2020
DOI: 10.1177/0036850420930982
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Distribution law of floor stress during mining of the upper protective coal seam

Abstract: Floor stress distribution is the main index for evaluating the mining effect of upper protective coal seam. However, parameters currently used in theoretical analysis of mining-induced stress lack practicality. Therefore, in this article, a model for calculating floor stress during mining of upper protective coal seams was established based on the theory of elastic mechanics. Subsequently, the stress induced by the abutment pressure at any point in the five parts of the floor was derived. Moreover, the distrib… Show more

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Cited by 7 publications
(8 citation statements)
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References 45 publications
(47 reference statements)
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“…According to reference [20], the pressure of key block B on small coal pillar can be approximately considered as follows :…”
Section: Main Roof Fracture Structure Form Of Island Working Facementioning
confidence: 99%
“…According to reference [20], the pressure of key block B on small coal pillar can be approximately considered as follows :…”
Section: Main Roof Fracture Structure Form Of Island Working Facementioning
confidence: 99%
“…After the upper protective layer is mined, the roof and floor coal strata in the goaf will periodically appear in three stages, compression, expansion, and recovery, with the advancement of the working face [21]. In order to better study the characteristics of the bottom and roof collapse, the collapse characteristics when the working face is advanced to 30 m, 50 m, 80 m, and 140 m were selected for analysis.…”
Section: Analysis Of Collapse Characteristics Of Working Face Advanci...mentioning
confidence: 99%
“…However, when the working face is being mined back, the bottom plate is affected by the mining of the working face, and the stress is transferred to the deep part of the bottom plate of the working face of the roadway, which redistributes the stress in the rock surrounding the bottom plate. Then, there is a nonuniform stress field, i.e., a two-way unequal compressive stress field, in the rock surrounding the bottom plate, which results in different degrees of damage to the rock surrounding the bottom plate in different locations [6][7][8]. The damage to the bottom plate rock at different locations is caused by the nonuniform stress field.…”
Section: Introductionmentioning
confidence: 99%