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...
| Main Authors: | , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Public Library of Science (PLoS)
2020-01-01
|
| Series: | PLoS ONE |
| Online Access: | https://doi.org/10.1371/journal.pone.0228264 |
| _version_ | 1819147300724801536 |
|---|---|
| author | Weiyong Lu Changchun He Xin Zhang |
| author_facet | Weiyong Lu Changchun He Xin Zhang |
| author_sort | Weiyong Lu |
| collection | DOAJ |
| 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. |
| first_indexed | 2024-12-22T13:27:38Z |
| format | Article |
| id | doaj.art-b9f5cda37af140018e93e3f2e718405e |
| institution | Directory Open Access Journal |
| issn | 1932-6203 |
| language | English |
| last_indexed | 2024-12-22T13:27:38Z |
| publishDate | 2020-01-01 |
| publisher | Public Library of Science (PLoS) |
| record_format | Article |
| series | PLoS ONE |
| spelling | doaj.art-b9f5cda37af140018e93e3f2e718405e2022-12-21T18:24:17ZengPublic Library of Science (PLoS)PLoS ONE1932-62032020-01-01151e022826410.1371/journal.pone.0228264Height of overburden fracture based on key strata theory in longwall face.Weiyong LuChangchun HeXin ZhangAmong 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.https://doi.org/10.1371/journal.pone.0228264 |
| spellingShingle | Weiyong Lu Changchun He Xin Zhang Height of overburden fracture based on key strata theory in longwall face. PLoS ONE |
| 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 |
| url | https://doi.org/10.1371/journal.pone.0228264 |
| work_keys_str_mv | AT weiyonglu heightofoverburdenfracturebasedonkeystratatheoryinlongwallface AT changchunhe heightofoverburdenfracturebasedonkeystratatheoryinlongwallface AT xinzhang heightofoverburdenfracturebasedonkeystratatheoryinlongwallface |