Prevention of Water Inrushes in Deep Coal Mining over the Ordovician Aquifer: A Case Study in the Wutongzhuang Coal Mine of China

Through field observation and theoretical study, we found that the Hanxing mining area has a typical ternary structure in coal mining under high water pressure of the aquifer. This ternary structure is the Ordovician limestone aquifer-aquiclude including thin limestones-coal seam. Although the aquic...

Full description

Bibliographic Details
Main Authors: Huichao Yin, Bin Xu, Shangxian Yin, Wuzi Tian, Hui Yao, Haopeng Meng
Format: Article
Language:English
Published: Hindawi-Wiley 2021-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2021/5208670
id doaj-b102d2a174814252b48e9117f00883df
record_format Article
spelling doaj-b102d2a174814252b48e9117f00883df2021-09-27T00:53:04ZengHindawi-WileyGeofluids1468-81232021-01-01202110.1155/2021/5208670Prevention of Water Inrushes in Deep Coal Mining over the Ordovician Aquifer: A Case Study in the Wutongzhuang Coal Mine of ChinaHuichao Yin0Bin Xu1Shangxian Yin2Wuzi Tian3Hui Yao4Haopeng Meng5China University of Mining and TechnologyNorth China Institute of Science and TechnologyNorth China Institute of Science and TechnologyNorth China Institute of Science and TechnologyNorth China Institute of Science and TechnologyNorth China Institute of Science and TechnologyThrough field observation and theoretical study, we found that the Hanxing mining area has a typical ternary structure in coal mining under high water pressure of the aquifer. This ternary structure is the Ordovician limestone aquifer-aquiclude including thin limestones-coal seam. Although the aquiclude is considerably thick, there is still a great risk of water burst during mining under water pressure in the deep burial environment. Multidimensional characteristics of floor water inrush in deep mining are summarized in the paper, including water migration upwardly driven by the Ordovician confined water, the planar dispersion of the water inrush channel, the stepped increase of the water inrush intensity, the hysteretic effluent of the water inrush time and the exchange, and adsorption of the water quality. The water inrush mechanism is clarified that the permeability, dilatancy, fracturing, and ascending of the water from the Ordovician limestone aquifer form a planar and divergent flow through the transfer, storage, and transportation of thin limestone aquifers. The corresponding water inrush risk evaluation equation is also proposed. Based on the thickness of the aquiclude, the thickness of the failure zones, and the water inrush coefficient, the floor aquiclude is classified into five categories. While water inrush cannot be completely controlled by the traditional underground floor reinforcement with ultra-thick aquiclude or even zonal grouting, a comprehensive prevention and control concept of the four-dimensional floor water hazard in full time-space domain are proposed. A tridimensional prevention and control model of three-dimensional reticulated exploration, treatment, verification, and supplementation is presented. A full time domain technological quality control process of condition assessment, exploration, remediation, inspection, evaluation, monitoring, and reassurance is formed, and a water disaster prevention method with full time-space tridimensional network in deep coal mining is established. Case study in the Hanxing mining area demonstrates that the proposed methods are highly effective.http://dx.doi.org/10.1155/2021/5208670
collection DOAJ
language English
format Article
sources DOAJ
author Huichao Yin
Bin Xu
Shangxian Yin
Wuzi Tian
Hui Yao
Haopeng Meng
spellingShingle Huichao Yin
Bin Xu
Shangxian Yin
Wuzi Tian
Hui Yao
Haopeng Meng
Prevention of Water Inrushes in Deep Coal Mining over the Ordovician Aquifer: A Case Study in the Wutongzhuang Coal Mine of China
Geofluids
author_facet Huichao Yin
Bin Xu
Shangxian Yin
Wuzi Tian
Hui Yao
Haopeng Meng
author_sort Huichao Yin
title Prevention of Water Inrushes in Deep Coal Mining over the Ordovician Aquifer: A Case Study in the Wutongzhuang Coal Mine of China
title_short Prevention of Water Inrushes in Deep Coal Mining over the Ordovician Aquifer: A Case Study in the Wutongzhuang Coal Mine of China
title_full Prevention of Water Inrushes in Deep Coal Mining over the Ordovician Aquifer: A Case Study in the Wutongzhuang Coal Mine of China
title_fullStr Prevention of Water Inrushes in Deep Coal Mining over the Ordovician Aquifer: A Case Study in the Wutongzhuang Coal Mine of China
title_full_unstemmed Prevention of Water Inrushes in Deep Coal Mining over the Ordovician Aquifer: A Case Study in the Wutongzhuang Coal Mine of China
title_sort prevention of water inrushes in deep coal mining over the ordovician aquifer: a case study in the wutongzhuang coal mine of china
publisher Hindawi-Wiley
series Geofluids
issn 1468-8123
publishDate 2021-01-01
description Through field observation and theoretical study, we found that the Hanxing mining area has a typical ternary structure in coal mining under high water pressure of the aquifer. This ternary structure is the Ordovician limestone aquifer-aquiclude including thin limestones-coal seam. Although the aquiclude is considerably thick, there is still a great risk of water burst during mining under water pressure in the deep burial environment. Multidimensional characteristics of floor water inrush in deep mining are summarized in the paper, including water migration upwardly driven by the Ordovician confined water, the planar dispersion of the water inrush channel, the stepped increase of the water inrush intensity, the hysteretic effluent of the water inrush time and the exchange, and adsorption of the water quality. The water inrush mechanism is clarified that the permeability, dilatancy, fracturing, and ascending of the water from the Ordovician limestone aquifer form a planar and divergent flow through the transfer, storage, and transportation of thin limestone aquifers. The corresponding water inrush risk evaluation equation is also proposed. Based on the thickness of the aquiclude, the thickness of the failure zones, and the water inrush coefficient, the floor aquiclude is classified into five categories. While water inrush cannot be completely controlled by the traditional underground floor reinforcement with ultra-thick aquiclude or even zonal grouting, a comprehensive prevention and control concept of the four-dimensional floor water hazard in full time-space domain are proposed. A tridimensional prevention and control model of three-dimensional reticulated exploration, treatment, verification, and supplementation is presented. A full time domain technological quality control process of condition assessment, exploration, remediation, inspection, evaluation, monitoring, and reassurance is formed, and a water disaster prevention method with full time-space tridimensional network in deep coal mining is established. Case study in the Hanxing mining area demonstrates that the proposed methods are highly effective.
url http://dx.doi.org/10.1155/2021/5208670
work_keys_str_mv AT huichaoyin preventionofwaterinrushesindeepcoalminingovertheordovicianaquiferacasestudyinthewutongzhuangcoalmineofchina
AT binxu preventionofwaterinrushesindeepcoalminingovertheordovicianaquiferacasestudyinthewutongzhuangcoalmineofchina
AT shangxianyin preventionofwaterinrushesindeepcoalminingovertheordovicianaquiferacasestudyinthewutongzhuangcoalmineofchina
AT wuzitian preventionofwaterinrushesindeepcoalminingovertheordovicianaquiferacasestudyinthewutongzhuangcoalmineofchina
AT huiyao preventionofwaterinrushesindeepcoalminingovertheordovicianaquiferacasestudyinthewutongzhuangcoalmineofchina
AT haopengmeng preventionofwaterinrushesindeepcoalminingovertheordovicianaquiferacasestudyinthewutongzhuangcoalmineofchina
_version_ 1716867417240502272