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Experimental Studies on the Enhancement of Permeability of Anthracite by Acidizing: A Case Study in the Daning Block, Southern Qinshui Basin
[Image: see text] As the most active and top producing area of coalbed methane (CBM) in China, the southern Qinshui Basin (SQB) is dominated by anthracite. Due to the low permeability of coals, plenty of non-gas-producing and low production CBM wells exist in the SQB. The permeability enhancement th...
Autores principales: | , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
American Chemical Society
2021
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Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8613850/ https://www.ncbi.nlm.nih.gov/pubmed/34841153 http://dx.doi.org/10.1021/acsomega.1c04539 |
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author | Guo, Zhiqi Cao, Yunxing Dong, Shi Zhang, Zheng |
author_facet | Guo, Zhiqi Cao, Yunxing Dong, Shi Zhang, Zheng |
author_sort | Guo, Zhiqi |
collection | PubMed |
description | [Image: see text] As the most active and top producing area of coalbed methane (CBM) in China, the southern Qinshui Basin (SQB) is dominated by anthracite. Due to the low permeability of coals, plenty of non-gas-producing and low production CBM wells exist in the SQB. The permeability enhancement through some technological means is the key to increasing the CBM production of this area. In this paper, some typical anthracites were selected from the Daning block of the SQB to assess the effect of acidification treatments on permeability enhancement. The maceral composition determination shows that approximately 15% of minerals exist in the collected coal samples, and the X-ray diffractometer (XRD) results reveal that the minerals consist primarily of clay minerals, along with a little amount of quartz, calcite, and dolomite. Two types of acidizing fluids were used to conduct acidification treatments on the anthracites for different lengths of time. The N(2) permeability of the anthracites before and after acidification was measured and compared. The results show that the original samples exhibit low permeability. As the acidification time increases, the permeability of all of the samples shows an increasing trend, and the acid sensitivity index I(a) increases rapidly first and then levels off, and finally approaches 1. After 48 h of acidification, the samples show an increase ranging from 8.75 to 22.67 times (avg. 14.3 times) the original permeability. The permeability enhancement of the SQB anthracites is mainly attributed to the dissolution of acid-soluble minerals in the cleat system of coal. The minerals in the cleats are completely or partially dissolved by the acids, generating some soluble and insoluble substances; when the fluid flows through, the cleat space is reallocated. Overall, the cleat demineralization by acids frees up a lot of cleat spaces, leading to an increase in cleat connectivity. As a result, the fluid movement becomes smooth and the permeability of coal improves. |
format | Online Article Text |
id | pubmed-8613850 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2021 |
publisher | American Chemical Society |
record_format | MEDLINE/PubMed |
spelling | pubmed-86138502021-11-26 Experimental Studies on the Enhancement of Permeability of Anthracite by Acidizing: A Case Study in the Daning Block, Southern Qinshui Basin Guo, Zhiqi Cao, Yunxing Dong, Shi Zhang, Zheng ACS Omega [Image: see text] As the most active and top producing area of coalbed methane (CBM) in China, the southern Qinshui Basin (SQB) is dominated by anthracite. Due to the low permeability of coals, plenty of non-gas-producing and low production CBM wells exist in the SQB. The permeability enhancement through some technological means is the key to increasing the CBM production of this area. In this paper, some typical anthracites were selected from the Daning block of the SQB to assess the effect of acidification treatments on permeability enhancement. The maceral composition determination shows that approximately 15% of minerals exist in the collected coal samples, and the X-ray diffractometer (XRD) results reveal that the minerals consist primarily of clay minerals, along with a little amount of quartz, calcite, and dolomite. Two types of acidizing fluids were used to conduct acidification treatments on the anthracites for different lengths of time. The N(2) permeability of the anthracites before and after acidification was measured and compared. The results show that the original samples exhibit low permeability. As the acidification time increases, the permeability of all of the samples shows an increasing trend, and the acid sensitivity index I(a) increases rapidly first and then levels off, and finally approaches 1. After 48 h of acidification, the samples show an increase ranging from 8.75 to 22.67 times (avg. 14.3 times) the original permeability. The permeability enhancement of the SQB anthracites is mainly attributed to the dissolution of acid-soluble minerals in the cleat system of coal. The minerals in the cleats are completely or partially dissolved by the acids, generating some soluble and insoluble substances; when the fluid flows through, the cleat space is reallocated. Overall, the cleat demineralization by acids frees up a lot of cleat spaces, leading to an increase in cleat connectivity. As a result, the fluid movement becomes smooth and the permeability of coal improves. American Chemical Society 2021-11-11 /pmc/articles/PMC8613850/ /pubmed/34841153 http://dx.doi.org/10.1021/acsomega.1c04539 Text en © 2021 The Authors. Published by American Chemical Society https://creativecommons.org/licenses/by-nc-nd/4.0/Permits non-commercial access and re-use, provided that author attribution and integrity are maintained; but does not permit creation of adaptations or other derivative works (https://creativecommons.org/licenses/by-nc-nd/4.0/). |
spellingShingle | Guo, Zhiqi Cao, Yunxing Dong, Shi Zhang, Zheng Experimental Studies on the Enhancement of Permeability of Anthracite by Acidizing: A Case Study in the Daning Block, Southern Qinshui Basin |
title | Experimental Studies on the Enhancement of Permeability
of Anthracite by Acidizing: A Case Study in the Daning Block, Southern
Qinshui Basin |
title_full | Experimental Studies on the Enhancement of Permeability
of Anthracite by Acidizing: A Case Study in the Daning Block, Southern
Qinshui Basin |
title_fullStr | Experimental Studies on the Enhancement of Permeability
of Anthracite by Acidizing: A Case Study in the Daning Block, Southern
Qinshui Basin |
title_full_unstemmed | Experimental Studies on the Enhancement of Permeability
of Anthracite by Acidizing: A Case Study in the Daning Block, Southern
Qinshui Basin |
title_short | Experimental Studies on the Enhancement of Permeability
of Anthracite by Acidizing: A Case Study in the Daning Block, Southern
Qinshui Basin |
title_sort | experimental studies on the enhancement of permeability
of anthracite by acidizing: a case study in the daning block, southern
qinshui basin |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8613850/ https://www.ncbi.nlm.nih.gov/pubmed/34841153 http://dx.doi.org/10.1021/acsomega.1c04539 |
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