片语

hydraulic conductivity and storage导储水参数

osmotic coefficient[物] 渗透系数

horizontal hydraulic conductivity水平渗透系数

soil saturated hydraulic conductivity土壤饱和导水率

saturated hydraulic conductivity[土壤] 饱和导水率

equivalent vertical hydraulic conductivity等效竖向渗透系数

coefficient of permeability[流] 渗透系数

soil hydraulic conductivity[土壤]

hydraulic c conductivity导水率

saturated soil hydraulic conductivity饱和水力传导度

estimating saturated hydraulic conductivity估计饱合水的导电性

英汉例句

• Different function forms of hydraulic conductivity coefficient influence the distributions of IFP in the local region of the tumor.

  不同函数形式分布的水力传导系数，影响肿瘤局部区域内间质流体压强的分布。

• 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%；

• Profiled at the same time with the yarn structure, strengthen the hydraulic conductivity function, so that sweat evaporates quickly discharged and feeling fresh.

  同时配合纱线异型断面结构，加强导水功能，使汗水迅速蒸发排出而感觉清爽。

• 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。

• 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堿度土壤饱和水力传导度的影响。

• The hydraulic conductivity tensor in obtained through connecting fractures in the fracture network model.

  裂隙巖体的渗透系数张量是一个非常重要的巖体水力学参数。

• It is necessary to study the unsaturated hydraulic conductivity of densely compacted bentonite under the confined conditions.

  因此，有必要研究侧限状态下高压实膨润土的非饱和渗透性能。

• Water content, effective porosity and unsaturated hydraulic conductivity of samples were measured.

  多孔介质非饱和导水率是地下水污染预测与评价的重要参数。

• Soil hydraulic conductivity is closely related to the movement of water and salts in soil profiles and is highly affected by solution salt concentration and its composition.

  水力传导度的变化直接影响土壤剖面的水盐运动，并和土壤溶液的盐分浓度及其组成有很大关系。

• The results indicated that N deficiency decreased root radial and axial hydraulic conductivity of maize.

  用蒸腾计法和解剖学方法分别研究了氮亏缺对玉米单根径、轴向导度的影响。

• 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。

• In quantitative study of the interaction between the lake water and groundwater, the hydraulic conductivity of lake bed sediment is a very important parameter.

  在湖水与地下水相互作用的定量研究中，湖底沉积物的渗透系数是极其重要的参数之一。

• The unsaturated hydraulic conductivity is a key parameter of porous media applied to groundwater pollution prediction and assessment.

  多孔介质非饱和导水率是地下水污染预测与评价的重要参数。

• Through the finite element model and using formulas given in this paper the changes of hydraulic conductivity in a mining face are examined.

  利用此关系式及有限元方法计算，得出了裂隙巖体渗透系数随应力的变化值。

• Effects of different tillage methods on saturated hydraulic conductivity and compactiveness of the surface soil;

  研究了不同耕作方式对土壤物理特性、水分状况、甘蔗苗期生长的影响 。

• The effect of irrigation water quality on unsaturated hydraulic conductivity (k) of undisturbed soil and its mechanism were studied.

  本文研究了灌溉水质对田间原状土壤非饱和导水率的影响及其机理。

• 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。

• Decreasing hydraulic conductivity and diffusion coefficient may delay the increasing rate of the concentration ratio at the base of a GCL.

  结果表明，减小渗透系数和扩散系数可以有效减缓衬垫底部浓度比的增加速度。

• 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。

• 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。

• It is of practical value to determine the hydraulic conductivity tensors of large-scale dynamo-relaxed rock masses at site of Daliushu dam on the Yellow River and to analyze the seepage field.

  黄河大柳树水利枢纽坝区巖体大范围发生了松动，确定其水力学特性指标并进行渗流分析具有重要的现实意义。

• This analysis indicated that the hydraulic conductivity could not be assumed as a constant value when groundwater flow was simulated with numerical model.

  因此，在进行现地地下水流数值模拟时，水力传导系数不能只假设为单一值。

• On the assumption that the hydraulic conductivity field follows a lognormal distribution, the direct Fourier transform is introduced to generate multiple realizations of hydraulic conductivity field.

  据以往研究，假设渗透系数场遵循对数正态分布，利用直接傅立叶变换方法来生成渗透系数随机场。