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    Liu Tianqi, Wang Bingguo, Zhang Junshuai, Duan Yan, 2021. Variation Law and Influencing Factors of Soil Saturated Hydraulic Conductivity in Jianghan Plain. Earth Science, 46(2): 671-682. doi: 10.3799/dqkx.2020.039
    Citation: Liu Tianqi, Wang Bingguo, Zhang Junshuai, Duan Yan, 2021. Variation Law and Influencing Factors of Soil Saturated Hydraulic Conductivity in Jianghan Plain. Earth Science, 46(2): 671-682. doi: 10.3799/dqkx.2020.039

    Variation Law and Influencing Factors of Soil Saturated Hydraulic Conductivity in Jianghan Plain

    doi: 10.3799/dqkx.2020.039
    • Received Date: 2019-12-12
    • Publish Date: 2021-02-15
    • At present,there is no deep understanding of the mechanism that affects the law of soil saturated hydraulic conductivity. The shallow soils in the lower reaches of Hanjiang River in Jianghan Plain from different sedimentary environment,lithologies and land use were sampled to carry out the variable head Darcy experiment by improved soil permeation instrument (TST-55).The results show that the mean soil saturated hydraulic conductivity is 4.94×10-5cm/s with log-normal distribution. In silty loam,the mean value of soil saturated hydraulic conductivity for alluvium and lacustrine deposits are 3.53×10-5cm/s and 1.98×10-5cm/s respectively,and the mean value for them is 8.13×10-7cm/s and 5.88×10-7cm/s in silty clay loam. For the same lithology,soil saturated hydraulic conductivity of alluvial sediments is obviously larger than that of lacustrine sediment. The average soil saturated hydraulic conductivity of sandy loam,silty loam and silty clay loam from high to low are 1.98×10-5cm/s,3.53×10-5cm/s and 8.13×10-7cm/s,respectively. The mean soil saturated hydraulic conductivities of silty loam and silty clay loam in cultivated soil are 3.75×10-5cm/s and 8.11×10-7cm/s,while the mean value of them are 1.88×10-6cm/s and 5.93×10-7cm/s in non-cultivated soil. The soil saturated hydraulic conductivity of cultivated soils is also higher than that of non-cultivated soils.

       

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