Articles | Volume 26, issue 13
https://doi.org/10.5194/hess-26-3359-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/hess-26-3359-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
05 Jul 2022
Research article |
| 05 Jul 2022
| 05 Jul 2022
Experimental study of non-Darcy flow characteristics in permeable stones
Zhongxia Li
School of Environmental Studies, China University of Geosciences, Wuhan, Hubei, 430074, China
Junwei Wan
School of Environmental Studies, China University of Geosciences, Wuhan, Hubei, 430074, China
Tao Xiong
School of Environmental Studies, China University of Geosciences, Wuhan, Hubei, 430074, China
Hongbin Zhan
CORRESPONDING AUTHOR
Department of Geology and Geophysics, Texas A & M University,
College Station, TX 77843-3115, USA
Linqing He
Changjiang Institute of Survey Technical Research MWR, Wuhan, China
Kun Huang
CORRESPONDING AUTHOR
School of Environmental Studies, China University of Geosciences, Wuhan, Hubei, 430074, China
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Short summary
Four permeable rocks with different pore sizes were considered to provide experimental evidence of Forchheimer flow and the transition between different flow regimes. The mercury injection technique was used to measure the pore size distribution, which is an essential factor for determining the flow regime, for four permeable stones. Finally, the influences of porosity and particle size on the Forchheimer coefficients were discussed.
Four permeable rocks with different pore sizes were considered to provide experimental evidence...
Special issue