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Height of overburden fracture based on key strata theory in longwall face
Among the three overburden zones (the caving zone, the fracture zone, and the continuous deformation zone) in longwall coal mining, the continuous deformation zone is often considered to be continuous without cracks, so continuum mechanics can be used to calculate the subsidence of overburden strata...
Autores principales: | , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Public Library of Science
2020
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6980533/ https://www.ncbi.nlm.nih.gov/pubmed/31978195 http://dx.doi.org/10.1371/journal.pone.0228264 |
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author | Lu, Weiyong He, Changchun Zhang, Xin |
author_facet | Lu, Weiyong He, Changchun Zhang, Xin |
author_sort | Lu, Weiyong |
collection | PubMed |
description | Among the three overburden zones (the caving zone, the fracture zone, and the continuous deformation zone) in longwall coal mining, the continuous deformation zone is often considered to be continuous without cracks, so continuum mechanics can be used to calculate the subsidence of overburden strata. Longwall coal mining, however, will induce the generation of wide cracks in the surface and thus may cause the continuous deformation zone to fracture. In this paper, whether there are cracks in the continuous deformation zone as well as the height of overburden fracture in longwall face and the subsidence and deformation of strata of different fracture penetration ratios were studied by means of physical simulation, theoretical analysis and numerical simulation. The results show that: (1) Rock stratum starts to fracture as long as it has slightly subsided for only tens of millimeters, and the height of fracture development is the height of working face overburden. (2) With the increase of fracture penetration ratio, the subsidence of key strata remains basically unchanged; the surface deformation range and the maximum compression deformation decrease, while the maximum horizontal movement and maximum horizontal tensile deformation increase. Therefore, the subsidence of overburden strata which have fractured but have not broken can be calculated through the continuum mechanics method. |
format | Online Article Text |
id | pubmed-6980533 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2020 |
publisher | Public Library of Science |
record_format | MEDLINE/PubMed |
spelling | pubmed-69805332020-02-04 Height of overburden fracture based on key strata theory in longwall face Lu, Weiyong He, Changchun Zhang, Xin PLoS One Research Article Among the three overburden zones (the caving zone, the fracture zone, and the continuous deformation zone) in longwall coal mining, the continuous deformation zone is often considered to be continuous without cracks, so continuum mechanics can be used to calculate the subsidence of overburden strata. Longwall coal mining, however, will induce the generation of wide cracks in the surface and thus may cause the continuous deformation zone to fracture. In this paper, whether there are cracks in the continuous deformation zone as well as the height of overburden fracture in longwall face and the subsidence and deformation of strata of different fracture penetration ratios were studied by means of physical simulation, theoretical analysis and numerical simulation. The results show that: (1) Rock stratum starts to fracture as long as it has slightly subsided for only tens of millimeters, and the height of fracture development is the height of working face overburden. (2) With the increase of fracture penetration ratio, the subsidence of key strata remains basically unchanged; the surface deformation range and the maximum compression deformation decrease, while the maximum horizontal movement and maximum horizontal tensile deformation increase. Therefore, the subsidence of overburden strata which have fractured but have not broken can be calculated through the continuum mechanics method. Public Library of Science 2020-01-24 /pmc/articles/PMC6980533/ /pubmed/31978195 http://dx.doi.org/10.1371/journal.pone.0228264 Text en © 2020 Lu et al http://creativecommons.org/licenses/by/4.0/ This is an open access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/) , which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. |
spellingShingle | Research Article Lu, Weiyong He, Changchun Zhang, Xin Height of overburden fracture based on key strata theory in longwall face |
title | Height of overburden fracture based on key strata theory in longwall face |
title_full | Height of overburden fracture based on key strata theory in longwall face |
title_fullStr | Height of overburden fracture based on key strata theory in longwall face |
title_full_unstemmed | Height of overburden fracture based on key strata theory in longwall face |
title_short | Height of overburden fracture based on key strata theory in longwall face |
title_sort | height of overburden fracture based on key strata theory in longwall face |
topic | Research Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6980533/ https://www.ncbi.nlm.nih.gov/pubmed/31978195 http://dx.doi.org/10.1371/journal.pone.0228264 |
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