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Evaluating the scale dependency of measured hydraulic conductivity using double-ring infiltrometers and numerical simulation

机译:使用双环渗透仪和数值模拟评估测量水力传导率的比例依赖性

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Saturated hydraulic conductivity measurements are important for understanding and modeling hydrological processes at the field scale. Few systematic studies have been conducted on how the size of double-ring infiltrometers affects the measured hydraulic conductivity. To determine this size effect, we measured saturated hydraulic conductivity at seven sites using four different sizes of double-ring infiltrometers. Inner ring diameters d_i were 20, 40, 80, and 120 cm. Detailed numerical investigationswere also conducted to explain how the inner-ring size of a double-ring infiltrometer influences the measured hydraulic conductivity in a heterogeneous soil. Field and simulation results both demonstrated that the variability of measured hydraulic conductivity was greater for smaller inner rings (e.g. d_i< 40 cm), and it gradually decreases as the ring size increases. Our study indicates that where soil spatial variability is high, infiltrometers having a large inner ring (in general > 80 cm) are essential for reliable measurement.
机译:饱和液压导电性测量对于在现场规模上理解和建模水文过程是重要的。关于双环渗透仪的尺寸如何影响测量的液压导电性的少量系统研究。为了确定这种尺寸的效果,我们使用四种不同尺寸的双环渗透仪测量饱和液压导电性。内环直径D_i为20,40,80和120厘米。详细的数值研究还进行了解释双环渗透表的内圈尺寸如何影响异质土壤中的测量的液压导电性。场和仿真结果既表明,测量的液压导电率的可变性对于较小的内圈(例如D_I <40cm)越大,并且随着环尺寸的增加而逐渐减小。我们的研究表明,在土壤空间可变性高的情况下,具有大内环的渗透仪(通常> 80cm)对于可靠的测量是必不可少的。

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