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A Modified Pressure Pulse Decay Experimental Apparatus and Its Application in Permeability Measurements
Permeability is an essential factor used for evaluating the commercial exploitation of unconventional energy. The pressure pulse decay method is one of the most effective methods to measure permeability and has been improved by adding a pressure transducer upstream and a chamber upstream and downstr...
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Published in: | Applied geophysics 2023-12, Vol.20 (4), p.534-546 |
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creator | Wang, Gang Sun, Xiao-xiang Xiao, Zhi-yong Wang, Chang-Sheng Yu, Jun-hong Jiang, Feng Zheng, Cheng-cheng |
description | Permeability is an essential factor used for evaluating the commercial exploitation of unconventional energy. The pressure pulse decay method is one of the most effective methods to measure permeability and has been improved by adding a pressure transducer upstream and a chamber upstream and downstream. The relationship between the pulse pressure and equilibrium time under different storage volumes is investigated based on a developed apparatus. Moreover, the effect of compressive storage on permeability measurements has been examined by comparing the Brace’s et al.’s solution and Jones’ solution. The following results were obtained for the constant injection pressure. 1) The equilibrium pressure increases with a decrease in the upstream storage volume and decreases with an increase in the downstream storage volume. 2) The equilibrium time increases with an increase in the storage volume, and the similar volume of the upstream and downstream can accelerate the test procedure. 3) A linear relationship between the storage volume and equilibrium time is not apparent when the volume of the upstream and downstream are asymmetric. However, this linear relationship is evident when the volume of the upstream and downstream are symmetrical. 4) The influence of the downstream storage volume is more significant than the upstream volume on the measurement of permeability. The results are of guiding significance for selecting the proper storage volume to measure permeability. |
doi_str_mv | 10.1007/s11770-022-0999-2 |
format | article |
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The pressure pulse decay method is one of the most effective methods to measure permeability and has been improved by adding a pressure transducer upstream and a chamber upstream and downstream. The relationship between the pulse pressure and equilibrium time under different storage volumes is investigated based on a developed apparatus. Moreover, the effect of compressive storage on permeability measurements has been examined by comparing the Brace’s et al.’s solution and Jones’ solution. The following results were obtained for the constant injection pressure. 1) The equilibrium pressure increases with a decrease in the upstream storage volume and decreases with an increase in the downstream storage volume. 2) The equilibrium time increases with an increase in the storage volume, and the similar volume of the upstream and downstream can accelerate the test procedure. 3) A linear relationship between the storage volume and equilibrium time is not apparent when the volume of the upstream and downstream are asymmetric. However, this linear relationship is evident when the volume of the upstream and downstream are symmetrical. 4) The influence of the downstream storage volume is more significant than the upstream volume on the measurement of permeability. The results are of guiding significance for selecting the proper storage volume to measure permeability.</description><identifier>ISSN: 1672-7975</identifier><identifier>EISSN: 1993-0658</identifier><identifier>DOI: 10.1007/s11770-022-0999-2</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Decay ; Earth and Environmental Science ; Earth Sciences ; Equilibrium ; Exploitation ; Geophysics/Geodesy ; Geotechnical Engineering & Applied Earth Sciences ; Permeability ; Pressure ; Transducers ; Upstream</subject><ispartof>Applied geophysics, 2023-12, Vol.20 (4), p.534-546</ispartof><rights>The Editorial Department of APPLIED GEOPHYSICS 2022</rights><rights>The Editorial Department of APPLIED GEOPHYSICS 2022.</rights><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c268t-8a75edd7d733c66450fd65e96f436afcd00b8dfffff0ea6936f4d2c34bc36a653</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Wang, Gang</creatorcontrib><creatorcontrib>Sun, Xiao-xiang</creatorcontrib><creatorcontrib>Xiao, Zhi-yong</creatorcontrib><creatorcontrib>Wang, Chang-Sheng</creatorcontrib><creatorcontrib>Yu, Jun-hong</creatorcontrib><creatorcontrib>Jiang, Feng</creatorcontrib><creatorcontrib>Zheng, Cheng-cheng</creatorcontrib><title>A Modified Pressure Pulse Decay Experimental Apparatus and Its Application in Permeability Measurements</title><title>Applied geophysics</title><addtitle>Appl. Geophys</addtitle><description>Permeability is an essential factor used for evaluating the commercial exploitation of unconventional energy. The pressure pulse decay method is one of the most effective methods to measure permeability and has been improved by adding a pressure transducer upstream and a chamber upstream and downstream. The relationship between the pulse pressure and equilibrium time under different storage volumes is investigated based on a developed apparatus. Moreover, the effect of compressive storage on permeability measurements has been examined by comparing the Brace’s et al.’s solution and Jones’ solution. The following results were obtained for the constant injection pressure. 1) The equilibrium pressure increases with a decrease in the upstream storage volume and decreases with an increase in the downstream storage volume. 2) The equilibrium time increases with an increase in the storage volume, and the similar volume of the upstream and downstream can accelerate the test procedure. 3) A linear relationship between the storage volume and equilibrium time is not apparent when the volume of the upstream and downstream are asymmetric. However, this linear relationship is evident when the volume of the upstream and downstream are symmetrical. 4) The influence of the downstream storage volume is more significant than the upstream volume on the measurement of permeability. The results are of guiding significance for selecting the proper storage volume to measure permeability.</description><subject>Decay</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Equilibrium</subject><subject>Exploitation</subject><subject>Geophysics/Geodesy</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Permeability</subject><subject>Pressure</subject><subject>Transducers</subject><subject>Upstream</subject><issn>1672-7975</issn><issn>1993-0658</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNp1UMtOwzAQtBBIlMIHcLPE2eBHYsfHqhSo1Ioe4Gy58aZylSbBTiT69zgKEif2squdnVnNIHTP6COjVD1FxpSihHJOqNaa8As0Y1oLQmVeXKZZKk6UVvk1uonxSKkUXGYzdFjgbet85cHhXYAYhwB4N9QR8DOU9oxX3x0Ef4KmtzVedJ0Nth8ito3D6z6Om9qXtvdtg32DdxBOYPe-9v0Zb8GOciM33qKryibVu98-R58vq4_lG9m8v66Xiw0puSx6UliVg3PKKSFKKbOcVk7moGWVCWmr0lG6L1w1FgUrtUiA46XI9mXCZS7m6GHS7UL7NUDszbEdQpNeGq6LXGeMJ-tzxKarMrQxBqhMlzzacDaMmjFPM-VpUp5mzNPwxOETJ6bb5gDhT_l_0g_vPnn6</recordid><startdate>20231201</startdate><enddate>20231201</enddate><creator>Wang, Gang</creator><creator>Sun, Xiao-xiang</creator><creator>Xiao, Zhi-yong</creator><creator>Wang, Chang-Sheng</creator><creator>Yu, Jun-hong</creator><creator>Jiang, Feng</creator><creator>Zheng, Cheng-cheng</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>H8D</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>L7M</scope></search><sort><creationdate>20231201</creationdate><title>A Modified Pressure Pulse Decay Experimental Apparatus and Its Application in Permeability Measurements</title><author>Wang, Gang ; Sun, Xiao-xiang ; Xiao, Zhi-yong ; Wang, Chang-Sheng ; Yu, Jun-hong ; Jiang, Feng ; Zheng, Cheng-cheng</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c268t-8a75edd7d733c66450fd65e96f436afcd00b8dfffff0ea6936f4d2c34bc36a653</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Decay</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Equilibrium</topic><topic>Exploitation</topic><topic>Geophysics/Geodesy</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Permeability</topic><topic>Pressure</topic><topic>Transducers</topic><topic>Upstream</topic><toplevel>online_resources</toplevel><creatorcontrib>Wang, Gang</creatorcontrib><creatorcontrib>Sun, Xiao-xiang</creatorcontrib><creatorcontrib>Xiao, Zhi-yong</creatorcontrib><creatorcontrib>Wang, Chang-Sheng</creatorcontrib><creatorcontrib>Yu, Jun-hong</creatorcontrib><creatorcontrib>Jiang, Feng</creatorcontrib><creatorcontrib>Zheng, Cheng-cheng</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Applied geophysics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wang, Gang</au><au>Sun, Xiao-xiang</au><au>Xiao, Zhi-yong</au><au>Wang, Chang-Sheng</au><au>Yu, Jun-hong</au><au>Jiang, Feng</au><au>Zheng, Cheng-cheng</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A Modified Pressure Pulse Decay Experimental Apparatus and Its Application in Permeability Measurements</atitle><jtitle>Applied geophysics</jtitle><stitle>Appl. Geophys</stitle><date>2023-12-01</date><risdate>2023</risdate><volume>20</volume><issue>4</issue><spage>534</spage><epage>546</epage><pages>534-546</pages><issn>1672-7975</issn><eissn>1993-0658</eissn><abstract>Permeability is an essential factor used for evaluating the commercial exploitation of unconventional energy. The pressure pulse decay method is one of the most effective methods to measure permeability and has been improved by adding a pressure transducer upstream and a chamber upstream and downstream. The relationship between the pulse pressure and equilibrium time under different storage volumes is investigated based on a developed apparatus. Moreover, the effect of compressive storage on permeability measurements has been examined by comparing the Brace’s et al.’s solution and Jones’ solution. The following results were obtained for the constant injection pressure. 1) The equilibrium pressure increases with a decrease in the upstream storage volume and decreases with an increase in the downstream storage volume. 2) The equilibrium time increases with an increase in the storage volume, and the similar volume of the upstream and downstream can accelerate the test procedure. 3) A linear relationship between the storage volume and equilibrium time is not apparent when the volume of the upstream and downstream are asymmetric. However, this linear relationship is evident when the volume of the upstream and downstream are symmetrical. 4) The influence of the downstream storage volume is more significant than the upstream volume on the measurement of permeability. The results are of guiding significance for selecting the proper storage volume to measure permeability.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s11770-022-0999-2</doi><tpages>13</tpages></addata></record> |
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subjects | Decay Earth and Environmental Science Earth Sciences Equilibrium Exploitation Geophysics/Geodesy Geotechnical Engineering & Applied Earth Sciences Permeability Pressure Transducers Upstream |
title | A Modified Pressure Pulse Decay Experimental Apparatus and Its Application in Permeability Measurements |
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