysis of model parameters showed: Saturated hydraulic conductivity is the most sensitive factor for two soil groups, and saturated water content takes second place.

对模型参数的敏感性分析表明：饱和水力传导度是最敏感的参数，饱和含水量的敏感性次之。

4·The saturated hydraulic conductivity of undisturbed soil can represent the really case in the field and is significant to study soil moisture balance and soil water conservation.

原状土的饱和导水率能反映田间的实际情况，对研究土壤水分平衡和水土保持有极其重要的意义。

5·The macropore and saturated hydraulic conductivity have increase with the increase of altitude and have great variability and complexity.

土壤大孔隙和土壤饱和导水率深度增加呈减小的趋势，并且变异性和复杂性很大。

6·The models of specific electrical conductivity were studied which can be used for saturated anisotropic clay.

本文研讨可适用于各向异性饱和粘土的比电导模型。

7·The soil saturated hydraulic conductivity in different vegetation degeneration type and its influential factors in southwest karst region of China were studied.

通过对西南喀斯特地区典型土壤的饱和导水率的分析，研究了喀斯特地区不同植被退化类型下土壤的饱和导水率及其影响因素。

8·The result shows that the saturated hydraulic conductivity has great spatial variability with the various coefficient 67%, and the soil bulky density has lower variability.

结果表明： 饱和导水率具有较大的空间变异性， 变异系数达67%；

9·It is of great significance to the study of ionic contamination that the electrical conductivity of pore fluid in saturated sandy soil reflects the ion content.

饱和砂性土的孔隙水电导率直接反映了孔隙水中离子的含量，对研究土体离子污染有重要意义。

10·While groundwater flows through an unconfined aquifer due to heterogeneity, the vertical average saturated hydraulic conductivity is a function of hydraulic head.

地下水流于非拘限含水层流动时，因含水层之非均质性，使得垂直平均之饱和水力传导系数随地下水水位高低而变化。