含水岩组概化的累积导水系数法

白宏伟; 刘延锋; 靳孟贵

doi:10.3799/dqkx.2017.069

Volume 42 Issue 5

May 2017

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Bai Hongwei, Liu Yanfeng, Jin Menggui, 2017. Generalization of Aquifer Group by Cumulative Transmissivity Method. Earth Science, 42(5): 813-820. doi: 10.3799/dqkx.2017.069

Citation:

Bai Hongwei, Liu Yanfeng, Jin Menggui, 2017. Generalization of Aquifer Group by Cumulative Transmissivity Method. Earth Science, 42(5): 813-820. doi: 10.3799/dqkx.2017.069

Bai Hongwei, Liu Yanfeng, Jin Menggui, 2017. Generalization of Aquifer Group by Cumulative Transmissivity Method. Earth Science, 42(5): 813-820. doi: 10.3799/dqkx.2017.069

Citation:

Bai Hongwei, Liu Yanfeng, Jin Menggui, 2017. Generalization of Aquifer Group by Cumulative Transmissivity Method. Earth Science, 42(5): 813-820. doi: 10.3799/dqkx.2017.069

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Generalization of Aquifer Group by Cumulative Transmissivity Method

doi: 10.3799/dqkx.2017.069

Bai Hongwei^{1,2
,},
Liu Yanfeng^1,2,
Jin Menggui^{1,2
,
,}

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

Received Date: 2016-12-17
Publish Date: 2017-05-15

Abstract

Abstract

Groundwater flow system theory and numerical simulation technique are foundamentals in hydrogeology. Generalizing aquifer group is an important foundation for groundwater flow system analysis and numerical simulation, which directly affects the accuracy and the reliability of the simulation results. This paper proposes a new method named cumulative transmissivity to generalize aquifer group, aiming at improving the generalization accuracy and reliability. The new method is characterized by aquifer structure based on the changes of the accumulated transmissivity (product of hydraulic conductivity and its thickness) with depth and the integral characteristics of the hydrogeological profile. A case study in the Manas River basin is presented in this paper. Based on the generalization, a hydrogeological structure model is built using the GMS software and its TINS module. The results indicate that the aquifer structures generalized using this method have a high rationality and fidelity. The 3D model well displays the spatial distribution of the aquifers and auitards in the study area and provides a good foundation for groundwater flow model.
- aquifer group,
- cumulative transmissivity method,
- structure model,
- generalization,
- hydraulic conductivity,
- groundwater,
- hydrogeology

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References(41)

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Generalization of Aquifer Group by Cumulative Transmissivity Method

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