江汉平原土壤饱和渗透系数变化规律及影响因素

刘天奇; 汪丙国; 张钧帅; 段燕

doi:10.3799/dqkx.2020.039

Volume 46 Issue 2

Feb. 2021

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Article Navigation > Earth Science > 2021 > 46(2): 671-682

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

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

doi: 10.3799/dqkx.2020.039

School of Environmental Studies, China University of Geosciences, Wuhan 430078, China

Received Date: 2019-12-12
Publish Date: 2021-02-15

Abstract

Abstract

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.
- Jianghan Plain,
- soil saturated hydraulic conductivity,
- variable head Darcy method,
- variation law,
- influencing factor,
- hydrogeology

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

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