Experimental Study on Reynolds Number Evolution of Gas-Filled Coal

The flow state of gas in coals is very complicated. We should pay attention to whether the permeability calculated by Darcy’s law is in accordance with the actual situation. We conducted an experiment on coal permeability and deformation under fixing confining pressure and increasing axial stress co...

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Main Authors: Chao Liu, Minghui Li, Honggang Zhao
Format: Article
Language:English
Published: Hindawi-Wiley 2019-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2019/7965918
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spelling doaj-ebb1216cea5e4ab7a12da0915389a2cc2020-11-25T02:36:02ZengHindawi-WileyGeofluids1468-81151468-81232019-01-01201910.1155/2019/79659187965918Experimental Study on Reynolds Number Evolution of Gas-Filled CoalChao Liu0Minghui Li1Honggang Zhao2State Key Laboratory of Coal Mine Disaster Dynamics and Control, Chongqing University, Chongqing 400030, ChinaState Key Laboratory of Coal Mine Disaster Dynamics and Control, Chongqing University, Chongqing 400030, ChinaState Key Laboratory of Coal Mine Disaster Dynamics and Control, Chongqing University, Chongqing 400030, ChinaThe flow state of gas in coals is very complicated. We should pay attention to whether the permeability calculated by Darcy’s law is in accordance with the actual situation. We conducted an experiment on coal permeability and deformation under fixing confining pressure and increasing axial stress conditions. The objective is to investigate the variation of Reynolds number Re. In this study, the dynamic evolution of the Reynolds number is calculated under the relevant assumptions. The Reynolds number increases with an increase in the axial stress. In addition, the larger the value of initial Reynolds numbers, the greater the value of Re in the postpeak, and the possibility of nonlinear flow state is higher. Further, if the mass density (ρ) and fluid viscosity (μ) are constant, the decrease in the amplitudes of the flow rate is less than the increase in the equivalent diameter of the seepage path. Moreover, the tensile stress generated around the pores and fractures parallel or nearly parallel to the axial stress direction with increase in the axial stress results in an increase in the Reynolds numbers and equivalent diameter of the seepage path increase due to the development, expansion, and penetration of the cracks.http://dx.doi.org/10.1155/2019/7965918
collection DOAJ
language English
format Article
sources DOAJ
author Chao Liu
Minghui Li
Honggang Zhao
spellingShingle Chao Liu
Minghui Li
Honggang Zhao
Experimental Study on Reynolds Number Evolution of Gas-Filled Coal
Geofluids
author_facet Chao Liu
Minghui Li
Honggang Zhao
author_sort Chao Liu
title Experimental Study on Reynolds Number Evolution of Gas-Filled Coal
title_short Experimental Study on Reynolds Number Evolution of Gas-Filled Coal
title_full Experimental Study on Reynolds Number Evolution of Gas-Filled Coal
title_fullStr Experimental Study on Reynolds Number Evolution of Gas-Filled Coal
title_full_unstemmed Experimental Study on Reynolds Number Evolution of Gas-Filled Coal
title_sort experimental study on reynolds number evolution of gas-filled coal
publisher Hindawi-Wiley
series Geofluids
issn 1468-8115
1468-8123
publishDate 2019-01-01
description The flow state of gas in coals is very complicated. We should pay attention to whether the permeability calculated by Darcy’s law is in accordance with the actual situation. We conducted an experiment on coal permeability and deformation under fixing confining pressure and increasing axial stress conditions. The objective is to investigate the variation of Reynolds number Re. In this study, the dynamic evolution of the Reynolds number is calculated under the relevant assumptions. The Reynolds number increases with an increase in the axial stress. In addition, the larger the value of initial Reynolds numbers, the greater the value of Re in the postpeak, and the possibility of nonlinear flow state is higher. Further, if the mass density (ρ) and fluid viscosity (μ) are constant, the decrease in the amplitudes of the flow rate is less than the increase in the equivalent diameter of the seepage path. Moreover, the tensile stress generated around the pores and fractures parallel or nearly parallel to the axial stress direction with increase in the axial stress results in an increase in the Reynolds numbers and equivalent diameter of the seepage path increase due to the development, expansion, and penetration of the cracks.
url http://dx.doi.org/10.1155/2019/7965918
work_keys_str_mv AT chaoliu experimentalstudyonreynoldsnumberevolutionofgasfilledcoal
AT minghuili experimentalstudyonreynoldsnumberevolutionofgasfilledcoal
AT honggangzhao experimentalstudyonreynoldsnumberevolutionofgasfilledcoal
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