Characterization of aquifer system using electrical resistivity tomography (ERT) and induced polarisation (IP) techniques
Groundwater plays a major role as an alternative freshwater resource for irrigation and industrial purposes. This study aimed to characterize the subsurface of aquifer systems in TelukIntan district, Perak, Malaysia using Electrical Resistivity Tomography (ERT) and Induced Polarization (IP) methods....
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| Veröffentlicht in: | IOP conference series. Earth and environmental science 2021-10, Vol.880 (1), p.12025 |
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| creator | Akhtar, N Mislan, M S Syakir, M I Anees, M T Yusuff, M S M |
| description | Groundwater plays a major role as an alternative freshwater resource for irrigation and industrial purposes. This study aimed to characterize the subsurface of aquifer systems in TelukIntan district, Perak, Malaysia using Electrical Resistivity Tomography (ERT) and Induced Polarization (IP) methods. The horizontal profiling (TL1 and TL2) was conducted at length of 400 m. The estimated depth is 150 m below ground level (b.g.l.). An ABEM SAS 4000 Terrameter and ABEM LUND ES464 Imaging System were applied to create a resistivity pseudo-section using polar-dipole configuration. The collected geo-electrical data was interpreted using RESIST software with partial curve matching and computer iteration. ERT and IP survey profile results were validated with in-situ borehole data from borehole 2 (B2). Eleven samples of soil profile were collected at depth from 5.6 m to 61.2 m, with average percentage of sand, silt and clay are 93.77 %, 5.78 % and 0.02 %, respectively. The geology of subsurface settings is the key factor in determining the aquifer system characterized by interlayer sand-silt sequence indicating the saturation zone of aquifer underlain by shale at the bottom. Further study on hydraulics perspective is important to understand the overall capacity of the aquifer. |
| doi_str_mv | 10.1088/1755-1315/880/1/012025 |
| format | Article |
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This study aimed to characterize the subsurface of aquifer systems in TelukIntan district, Perak, Malaysia using Electrical Resistivity Tomography (ERT) and Induced Polarization (IP) methods. The horizontal profiling (TL1 and TL2) was conducted at length of 400 m. The estimated depth is 150 m below ground level (b.g.l.). An ABEM SAS 4000 Terrameter and ABEM LUND ES464 Imaging System were applied to create a resistivity pseudo-section using polar-dipole configuration. The collected geo-electrical data was interpreted using RESIST software with partial curve matching and computer iteration. ERT and IP survey profile results were validated with in-situ borehole data from borehole 2 (B2). Eleven samples of soil profile were collected at depth from 5.6 m to 61.2 m, with average percentage of sand, silt and clay are 93.77 %, 5.78 % and 0.02 %, respectively. The geology of subsurface settings is the key factor in determining the aquifer system characterized by interlayer sand-silt sequence indicating the saturation zone of aquifer underlain by shale at the bottom. Further study on hydraulics perspective is important to understand the overall capacity of the aquifer.</description><identifier>ISSN: 1755-1307</identifier><identifier>EISSN: 1755-1315</identifier><identifier>DOI: 10.1088/1755-1315/880/1/012025</identifier><language>eng</language><publisher>Bristol: IOP Publishing</publisher><subject>Aquifer system ; Aquifer systems ; Aquifers ; Boreholes ; Dipoles ; Electrical resistivity ; electrical resistivity tomography (ERT) ; Fluid flow ; Freshwater resources ; Geology ; Ground level ; Groundwater ; Hydraulics ; induced polarisation (IP) ; Induced polarization ; Interlayers ; Iterative methods ; Polarization ; Sand ; Saturation zone ; Shale ; Silt ; Soil profiles ; Soil properties ; sub surface profiling ; Tomography</subject><ispartof>IOP conference series. Earth and environmental science, 2021-10, Vol.880 (1), p.12025</ispartof><rights>Published under licence by IOP Publishing Ltd</rights><rights>2021. 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Earth and environmental science</title><addtitle>IOP Conf. Ser.: Earth Environ. Sci</addtitle><description>Groundwater plays a major role as an alternative freshwater resource for irrigation and industrial purposes. This study aimed to characterize the subsurface of aquifer systems in TelukIntan district, Perak, Malaysia using Electrical Resistivity Tomography (ERT) and Induced Polarization (IP) methods. The horizontal profiling (TL1 and TL2) was conducted at length of 400 m. The estimated depth is 150 m below ground level (b.g.l.). An ABEM SAS 4000 Terrameter and ABEM LUND ES464 Imaging System were applied to create a resistivity pseudo-section using polar-dipole configuration. The collected geo-electrical data was interpreted using RESIST software with partial curve matching and computer iteration. ERT and IP survey profile results were validated with in-situ borehole data from borehole 2 (B2). Eleven samples of soil profile were collected at depth from 5.6 m to 61.2 m, with average percentage of sand, silt and clay are 93.77 %, 5.78 % and 0.02 %, respectively. The geology of subsurface settings is the key factor in determining the aquifer system characterized by interlayer sand-silt sequence indicating the saturation zone of aquifer underlain by shale at the bottom. Further study on hydraulics perspective is important to understand the overall capacity of the aquifer.</description><subject>Aquifer system</subject><subject>Aquifer systems</subject><subject>Aquifers</subject><subject>Boreholes</subject><subject>Dipoles</subject><subject>Electrical resistivity</subject><subject>electrical resistivity tomography (ERT)</subject><subject>Fluid flow</subject><subject>Freshwater resources</subject><subject>Geology</subject><subject>Ground level</subject><subject>Groundwater</subject><subject>Hydraulics</subject><subject>induced polarisation (IP)</subject><subject>Induced polarization</subject><subject>Interlayers</subject><subject>Iterative methods</subject><subject>Polarization</subject><subject>Sand</subject><subject>Saturation zone</subject><subject>Shale</subject><subject>Silt</subject><subject>Soil profiles</subject><subject>Soil properties</subject><subject>sub surface profiling</subject><subject>Tomography</subject><issn>1755-1307</issn><issn>1755-1315</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>O3W</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNqFkF1LwzAUhosoOKd_QQLezIva5LTpx6WMqYOBovM6pGm6ZXRNl6RC_fW2VCaC4NU5cN7nPfB43jXBdwSnaUASSn0SEhqkKQ5IgAlgoCfe5Hg4Pe44OfcurN1hHCdRmE28br7lhgsnjfrkTuka6RLxQ6tKaZDtrJN71FpVb5CspHBGCV4hI62yTn0o1yGn93pjeLPt0Gzxur5FvC6QqotWyAI1uuJG2bF4tny5RU6Kba0OrbSX3lnJKyuvvufUe39YrOdP_ur5cTm_X_kiBKB-CjlkSZyXMVDOS8gxyROIUxJBlIeAJZFCQCEhE1nUI7nEECfAS0EhpTwPp97N2NsYPfx1bKdbU_cvGdAsSSPAJOlT8ZgSRltrZMkao_bcdIxgNmhmg0E22GS9ZkbYqLkHYQSVbn6a_4Vmf0CLxduvGGuKMvwCLyiNHw</recordid><startdate>20211001</startdate><enddate>20211001</enddate><creator>Akhtar, N</creator><creator>Mislan, M S</creator><creator>Syakir, M I</creator><creator>Anees, M T</creator><creator>Yusuff, M S M</creator><general>IOP Publishing</general><scope>O3W</scope><scope>TSCCA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>PATMY</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PYCSY</scope></search><sort><creationdate>20211001</creationdate><title>Characterization of aquifer system using electrical resistivity tomography (ERT) and induced polarisation (IP) techniques</title><author>Akhtar, N ; Mislan, M S ; Syakir, M I ; Anees, M T ; Yusuff, M S M</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3225-82b2976bf625aaf2b01b72681424b320e1ecc2de29c94c32be02672afc5285ab3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Aquifer system</topic><topic>Aquifer systems</topic><topic>Aquifers</topic><topic>Boreholes</topic><topic>Dipoles</topic><topic>Electrical resistivity</topic><topic>electrical resistivity tomography (ERT)</topic><topic>Fluid flow</topic><topic>Freshwater resources</topic><topic>Geology</topic><topic>Ground level</topic><topic>Groundwater</topic><topic>Hydraulics</topic><topic>induced polarisation (IP)</topic><topic>Induced polarization</topic><topic>Interlayers</topic><topic>Iterative methods</topic><topic>Polarization</topic><topic>Sand</topic><topic>Saturation zone</topic><topic>Shale</topic><topic>Silt</topic><topic>Soil profiles</topic><topic>Soil properties</topic><topic>sub surface profiling</topic><topic>Tomography</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Akhtar, N</creatorcontrib><creatorcontrib>Mislan, M S</creatorcontrib><creatorcontrib>Syakir, M I</creatorcontrib><creatorcontrib>Anees, M T</creatorcontrib><creatorcontrib>Yusuff, M S M</creatorcontrib><collection>Institute of Physics Open Access Journal Titles</collection><collection>IOPscience (Open Access)</collection><collection>CrossRef</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>Environmental Science Database</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Environmental Science Collection</collection><jtitle>IOP conference series. 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This study aimed to characterize the subsurface of aquifer systems in TelukIntan district, Perak, Malaysia using Electrical Resistivity Tomography (ERT) and Induced Polarization (IP) methods. The horizontal profiling (TL1 and TL2) was conducted at length of 400 m. The estimated depth is 150 m below ground level (b.g.l.). An ABEM SAS 4000 Terrameter and ABEM LUND ES464 Imaging System were applied to create a resistivity pseudo-section using polar-dipole configuration. The collected geo-electrical data was interpreted using RESIST software with partial curve matching and computer iteration. ERT and IP survey profile results were validated with in-situ borehole data from borehole 2 (B2). Eleven samples of soil profile were collected at depth from 5.6 m to 61.2 m, with average percentage of sand, silt and clay are 93.77 %, 5.78 % and 0.02 %, respectively. The geology of subsurface settings is the key factor in determining the aquifer system characterized by interlayer sand-silt sequence indicating the saturation zone of aquifer underlain by shale at the bottom. Further study on hydraulics perspective is important to understand the overall capacity of the aquifer.</abstract><cop>Bristol</cop><pub>IOP Publishing</pub><doi>10.1088/1755-1315/880/1/012025</doi><tpages>14</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | Aquifer system Aquifer systems Aquifers Boreholes Dipoles Electrical resistivity electrical resistivity tomography (ERT) Fluid flow Freshwater resources Geology Ground level Groundwater Hydraulics induced polarisation (IP) Induced polarization Interlayers Iterative methods Polarization Sand Saturation zone Shale Silt Soil profiles Soil properties sub surface profiling Tomography |
| title | Characterization of aquifer system using electrical resistivity tomography (ERT) and induced polarisation (IP) techniques |
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