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Characteristics and Geological Impact Factors of Coalbed Methane Production in the Taiyuan Formation of the Gujiao Block
The coalbed methane resources of the Gujiao Block are abundant, and the exploration degree is high. The gas production and water production of different CBM (coalbed methane) wells vary greatly. The average gas production of CBM wells in the study area is mostly less than 1000 m3/d, while the averag...
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Published in: | Processes 2023-07, Vol.11 (7), p.2000 |
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description | The coalbed methane resources of the Gujiao Block are abundant, and the exploration degree is high. The gas production and water production of different CBM (coalbed methane) wells vary greatly. The average gas production of CBM wells in the study area is mostly less than 1000 m3/d, while the average water production is mostly less than 5 m3/d. The gas production of CBM wells near the core of the Malan syncline is relatively high. A series of large faults exist in the central and eastern parts of the study area, and CBM wells nearby produce more water but less gas. The salinity of water discharged from CBM wells ranges from 810.34 to 3115.48 mg/L, which is consistent with the trend of a gradual increase from north to south. The gas content distribution follows this same gradually increasing north to south trend. Coal thickness and buried depth have little effect on gas production, but have some effects on water production. The endogenous fracture system in the coal reservoir is extremely developed and the porosity and permeability of the reservoirs are low, which is not conducive to the migration and recovery of coalbed methane. The adsorption capacity of the coal sample is strong. However, the continuous uplift and denudation of the stratum from the middle Yanshanian to the Himalayan region are not conducive to the preservation and enrichment of coalbed methane. In addition, a series of large faults exist in this area, and the coal structures are broken. A large amount of coalbed methane is continually being released. Generally, structural and hydrological conditions affect the porosity, permeability, and gas content of coal reservoirs, thereby affecting the productivity of coalbed methane wells. The comprehensive analysis shows that the Xingjiashe well field in the southern part of the study area is a favorable area for CBM exploration and development. |
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The gas production and water production of different CBM (coalbed methane) wells vary greatly. The average gas production of CBM wells in the study area is mostly less than 1000 m3/d, while the average water production is mostly less than 5 m3/d. The gas production of CBM wells near the core of the Malan syncline is relatively high. A series of large faults exist in the central and eastern parts of the study area, and CBM wells nearby produce more water but less gas. The salinity of water discharged from CBM wells ranges from 810.34 to 3115.48 mg/L, which is consistent with the trend of a gradual increase from north to south. The gas content distribution follows this same gradually increasing north to south trend. Coal thickness and buried depth have little effect on gas production, but have some effects on water production. The endogenous fracture system in the coal reservoir is extremely developed and the porosity and permeability of the reservoirs are low, which is not conducive to the migration and recovery of coalbed methane. The adsorption capacity of the coal sample is strong. However, the continuous uplift and denudation of the stratum from the middle Yanshanian to the Himalayan region are not conducive to the preservation and enrichment of coalbed methane. In addition, a series of large faults exist in this area, and the coal structures are broken. A large amount of coalbed methane is continually being released. Generally, structural and hydrological conditions affect the porosity, permeability, and gas content of coal reservoirs, thereby affecting the productivity of coalbed methane wells. The comprehensive analysis shows that the Xingjiashe well field in the southern part of the study area is a favorable area for CBM exploration and development.</description><identifier>ISSN: 2227-9717</identifier><identifier>EISSN: 2227-9717</identifier><identifier>DOI: 10.3390/pr11072000</identifier><language>eng</language><publisher>Basel: MDPI AG</publisher><subject>Coal ; Coalbed methane ; Drainage ; Exploration ; Fault lines ; Gas production ; Geology ; Hydrology ; Impact factors ; Methane ; Natural gas ; Permeability ; Plate tectonics ; Porosity ; Reservoirs ; Stone ; Synclines ; Wells</subject><ispartof>Processes, 2023-07, Vol.11 (7), p.2000</ispartof><rights>COPYRIGHT 2023 MDPI AG</rights><rights>2023 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c334t-a455e7d79a21150929e3eef88dc57429d9ca110d06e868f4beed98daabfe4813</citedby><cites>FETCH-LOGICAL-c334t-a455e7d79a21150929e3eef88dc57429d9ca110d06e868f4beed98daabfe4813</cites><orcidid>0000-0002-1008-3781</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2843105754/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2843105754?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,25730,27900,27901,36988,44565,75095</link.rule.ids></links><search><creatorcontrib>Wang, Gang</creatorcontrib><creatorcontrib>Xie, Yiwei</creatorcontrib><creatorcontrib>Chang, Huizhen</creatorcontrib><creatorcontrib>Du, Liqiang</creatorcontrib><creatorcontrib>Wang, Qi</creatorcontrib><creatorcontrib>He, Tao</creatorcontrib><creatorcontrib>Zhang, Shuaiyi</creatorcontrib><title>Characteristics and Geological Impact Factors of Coalbed Methane Production in the Taiyuan Formation of the Gujiao Block</title><title>Processes</title><description>The coalbed methane resources of the Gujiao Block are abundant, and the exploration degree is high. The gas production and water production of different CBM (coalbed methane) wells vary greatly. The average gas production of CBM wells in the study area is mostly less than 1000 m3/d, while the average water production is mostly less than 5 m3/d. The gas production of CBM wells near the core of the Malan syncline is relatively high. A series of large faults exist in the central and eastern parts of the study area, and CBM wells nearby produce more water but less gas. The salinity of water discharged from CBM wells ranges from 810.34 to 3115.48 mg/L, which is consistent with the trend of a gradual increase from north to south. The gas content distribution follows this same gradually increasing north to south trend. Coal thickness and buried depth have little effect on gas production, but have some effects on water production. 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The comprehensive analysis shows that the Xingjiashe well field in the southern part of the study area is a favorable area for CBM exploration and development.</description><subject>Coal</subject><subject>Coalbed methane</subject><subject>Drainage</subject><subject>Exploration</subject><subject>Fault lines</subject><subject>Gas production</subject><subject>Geology</subject><subject>Hydrology</subject><subject>Impact factors</subject><subject>Methane</subject><subject>Natural gas</subject><subject>Permeability</subject><subject>Plate tectonics</subject><subject>Porosity</subject><subject>Reservoirs</subject><subject>Stone</subject><subject>Synclines</subject><subject>Wells</subject><issn>2227-9717</issn><issn>2227-9717</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><recordid>eNpNUd9LAzEMPkTBMffiX1DwTZj2x3W9Ps7h5mCiD3s_sja3dd6uZ3sH7r-3c4ISSEK-70tIkmW3jD4IoeljGxijilNKL7IB51yNtWLq8l9-nY1i3CcC1UwUcjLIvmY7CGA6DC52zkQCjSUL9LXfOgM1WR7ahJJ5cj5E4isy81Bv0JJX7HbQIHkP3vamc74hriHdDska3LGHhsx9OMAPkGQnYNHvHXjyVHvzcZNdVVBHHP3GYbaeP69nL-PV22I5m67GRoi8G0MuJSqrNHDGJNVco0CsisIaqXKurTaQtrZ0gsWkqPINotWFBdhUmBdMDLO7c9s2-M8eY1fufR-aNLHkRS4YlUrmifVwZm2hxtI1le_SUZJZPDjjG6xcqk-V1ExTqXkS3J8FJvgYA1ZlG9wBwrFktDw9o_x7hvgGBbd8ig</recordid><startdate>20230701</startdate><enddate>20230701</enddate><creator>Wang, Gang</creator><creator>Xie, Yiwei</creator><creator>Chang, Huizhen</creator><creator>Du, Liqiang</creator><creator>Wang, Qi</creator><creator>He, Tao</creator><creator>Zhang, Shuaiyi</creator><general>MDPI AG</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7SR</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FH</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>D1I</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>JG9</scope><scope>KB.</scope><scope>LK8</scope><scope>M7P</scope><scope>PDBOC</scope><scope>PHGZM</scope><scope>PHGZT</scope><scope>PIMPY</scope><scope>PKEHL</scope><scope>PQEST</scope><scope>PQGLB</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><orcidid>https://orcid.org/0000-0002-1008-3781</orcidid></search><sort><creationdate>20230701</creationdate><title>Characteristics and Geological Impact Factors of Coalbed Methane Production in the Taiyuan Formation of the Gujiao Block</title><author>Wang, Gang ; 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The gas production and water production of different CBM (coalbed methane) wells vary greatly. The average gas production of CBM wells in the study area is mostly less than 1000 m3/d, while the average water production is mostly less than 5 m3/d. The gas production of CBM wells near the core of the Malan syncline is relatively high. A series of large faults exist in the central and eastern parts of the study area, and CBM wells nearby produce more water but less gas. The salinity of water discharged from CBM wells ranges from 810.34 to 3115.48 mg/L, which is consistent with the trend of a gradual increase from north to south. The gas content distribution follows this same gradually increasing north to south trend. Coal thickness and buried depth have little effect on gas production, but have some effects on water production. The endogenous fracture system in the coal reservoir is extremely developed and the porosity and permeability of the reservoirs are low, which is not conducive to the migration and recovery of coalbed methane. The adsorption capacity of the coal sample is strong. However, the continuous uplift and denudation of the stratum from the middle Yanshanian to the Himalayan region are not conducive to the preservation and enrichment of coalbed methane. In addition, a series of large faults exist in this area, and the coal structures are broken. A large amount of coalbed methane is continually being released. Generally, structural and hydrological conditions affect the porosity, permeability, and gas content of coal reservoirs, thereby affecting the productivity of coalbed methane wells. The comprehensive analysis shows that the Xingjiashe well field in the southern part of the study area is a favorable area for CBM exploration and development.</abstract><cop>Basel</cop><pub>MDPI AG</pub><doi>10.3390/pr11072000</doi><orcidid>https://orcid.org/0000-0002-1008-3781</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Coal Coalbed methane Drainage Exploration Fault lines Gas production Geology Hydrology Impact factors Methane Natural gas Permeability Plate tectonics Porosity Reservoirs Stone Synclines Wells |
title | Characteristics and Geological Impact Factors of Coalbed Methane Production in the Taiyuan Formation of the Gujiao Block |
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