P-wave velocity anisotropy in Hamra Quartzites reservoir, Hassi Messaoud oil field in Algeria
The P-wave velocity and physical parameters were measured for core samples taken from Hamra Quartzites reservoir in Hassi Messaoud oil field (Algeria). The Pundit Lab tool was used to measure the P-wave velocity and the optical scanning technology was utilized for thermal conductivity. The permeabil...
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| Veröffentlicht in: | Arabian journal of geosciences 2022-05, Vol.15 (9), Article 800 |
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| creator | Zerrouki, Ahmed Ali Geraud, Yves Dobbi, Abdelmadjid Diraisson, Marc Baddari, Kamel Lebtahi, Hamid |
| description | The P-wave velocity and physical parameters were measured for core samples taken from Hamra Quartzites reservoir in Hassi Messaoud oil field (Algeria). The Pundit Lab tool was used to measure the P-wave velocity and the optical scanning technology was utilized for thermal conductivity. The permeability and porosity are also executed for cylindrical samples; these measures are taken under room temperature and ambient pressure. The physical and petrophysical measurements were carried out in order to search relationships between P-wave velocity anisotropy, thermal conductivity, grain size, density, P-wave velocity, thermal conductivity anisotropy, and porosity for all samples after their classification in uncemented and cemented sets. The origin of P-wave velocity anisotropy basing on thin section of samples and using microscopy analysis is also investigated. The obtained results show good correlation coefficients (R) between P-wave velocity anisotropy, grain size, P-wave velocity, and thermal conductivity in cemented set. The highest correlation coefficient is found between P-wave velocity anisotropy and thermal conductivity in cemented set (
R
=0.92). The P-wave velocity anisotropy ranges between 9.93 and 11.14% for anisotropic samples. The microscopy analysis of thin sections for studied samples shows that open and closed microcracks are the origin of P-wave velocity anisotropy in Hamra Quartzites reservoir. The P-wave velocity anisotropy of samples is proportional to the width of parallel microcracks. |
| doi_str_mv | 10.1007/s12517-022-10022-8 |
| format | Article |
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R
=0.92). The P-wave velocity anisotropy ranges between 9.93 and 11.14% for anisotropic samples. The microscopy analysis of thin sections for studied samples shows that open and closed microcracks are the origin of P-wave velocity anisotropy in Hamra Quartzites reservoir. The P-wave velocity anisotropy of samples is proportional to the width of parallel microcracks.</description><identifier>ISSN: 1866-7511</identifier><identifier>EISSN: 1866-7538</identifier><identifier>DOI: 10.1007/s12517-022-10022-8</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Anisotropy ; Coefficients ; Cores ; Correlation coefficient ; Correlation coefficients ; Earth and Environmental Science ; Earth science ; Earth Sciences ; Grain size ; Heat conductivity ; Heat transfer ; Microcracks ; Microscopy ; Oil and gas fields ; Oil fields ; Original Paper ; P waves ; Particle size ; Permeability ; Physical properties ; Porosity ; Pressure ; Quartzite ; Reservoirs ; Room temperature ; Sciences of the Universe ; Thermal conductivity ; Velocity ; Wave velocity</subject><ispartof>Arabian journal of geosciences, 2022-05, Vol.15 (9), Article 800</ispartof><rights>Saudi Society for Geosciences 2022</rights><rights>Saudi Society for Geosciences 2022.</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c1988-bfb68f3f4ef6caf1b4b40ff8631fb59342fec1038dd2f9971c78de5420fcd5903</citedby><cites>FETCH-LOGICAL-c1988-bfb68f3f4ef6caf1b4b40ff8631fb59342fec1038dd2f9971c78de5420fcd5903</cites><orcidid>0000-0002-2352-3045</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12517-022-10022-8$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12517-022-10022-8$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>230,314,780,784,885,27924,27925,41488,42557,51319</link.rule.ids><backlink>$$Uhttps://hal.univ-lorraine.fr/hal-04194102$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Zerrouki, Ahmed Ali</creatorcontrib><creatorcontrib>Geraud, Yves</creatorcontrib><creatorcontrib>Dobbi, Abdelmadjid</creatorcontrib><creatorcontrib>Diraisson, Marc</creatorcontrib><creatorcontrib>Baddari, Kamel</creatorcontrib><creatorcontrib>Lebtahi, Hamid</creatorcontrib><title>P-wave velocity anisotropy in Hamra Quartzites reservoir, Hassi Messaoud oil field in Algeria</title><title>Arabian journal of geosciences</title><addtitle>Arab J Geosci</addtitle><description>The P-wave velocity and physical parameters were measured for core samples taken from Hamra Quartzites reservoir in Hassi Messaoud oil field (Algeria). The Pundit Lab tool was used to measure the P-wave velocity and the optical scanning technology was utilized for thermal conductivity. The permeability and porosity are also executed for cylindrical samples; these measures are taken under room temperature and ambient pressure. The physical and petrophysical measurements were carried out in order to search relationships between P-wave velocity anisotropy, thermal conductivity, grain size, density, P-wave velocity, thermal conductivity anisotropy, and porosity for all samples after their classification in uncemented and cemented sets. The origin of P-wave velocity anisotropy basing on thin section of samples and using microscopy analysis is also investigated. The obtained results show good correlation coefficients (R) between P-wave velocity anisotropy, grain size, P-wave velocity, and thermal conductivity in cemented set. The highest correlation coefficient is found between P-wave velocity anisotropy and thermal conductivity in cemented set (
R
=0.92). The P-wave velocity anisotropy ranges between 9.93 and 11.14% for anisotropic samples. The microscopy analysis of thin sections for studied samples shows that open and closed microcracks are the origin of P-wave velocity anisotropy in Hamra Quartzites reservoir. The P-wave velocity anisotropy of samples is proportional to the width of parallel microcracks.</description><subject>Anisotropy</subject><subject>Coefficients</subject><subject>Cores</subject><subject>Correlation coefficient</subject><subject>Correlation coefficients</subject><subject>Earth and Environmental Science</subject><subject>Earth science</subject><subject>Earth Sciences</subject><subject>Grain size</subject><subject>Heat conductivity</subject><subject>Heat transfer</subject><subject>Microcracks</subject><subject>Microscopy</subject><subject>Oil and gas fields</subject><subject>Oil fields</subject><subject>Original Paper</subject><subject>P waves</subject><subject>Particle size</subject><subject>Permeability</subject><subject>Physical properties</subject><subject>Porosity</subject><subject>Pressure</subject><subject>Quartzite</subject><subject>Reservoirs</subject><subject>Room temperature</subject><subject>Sciences of the Universe</subject><subject>Thermal conductivity</subject><subject>Velocity</subject><subject>Wave velocity</subject><issn>1866-7511</issn><issn>1866-7538</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><recordid>eNp9kEFLwzAYhoMoOKd_wFPAk2A1X5q26XEMdcJEBT1KSNtEM7pmJm1l_npTK_PmJcmXPO9LeBA6BXIJhGRXHmgCWUQojcIcVr6HJsDTNMqSmO_vzgCH6Mj7FSEpJxmfoNfH6FP2CveqtqVpt1g2xtvW2c0WmwYv5NpJ_NRJ136ZVnnslFeut8ZdhDfvDb5X3kvbVdiaGmuj6mrIzeo35Yw8Rgda1l6d_O5T9HJz_TxfRMuH27v5bBmVkHMeFbpIuY41UzotpYaCFYxozdMYdJHkMaNalUBiXlVU53kGZcYrlTBKdFklOYmn6HzsfZe12Dizlm4rrDRiMVuK4Y4wyBkQ2kNgz0Z24-xHp3wrVrZzTfieoGlCSU4YGyg6UqWz3juld7VAxKBcjMpFkC1-lAseQvEY8gFugoG_6n9S3y8Hg6A</recordid><startdate>202205</startdate><enddate>202205</enddate><creator>Zerrouki, Ahmed Ali</creator><creator>Geraud, Yves</creator><creator>Dobbi, Abdelmadjid</creator><creator>Diraisson, Marc</creator><creator>Baddari, Kamel</creator><creator>Lebtahi, Hamid</creator><general>Springer International Publishing</general><general>Springer Nature B.V</general><general>Springer</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0002-2352-3045</orcidid></search><sort><creationdate>202205</creationdate><title>P-wave velocity anisotropy in Hamra Quartzites reservoir, Hassi Messaoud oil field in Algeria</title><author>Zerrouki, Ahmed Ali ; Geraud, Yves ; Dobbi, Abdelmadjid ; Diraisson, Marc ; Baddari, Kamel ; Lebtahi, Hamid</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c1988-bfb68f3f4ef6caf1b4b40ff8631fb59342fec1038dd2f9971c78de5420fcd5903</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Anisotropy</topic><topic>Coefficients</topic><topic>Cores</topic><topic>Correlation coefficient</topic><topic>Correlation coefficients</topic><topic>Earth and Environmental Science</topic><topic>Earth science</topic><topic>Earth Sciences</topic><topic>Grain size</topic><topic>Heat conductivity</topic><topic>Heat transfer</topic><topic>Microcracks</topic><topic>Microscopy</topic><topic>Oil and gas fields</topic><topic>Oil fields</topic><topic>Original Paper</topic><topic>P waves</topic><topic>Particle size</topic><topic>Permeability</topic><topic>Physical properties</topic><topic>Porosity</topic><topic>Pressure</topic><topic>Quartzite</topic><topic>Reservoirs</topic><topic>Room temperature</topic><topic>Sciences of the Universe</topic><topic>Thermal conductivity</topic><topic>Velocity</topic><topic>Wave velocity</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zerrouki, Ahmed Ali</creatorcontrib><creatorcontrib>Geraud, Yves</creatorcontrib><creatorcontrib>Dobbi, Abdelmadjid</creatorcontrib><creatorcontrib>Diraisson, Marc</creatorcontrib><creatorcontrib>Baddari, Kamel</creatorcontrib><creatorcontrib>Lebtahi, Hamid</creatorcontrib><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Arabian journal of geosciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zerrouki, Ahmed Ali</au><au>Geraud, Yves</au><au>Dobbi, Abdelmadjid</au><au>Diraisson, Marc</au><au>Baddari, Kamel</au><au>Lebtahi, Hamid</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>P-wave velocity anisotropy in Hamra Quartzites reservoir, Hassi Messaoud oil field in Algeria</atitle><jtitle>Arabian journal of geosciences</jtitle><stitle>Arab J Geosci</stitle><date>2022-05</date><risdate>2022</risdate><volume>15</volume><issue>9</issue><artnum>800</artnum><issn>1866-7511</issn><eissn>1866-7538</eissn><abstract>The P-wave velocity and physical parameters were measured for core samples taken from Hamra Quartzites reservoir in Hassi Messaoud oil field (Algeria). The Pundit Lab tool was used to measure the P-wave velocity and the optical scanning technology was utilized for thermal conductivity. The permeability and porosity are also executed for cylindrical samples; these measures are taken under room temperature and ambient pressure. The physical and petrophysical measurements were carried out in order to search relationships between P-wave velocity anisotropy, thermal conductivity, grain size, density, P-wave velocity, thermal conductivity anisotropy, and porosity for all samples after their classification in uncemented and cemented sets. The origin of P-wave velocity anisotropy basing on thin section of samples and using microscopy analysis is also investigated. The obtained results show good correlation coefficients (R) between P-wave velocity anisotropy, grain size, P-wave velocity, and thermal conductivity in cemented set. The highest correlation coefficient is found between P-wave velocity anisotropy and thermal conductivity in cemented set (
R
=0.92). The P-wave velocity anisotropy ranges between 9.93 and 11.14% for anisotropic samples. The microscopy analysis of thin sections for studied samples shows that open and closed microcracks are the origin of P-wave velocity anisotropy in Hamra Quartzites reservoir. The P-wave velocity anisotropy of samples is proportional to the width of parallel microcracks.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><doi>10.1007/s12517-022-10022-8</doi><orcidid>https://orcid.org/0000-0002-2352-3045</orcidid></addata></record> |
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| subjects | Anisotropy Coefficients Cores Correlation coefficient Correlation coefficients Earth and Environmental Science Earth science Earth Sciences Grain size Heat conductivity Heat transfer Microcracks Microscopy Oil and gas fields Oil fields Original Paper P waves Particle size Permeability Physical properties Porosity Pressure Quartzite Reservoirs Room temperature Sciences of the Universe Thermal conductivity Velocity Wave velocity |
| title | P-wave velocity anisotropy in Hamra Quartzites reservoir, Hassi Messaoud oil field in Algeria |
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