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New approach to improve soil-water characteristic curve to reduce variation in estimation of unsaturated permeability function

机译:改善土壤-水特征曲线以减少非饱和渗透率函数估计变化的新方法

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The unsaturated permeability function is often estimated from the soil-water characteristic curve (SWCC) of a soil. A complete SWCC measurement can improve the estimation of the unsaturated permeability function. In most laboratories, the SWCC can be measured up to a suction of 100 kPa using a Tempe cell. However, complete measurement of the SWCC is an expensive and time-consuming task. Therefore, this paper presents a new approach to estimate SWCC data points beyond 100 kPa suction to complement the SWCC measured up to a suction of 100 kPa. The new SWCC is then used to estimate the unsaturated permeability function. The proposed approach uses knowledge of the grain-size distribution curve and measured SWCC data at 100 kPa suction to estimate the SWCC data points beyond 100 kPa suction. To verify the proposed procedure, SWCC tests were conducted over a wide range of suctions for coarse kaolin and a triaxial permeameter system was used to directly measure unsaturated permeability of the coarse kaolin. The proposed procedure is found to reduce the variation between unsaturated permeability functions estimated by various estimation models.
机译:非饱和渗透率函数通常是根据土壤的土壤水特征曲线(SWCC)估算的。完整的SWCC测量可以改善对非饱和渗透率函数的估计。在大多数实验室中,使用Tempe池可以测量SWCC的最大吸力为100 kPa。但是,完整测量SWCC是一项昂贵且耗时的任务。因此,本文提出了一种新的方法来估算超过100 kPa吸力的SWCC数据点,以补充测量到100 kPa吸力的SWCC。然后使用新的SWCC估算非饱和渗透率函数。所提出的方法利用了粒度分布曲线的知识以及在100 kPa吸力下测得的SWCC数据,以估算100 kPa吸力以外的SWCC数据点。为了验证所提出的程序,对粗高岭土的吸力进行了广泛的SWCC测试,并使用三轴渗透仪系统直接测量了粗高岭土的不饱和渗透率。发现所提出的程序减少了由各种估计模型估计的非饱和渗透率函数之间的变化。

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