'Three hole' in-situ test and evaluation of fault impermeability of coal seam floor

The double-hole method in-situ pressure permeability test technology adopts single-direction pressure permeability test without considering the direction and anisotropy of rock fissures. The results are quite different from the actual situation of multi-directional compression of complex rock strata...

Full description

Bibliographic Details
Main Authors: DAI Lei, DUAN Lihong
Format: Article
Language:zho
Published: Editorial Department of Industry and Mine Automation 2022-05-01
Series:Gong-kuang zidonghua
Subjects:
Online Access:http://www.gkzdh.cn/article/doi/10.13272/j.issn.1671-251x.2021110018
_version_ 1797869011468288000
author DAI Lei
DUAN Lihong
author_facet DAI Lei
DUAN Lihong
author_sort DAI Lei
collection DOAJ
description The double-hole method in-situ pressure permeability test technology adopts single-direction pressure permeability test without considering the direction and anisotropy of rock fissures. The results are quite different from the actual situation of multi-directional compression of complex rock strata. The 'three-hole' in-situ pressure permeability test method is adopted to conduct forward water pressure test and reverse water pressure test on FN-6 normal fault of the second horizontal coal seam in Chengjiao Coal Mine. Three holes are arranged in a typical roadway for water injection and water pressure monitoring respectively. The first water pressure test is a forward water pressure test, and the second water pressure test is a reverse water pressure test. The point where the water pressure and pressure permeability flow volume of the water pressure monitoring hole change synchronously with the water injection pressure is taken as the initial permeability characteristic point. And the corresponding water injection pressure is determined as the initial permeability pressure. If the water injection pressure continues to increase according to the design pressure, the permeability pressure is smaller than the water injection pressure and remains stable, and the water injection flow is relatively stable, it indicates that in the original state, the in-situ rock stratum has extremely strong permeability resistance and it is an aquifuge. On the contrary, it is a diversion fissure zone. The test results of the forward water pressure test shows that the water conductivity of the upper section of the FN-6 normal fault is extremely weak in the initial state. This section is an aquifuge. With the increase of water injection pressure, the rock mass between the water pressure hole and the water pressure monitoring hole is densely split, resulting in fissures. However, the scale and water conductivity are relatively small, and only seepage from micro fissures is dominant. During the reverse water pressure test, the number of water diversion channels is increased compared with that in the forward water pressure test. This leads to the decrease of the pressure difference between the water pressure hole and the water pressure monitoring hole. And the dominant water diversion channel is formed between the water pressure monitoring hole and the water pressure hole. The actual permeability state can be formed only when the critical permeability pressure (the critical permeability pressure of FN-6 normal fault is 11 MPa) is exceeded.
first_indexed 2024-04-10T00:05:57Z
format Article
id doaj.art-bd84a8e1e63942eaae22f492d9752d84
institution Directory Open Access Journal
issn 1671-251X
language zho
last_indexed 2024-04-10T00:05:57Z
publishDate 2022-05-01
publisher Editorial Department of Industry and Mine Automation
record_format Article
series Gong-kuang zidonghua
spelling doaj.art-bd84a8e1e63942eaae22f492d9752d842023-03-17T01:02:43ZzhoEditorial Department of Industry and Mine AutomationGong-kuang zidonghua1671-251X2022-05-0148512813210.13272/j.issn.1671-251x.2021110018'Three hole' in-situ test and evaluation of fault impermeability of coal seam floorDAI LeiDUAN LihongThe double-hole method in-situ pressure permeability test technology adopts single-direction pressure permeability test without considering the direction and anisotropy of rock fissures. The results are quite different from the actual situation of multi-directional compression of complex rock strata. The 'three-hole' in-situ pressure permeability test method is adopted to conduct forward water pressure test and reverse water pressure test on FN-6 normal fault of the second horizontal coal seam in Chengjiao Coal Mine. Three holes are arranged in a typical roadway for water injection and water pressure monitoring respectively. The first water pressure test is a forward water pressure test, and the second water pressure test is a reverse water pressure test. The point where the water pressure and pressure permeability flow volume of the water pressure monitoring hole change synchronously with the water injection pressure is taken as the initial permeability characteristic point. And the corresponding water injection pressure is determined as the initial permeability pressure. If the water injection pressure continues to increase according to the design pressure, the permeability pressure is smaller than the water injection pressure and remains stable, and the water injection flow is relatively stable, it indicates that in the original state, the in-situ rock stratum has extremely strong permeability resistance and it is an aquifuge. On the contrary, it is a diversion fissure zone. The test results of the forward water pressure test shows that the water conductivity of the upper section of the FN-6 normal fault is extremely weak in the initial state. This section is an aquifuge. With the increase of water injection pressure, the rock mass between the water pressure hole and the water pressure monitoring hole is densely split, resulting in fissures. However, the scale and water conductivity are relatively small, and only seepage from micro fissures is dominant. During the reverse water pressure test, the number of water diversion channels is increased compared with that in the forward water pressure test. This leads to the decrease of the pressure difference between the water pressure hole and the water pressure monitoring hole. And the dominant water diversion channel is formed between the water pressure monitoring hole and the water pressure hole. The actual permeability state can be formed only when the critical permeability pressure (the critical permeability pressure of FN-6 normal fault is 11 MPa) is exceeded.http://www.gkzdh.cn/article/doi/10.13272/j.issn.1671-251x.2021110018water inrush from coal floorwater resisting capacity of surrounding rockin-situ testimpermeability performancetwo-way pressure permeability test'three-hole' method in-situ pressure permeability test technologyforward water pressurereverse water pressure
spellingShingle DAI Lei
DUAN Lihong
'Three hole' in-situ test and evaluation of fault impermeability of coal seam floor
Gong-kuang zidonghua
water inrush from coal floor
water resisting capacity of surrounding rock
in-situ test
impermeability performance
two-way pressure permeability test
'three-hole' method in-situ pressure permeability test technology
forward water pressure
reverse water pressure
title 'Three hole' in-situ test and evaluation of fault impermeability of coal seam floor
title_full 'Three hole' in-situ test and evaluation of fault impermeability of coal seam floor
title_fullStr 'Three hole' in-situ test and evaluation of fault impermeability of coal seam floor
title_full_unstemmed 'Three hole' in-situ test and evaluation of fault impermeability of coal seam floor
title_short 'Three hole' in-situ test and evaluation of fault impermeability of coal seam floor
title_sort three hole in situ test and evaluation of fault impermeability of coal seam floor
topic water inrush from coal floor
water resisting capacity of surrounding rock
in-situ test
impermeability performance
two-way pressure permeability test
'three-hole' method in-situ pressure permeability test technology
forward water pressure
reverse water pressure
url http://www.gkzdh.cn/article/doi/10.13272/j.issn.1671-251x.2021110018
work_keys_str_mv AT dailei threeholeinsitutestandevaluationoffaultimpermeabilityofcoalseamfloor
AT duanlihong threeholeinsitutestandevaluationoffaultimpermeabilityofcoalseamfloor