TY - JOUR
T1 - Application of time-domain electromagnetic method in mapping saltwater intrusion of a coastal alluvial aquifer, North Oman
AU - El-Kaliouby, Hesham
AU - Abdalla, Osman
N1 - Publisher Copyright:
© 2015 Elsevier B.V.
PY - 2015/4/1
Y1 - 2015/4/1
N2 - One-third of the population of Oman depends on the groundwater extracted from the alluvium deposits located along the coast of the Gulf of Oman. However, groundwater depletion and seawater intrusion constitute major challenges along the coastal water accumulations in Oman. The objective of this study is to locate the extent of seawater intrusion and to map the shallow alluvial aquifer in the region, where water accumulates from the rain or the flooding at AlKhod dam. In order to assess the effect of groundwater infiltration, which recharges the aquifer and fights the seawater invasion, a quantitative approach for the groundwater quality and distribution is required to provide reasonable knowledge on the spatial distribution of the aquifers, their thickness and the type of sediments. When groundwater wells and their subsurface geologic and electrical logs are not available or not deep enough, surface geophysical surveys can be considered due to their low cost and short acquisition time. The application of time-domain electromagnetic (TDEM) method in Al-Khod area, Oman has proven to be a successful tool in mapping the fresh/saline water interface and for locating the depth of fresh water aquifer. The depths and inland extents of the saline zone were mapped along three N-S TDEM profiles. The depths to the freshwater table and saline interface calculated from TDEM closely match the available well data.
AB - One-third of the population of Oman depends on the groundwater extracted from the alluvium deposits located along the coast of the Gulf of Oman. However, groundwater depletion and seawater intrusion constitute major challenges along the coastal water accumulations in Oman. The objective of this study is to locate the extent of seawater intrusion and to map the shallow alluvial aquifer in the region, where water accumulates from the rain or the flooding at AlKhod dam. In order to assess the effect of groundwater infiltration, which recharges the aquifer and fights the seawater invasion, a quantitative approach for the groundwater quality and distribution is required to provide reasonable knowledge on the spatial distribution of the aquifers, their thickness and the type of sediments. When groundwater wells and their subsurface geologic and electrical logs are not available or not deep enough, surface geophysical surveys can be considered due to their low cost and short acquisition time. The application of time-domain electromagnetic (TDEM) method in Al-Khod area, Oman has proven to be a successful tool in mapping the fresh/saline water interface and for locating the depth of fresh water aquifer. The depths and inland extents of the saline zone were mapped along three N-S TDEM profiles. The depths to the freshwater table and saline interface calculated from TDEM closely match the available well data.
KW - Coastal aquifers
KW - Electromagnetic methods
KW - Groundwater
KW - Salinization
KW - Sea water intrusion
KW - Time-Domain
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U2 - 10.1016/j.jappgeo.2015.02.003
DO - 10.1016/j.jappgeo.2015.02.003
M3 - Article
AN - SCOPUS:84923040750
SN - 0926-9851
VL - 115
SP - 59
EP - 64
JO - Journal of Applied Geophysics
JF - Journal of Applied Geophysics
ER -