Resolution effect in X-ray microcomputed tomography imaging and small pore’s contribution to permeability for a Berea sandstone
•A Berea sandstone sample was scanned twice under two different resolutions.•Higher resolution affect pore characteristic parameters by including small pores.•But small pores do not influence permeability (K) significantly.•Using diffusional tortuosity can estimate K better than geometric tortuosity...
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Veröffentlicht in: | Journal of hydrology (Amsterdam) 2014-03, Vol.510, p.403-411 |
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creator | Peng, Sheng Marone, Federica Dultz, Stefan |
description | •A Berea sandstone sample was scanned twice under two different resolutions.•Higher resolution affect pore characteristic parameters by including small pores.•But small pores do not influence permeability (K) significantly.•Using diffusional tortuosity can estimate K better than geometric tortuosity.
Resolution selection when using X-ray microcomputed tomography should be made based on the compromise between accuracy and representativeness. The question is then how accurate is accurate enough, that is, how small a pore is small enough to be ignored without generating misleading results on pore representation and subsequent flow properties such as permeability. In this study, synchrotron X-ray microcomputed tomographic scans of a Berea sandstone sample were acquired for two resolutions (with 1.85 and 5.92μm pixel width). Higher resolution images resolve more small pores, and have similar large pores as the lower resolution images. Pore characterization and permeability estimation were conducted based on these two sets of images. The pore parameters and permeability were also measured for another larger sample from the same rock fragment through laboratory experiments. The comparison between the different resolution image analyses and the laboratory measurement indicates that small pores contribute to larger porosity, smaller tortuosity, and larger surface area, but do not influence permeability significantly. Therefore, relatively low resolution (pixel width up to 5.92μm) can be used for Berea sandstone when permeability is the focus. However, use of even lower resolution needs to be careful since lower resolution not only excludes more small pores, but also has the potential to overestimate the pore size and thereby the permeability. Kozeny–Carman equation was used to estimate the permeability with geometric and diffusional tortuosity. The results indicate that the latter tortuosity can serve better for the permeability estimation than the former. |
doi_str_mv | 10.1016/j.jhydrol.2013.12.028 |
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Resolution selection when using X-ray microcomputed tomography should be made based on the compromise between accuracy and representativeness. The question is then how accurate is accurate enough, that is, how small a pore is small enough to be ignored without generating misleading results on pore representation and subsequent flow properties such as permeability. In this study, synchrotron X-ray microcomputed tomographic scans of a Berea sandstone sample were acquired for two resolutions (with 1.85 and 5.92μm pixel width). Higher resolution images resolve more small pores, and have similar large pores as the lower resolution images. Pore characterization and permeability estimation were conducted based on these two sets of images. The pore parameters and permeability were also measured for another larger sample from the same rock fragment through laboratory experiments. The comparison between the different resolution image analyses and the laboratory measurement indicates that small pores contribute to larger porosity, smaller tortuosity, and larger surface area, but do not influence permeability significantly. Therefore, relatively low resolution (pixel width up to 5.92μm) can be used for Berea sandstone when permeability is the focus. However, use of even lower resolution needs to be careful since lower resolution not only excludes more small pores, but also has the potential to overestimate the pore size and thereby the permeability. Kozeny–Carman equation was used to estimate the permeability with geometric and diffusional tortuosity. The results indicate that the latter tortuosity can serve better for the permeability estimation than the former.</description><identifier>ISSN: 0022-1694</identifier><identifier>EISSN: 1879-2707</identifier><identifier>DOI: 10.1016/j.jhydrol.2013.12.028</identifier><identifier>CODEN: JHYDA7</identifier><language>eng</language><publisher>Kidlington: Elsevier B.V</publisher><subject>Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Hydrogeology ; Hydrology ; Hydrology. Hydrogeology ; Mathematical analysis ; Permeability ; Permeability estimation ; Pixels ; Pore-grain segmentation ; Porosity ; Resolution effect ; Sandstone ; Small pore effect ; Tomography ; Tortuosity ; X-rays</subject><ispartof>Journal of hydrology (Amsterdam), 2014-03, Vol.510, p.403-411</ispartof><rights>2014 Elsevier B.V.</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a428t-d5b63b51a998b67489521351ca482c07e25018ceb9f897977faa84e53811d6283</citedby><cites>FETCH-LOGICAL-a428t-d5b63b51a998b67489521351ca482c07e25018ceb9f897977faa84e53811d6283</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0022169413009256$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,27901,27902,65306</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=28331136$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Peng, Sheng</creatorcontrib><creatorcontrib>Marone, Federica</creatorcontrib><creatorcontrib>Dultz, Stefan</creatorcontrib><title>Resolution effect in X-ray microcomputed tomography imaging and small pore’s contribution to permeability for a Berea sandstone</title><title>Journal of hydrology (Amsterdam)</title><description>•A Berea sandstone sample was scanned twice under two different resolutions.•Higher resolution affect pore characteristic parameters by including small pores.•But small pores do not influence permeability (K) significantly.•Using diffusional tortuosity can estimate K better than geometric tortuosity.
Resolution selection when using X-ray microcomputed tomography should be made based on the compromise between accuracy and representativeness. The question is then how accurate is accurate enough, that is, how small a pore is small enough to be ignored without generating misleading results on pore representation and subsequent flow properties such as permeability. In this study, synchrotron X-ray microcomputed tomographic scans of a Berea sandstone sample were acquired for two resolutions (with 1.85 and 5.92μm pixel width). Higher resolution images resolve more small pores, and have similar large pores as the lower resolution images. Pore characterization and permeability estimation were conducted based on these two sets of images. The pore parameters and permeability were also measured for another larger sample from the same rock fragment through laboratory experiments. The comparison between the different resolution image analyses and the laboratory measurement indicates that small pores contribute to larger porosity, smaller tortuosity, and larger surface area, but do not influence permeability significantly. Therefore, relatively low resolution (pixel width up to 5.92μm) can be used for Berea sandstone when permeability is the focus. However, use of even lower resolution needs to be careful since lower resolution not only excludes more small pores, but also has the potential to overestimate the pore size and thereby the permeability. Kozeny–Carman equation was used to estimate the permeability with geometric and diffusional tortuosity. The results indicate that the latter tortuosity can serve better for the permeability estimation than the former.</description><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Hydrogeology</subject><subject>Hydrology</subject><subject>Hydrology. Hydrogeology</subject><subject>Mathematical analysis</subject><subject>Permeability</subject><subject>Permeability estimation</subject><subject>Pixels</subject><subject>Pore-grain segmentation</subject><subject>Porosity</subject><subject>Resolution effect</subject><subject>Sandstone</subject><subject>Small pore effect</subject><subject>Tomography</subject><subject>Tortuosity</subject><subject>X-rays</subject><issn>0022-1694</issn><issn>1879-2707</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><recordid>eNqNkc2KFDEUhYMo2I4-gpCN4KbK_FSlkpXoMDrCgCAK7kIqdasnTSopk_RA7fQxfD2fxIzduNW7uZvv3nM4B6HnlLSUUPHq0B5utylF3zJCeUtZS5h8gHZUDqphAxkeoh0hjDVUqO4xepLzgdThvNuhH58gR38sLgYM8wy2YBfw1yaZDS_Opmjjsh4LTLjEJe6TWW837Bazd2GPTZhwXoz3eI0Jfn3_mbGNoSQ3nh6WiFdIC5jReVc2PMeEDX4LCQzO9TiXGOApejQbn-HZeV-gL--uPl9eNzcf33-4fHPTmI7J0kz9KPjYU6OUHMXQSdUzyntqTSeZJQOwnlBpYVSzVIMahtkY2UHPJaWTYJJfoJenv2uK346Qi15ctuC9CRCPWVMhlKwwV_-DdlQpLmhF-xNao8o5wazXVONJm6ZE37ejD_rcjr5vR1OmyR83L84SJlvj52SCdfnvcSV4tSIq9_rEQY3mzkHS2ToIFiaXall6iu4fSr8BVmOqig</recordid><startdate>20140314</startdate><enddate>20140314</enddate><creator>Peng, Sheng</creator><creator>Marone, Federica</creator><creator>Dultz, Stefan</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>SOI</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20140314</creationdate><title>Resolution effect in X-ray microcomputed tomography imaging and small pore’s contribution to permeability for a Berea sandstone</title><author>Peng, Sheng ; Marone, Federica ; Dultz, Stefan</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a428t-d5b63b51a998b67489521351ca482c07e25018ceb9f897977faa84e53811d6283</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Hydrogeology</topic><topic>Hydrology</topic><topic>Hydrology. Hydrogeology</topic><topic>Mathematical analysis</topic><topic>Permeability</topic><topic>Permeability estimation</topic><topic>Pixels</topic><topic>Pore-grain segmentation</topic><topic>Porosity</topic><topic>Resolution effect</topic><topic>Sandstone</topic><topic>Small pore effect</topic><topic>Tomography</topic><topic>Tortuosity</topic><topic>X-rays</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Peng, Sheng</creatorcontrib><creatorcontrib>Marone, Federica</creatorcontrib><creatorcontrib>Dultz, Stefan</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</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>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Journal of hydrology (Amsterdam)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Peng, Sheng</au><au>Marone, Federica</au><au>Dultz, Stefan</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Resolution effect in X-ray microcomputed tomography imaging and small pore’s contribution to permeability for a Berea sandstone</atitle><jtitle>Journal of hydrology (Amsterdam)</jtitle><date>2014-03-14</date><risdate>2014</risdate><volume>510</volume><spage>403</spage><epage>411</epage><pages>403-411</pages><issn>0022-1694</issn><eissn>1879-2707</eissn><coden>JHYDA7</coden><abstract>•A Berea sandstone sample was scanned twice under two different resolutions.•Higher resolution affect pore characteristic parameters by including small pores.•But small pores do not influence permeability (K) significantly.•Using diffusional tortuosity can estimate K better than geometric tortuosity.
Resolution selection when using X-ray microcomputed tomography should be made based on the compromise between accuracy and representativeness. The question is then how accurate is accurate enough, that is, how small a pore is small enough to be ignored without generating misleading results on pore representation and subsequent flow properties such as permeability. In this study, synchrotron X-ray microcomputed tomographic scans of a Berea sandstone sample were acquired for two resolutions (with 1.85 and 5.92μm pixel width). Higher resolution images resolve more small pores, and have similar large pores as the lower resolution images. Pore characterization and permeability estimation were conducted based on these two sets of images. The pore parameters and permeability were also measured for another larger sample from the same rock fragment through laboratory experiments. The comparison between the different resolution image analyses and the laboratory measurement indicates that small pores contribute to larger porosity, smaller tortuosity, and larger surface area, but do not influence permeability significantly. Therefore, relatively low resolution (pixel width up to 5.92μm) can be used for Berea sandstone when permeability is the focus. However, use of even lower resolution needs to be careful since lower resolution not only excludes more small pores, but also has the potential to overestimate the pore size and thereby the permeability. Kozeny–Carman equation was used to estimate the permeability with geometric and diffusional tortuosity. The results indicate that the latter tortuosity can serve better for the permeability estimation than the former.</abstract><cop>Kidlington</cop><pub>Elsevier B.V</pub><doi>10.1016/j.jhydrol.2013.12.028</doi><tpages>9</tpages></addata></record> |
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subjects | Earth sciences Earth, ocean, space Exact sciences and technology Hydrogeology Hydrology Hydrology. Hydrogeology Mathematical analysis Permeability Permeability estimation Pixels Pore-grain segmentation Porosity Resolution effect Sandstone Small pore effect Tomography Tortuosity X-rays |
title | Resolution effect in X-ray microcomputed tomography imaging and small pore’s contribution to permeability for a Berea sandstone |
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