Time-lapse resistivity investigation of salinity changes at an ex-promontory land: a case study of Carey Island, Selangor, Malaysia

Time-lapse resistivity measurements and groundwater geochemistry were used to study salinity effect on groundwater aquifer at the ex-promontory-land of Carey Island in Malaysia. Resistivity was measured by ABEM Terrameter SAS4000 and ES10-64 electrode selector. Re�lationship between earth resis...

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Main Authors: Baharuddin, Mohamad Faizal Tajul, Taib, Samsudin, Hashim, Roslan, Zainal Abidin, Mohd Hazreek, Ishak, Mohd Fakhrurrazi
Format: Article
Language:English
Published: Springer 2011
Subjects:
Online Access:http://eprints.uthm.edu.my/7894/
http://eprints.uthm.edu.my/7894/1/J3626_e8c4bf18776656c105d24550c43af8b7.pdf
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author Baharuddin, Mohamad Faizal Tajul
Taib, Samsudin
Hashim, Roslan
Zainal Abidin, Mohd Hazreek
Ishak, Mohd Fakhrurrazi
author_facet Baharuddin, Mohamad Faizal Tajul
Taib, Samsudin
Hashim, Roslan
Zainal Abidin, Mohd Hazreek
Ishak, Mohd Fakhrurrazi
author_sort Baharuddin, Mohamad Faizal Tajul
building UTHM Institutional Repository
collection Online Access
description Time-lapse resistivity measurements and groundwater geochemistry were used to study salinity effect on groundwater aquifer at the ex-promontory-land of Carey Island in Malaysia. Resistivity was measured by ABEM Terrameter SAS4000 and ES10-64 electrode selector. Re�lationship between earth resistivity and total dissolved solids (TDS) was derived, and with re�sistivity images, used to identify water types: fresh (ρe > 6.5 � m), brackish (3 � m < ρe < 6.5 � m), or saline (ρe < 3 � m). Long-term monitoring of the studied area’s groundwater quality via measurements of its time-lapse resistivity showed salinity changes in the island’s groundwater aquifers not conforming to seawater-freshwater hydraulic gradient. In some aquifers far from the coast, saline water was dominant, while in some others, freshwater 30 m thick showed ground�water potential. Land transformation is believed to have changed the island’s hydrogeology, which receives saltwater pressure all the time, limiting freshwater recharge to the groundwater system. The time-lapse resistivity measurements showed active salinity changes at resistivity-image bottom moving up the image for two seasons’ (wet and dry) conditions. The salinity changes are believed to have been caused by incremental tide passing through highly porous material in the active-salinity-change area. The study’s results were used to plan a strategy for sustainable groundwater exploration of the island.
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spelling uthm-78942022-10-17T06:21:55Z http://eprints.uthm.edu.my/7894/ Time-lapse resistivity investigation of salinity changes at an ex-promontory land: a case study of Carey Island, Selangor, Malaysia Baharuddin, Mohamad Faizal Tajul Taib, Samsudin Hashim, Roslan Zainal Abidin, Mohd Hazreek Ishak, Mohd Fakhrurrazi T Technology (General) Time-lapse resistivity measurements and groundwater geochemistry were used to study salinity effect on groundwater aquifer at the ex-promontory-land of Carey Island in Malaysia. Resistivity was measured by ABEM Terrameter SAS4000 and ES10-64 electrode selector. Re�lationship between earth resistivity and total dissolved solids (TDS) was derived, and with re�sistivity images, used to identify water types: fresh (ρe > 6.5 � m), brackish (3 � m < ρe < 6.5 � m), or saline (ρe < 3 � m). Long-term monitoring of the studied area’s groundwater quality via measurements of its time-lapse resistivity showed salinity changes in the island’s groundwater aquifers not conforming to seawater-freshwater hydraulic gradient. In some aquifers far from the coast, saline water was dominant, while in some others, freshwater 30 m thick showed ground�water potential. Land transformation is believed to have changed the island’s hydrogeology, which receives saltwater pressure all the time, limiting freshwater recharge to the groundwater system. The time-lapse resistivity measurements showed active salinity changes at resistivity-image bottom moving up the image for two seasons’ (wet and dry) conditions. The salinity changes are believed to have been caused by incremental tide passing through highly porous material in the active-salinity-change area. The study’s results were used to plan a strategy for sustainable groundwater exploration of the island. Springer 2011 Article PeerReviewed text en http://eprints.uthm.edu.my/7894/1/J3626_e8c4bf18776656c105d24550c43af8b7.pdf Baharuddin, Mohamad Faizal Tajul and Taib, Samsudin and Hashim, Roslan and Zainal Abidin, Mohd Hazreek and Ishak, Mohd Fakhrurrazi (2011) Time-lapse resistivity investigation of salinity changes at an ex-promontory land: a case study of Carey Island, Selangor, Malaysia. Environ Monit Assess. pp. 345-369. https://doi.org/ 10.1007/s10661-010-1792-x
spellingShingle T Technology (General)
Baharuddin, Mohamad Faizal Tajul
Taib, Samsudin
Hashim, Roslan
Zainal Abidin, Mohd Hazreek
Ishak, Mohd Fakhrurrazi
Time-lapse resistivity investigation of salinity changes at an ex-promontory land: a case study of Carey Island, Selangor, Malaysia
title Time-lapse resistivity investigation of salinity changes at an ex-promontory land: a case study of Carey Island, Selangor, Malaysia
title_full Time-lapse resistivity investigation of salinity changes at an ex-promontory land: a case study of Carey Island, Selangor, Malaysia
title_fullStr Time-lapse resistivity investigation of salinity changes at an ex-promontory land: a case study of Carey Island, Selangor, Malaysia
title_full_unstemmed Time-lapse resistivity investigation of salinity changes at an ex-promontory land: a case study of Carey Island, Selangor, Malaysia
title_short Time-lapse resistivity investigation of salinity changes at an ex-promontory land: a case study of Carey Island, Selangor, Malaysia
title_sort time-lapse resistivity investigation of salinity changes at an ex-promontory land: a case study of carey island, selangor, malaysia
topic T Technology (General)
url http://eprints.uthm.edu.my/7894/
http://eprints.uthm.edu.my/7894/
http://eprints.uthm.edu.my/7894/1/J3626_e8c4bf18776656c105d24550c43af8b7.pdf