江汉平原第四系弱透水层渗透系数求算方法

张婧玮; 梁杏; 葛勤; 李惠; 朱波

doi:10.3799/dqkx.2017.064

Volume 42 Issue 5

May 2017

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Article Navigation > Earth Science > 2017 > 42(5): 761-770

Zhang Jingwei, Liang Xing, Ge Qin, Li Hui, Zhu Bo, 2017. Calculation Method about Hydraulic Conductivity of Quaternary Aquitard in Jianghan Plain. Earth Science, 42(5): 761-770. doi: 10.3799/dqkx.2017.064

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Zhang Jingwei, Liang Xing, Ge Qin, Li Hui, Zhu Bo, 2017. Calculation Method about Hydraulic Conductivity of Quaternary Aquitard in Jianghan Plain. Earth Science, 42(5): 761-770. doi: 10.3799/dqkx.2017.064

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Calculation Method about Hydraulic Conductivity of Quaternary Aquitard in Jianghan Plain

doi: 10.3799/dqkx.2017.064

Zhang Jingwei^1
,,
Liang Xing^{1,2
,
,},
Ge Qin¹,
Li Hui¹,
Zhu Bo¹

1.
School of Environmental Studies, China University of Geosciences, Wuhan 430074, China
2.
Laboratory of Basin Hydrology and Wetland Eco-Restoration, China University of Geosciences, Wuhan 430074, China

Received Date: 2016-12-27
Publish Date: 2017-05-15

Abstract

Abstract

The hydraulic conductivity of aquitard is an important parameter for the regional groundwater flow system and the effect of water-soil-biology in critical zone. Taking the 1:50 000 Yanglinwei-Luxikou in Jianghan plain as typical study area combining with the investigation of critical zone, 52 sediment samples from different depth and lithology were collected to conduct the laboratorial penetration test with improved permeameter, and amend the empirical formula of clay with K and granularity characteristic parameters. The results show that: the hydraulic conductivity of sediments related to lithology and large variability, range from 10^-10 to 10^-6 m/s; pore phreatic aquifer group mainly consists of silty clay and clay, hydraulic conductivity and variability is small, sedimentary environment is relatively stable; artesian aquifer group due to the continuous distribution of clay and silt, leading to large hydraulic conductivity and variability, present multicycle sedimentary environment of typical river-lake interaction. Utilize the significant binomial relation with effective pore ratio (e_u) and clay content (P), amend Terzaghi's empirical formula, and predicted data and experimental data are coincided basically, the range of specific value is less than an order of magnitude, validating the feasibility of amended Terzaghi's formula in river-lake plain.
- Jianghan plain,
- hydraulic conductivity,
- clay,
- Terzaghi's empirical formula,
- groundwater,
- hydrogeology

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References(44)

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Calculation Method about Hydraulic Conductivity of Quaternary Aquitard in Jianghan Plain

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