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The Study of Low-velocity Non-Darcy Flow for Low-permeability Media in North China Plain

Published: 31 May 2022 Publication History

Abstract

Vertical leakage across low-permeability strata and underflow from adjacent aquifers (interaquifer flows) can be important sources of recharge for groundwater aquifer. However, in low-permeability porous media, due to small-size pores in porous media and throat radius of a few micrometers, molecular force on the solid-liquid interface increases significantly, which leads to the low-velocity non-Darcy flow. Conventional groundwater modeling methods assume that groundwater flow is described by Darcian principles which are inadequate when the flow is low-velocity non-Darcy flow. In this study, experiments are performed to explore the mathematical relation between flow rate and hydraulic gradient of low-permeability media in North China Plain of China. Mathematical equation has been obtained by curve fitting method based on experiment data.

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BIC '22: Proceedings of the 2022 2nd International Conference on Bioinformatics and Intelligent Computing
January 2022
551 pages
ISBN:9781450395755
DOI:10.1145/3523286
Permission to make digital or hard copies of all or part of this work for personal or classroom use is granted without fee provided that copies are not made or distributed for profit or commercial advantage and that copies bear this notice and the full citation on the first page. Copyrights for components of this work owned by others than ACM must be honored. Abstracting with credit is permitted. To copy otherwise, or republish, to post on servers or to redistribute to lists, requires prior specific permission and/or a fee. Request permissions from [email protected]

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Association for Computing Machinery

New York, NY, United States

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Published: 31 May 2022

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