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Document Details
Document Type
:
Article In Journal
Document Title
:
Application of Magnetic and Electrical Geophysical Methods in the Exploration of Groundwater Resources of Wadi Malakan, Saudi Arabia
تطبيق الطرق الجيوفيزيائية المغنطيسية والكهربائية لاستكشاف المياة الجوفية في وادي ملكان ، المملكة العربية السعودية
Subject
:
Earth Sciences
Document Language
:
English
Abstract
:
Magnetic and DC resistivity methods are utilized at Wadi Malakan, Makkah Al-Mukarramah region, Saudi Arabia. Land magnetic survey is conducted to identify the main structure and the depth to the basement along the surveyed part of the wadi. 2-D Euler deconvolution technique is used and reveals the depth to magnetic sources and possible faults that may affect the groundwater flow. Profiling using Wenner array is used to identify the minimum resistivity value along each profile to provide the optimum location for conducting sounding. Sounding using Schlumberger array is used to delineate the saturation zones and the depth to basement at most significant selected sites. The integration between magnetic and DC resistivity methods provides valuable information about the possible location of saturated zones at the conducted part of the wadi. The results of the interpreted vertical electrical resisitivity soundings at VES6004 and VES6010 are confirmed by drilling. The coefficient of anisotropy is calculated and found to be very low which reveals that there is no preferential direction for current flow in which the average transverse resistivity is almost the same as the average longitudinal resistivity which implies that the wadi deposits are not stratified.
ISSN
:
1012-8832
Journal Name
:
Earth Sciences Journal
Volume
:
16
Issue Number
:
1
Publishing Year
:
1426 AH
2005 AD
Number Of Pages
:
26
Article Type
:
Article
Added Date
:
Sunday, October 11, 2009
Researchers
Researcher Name (Arabic)
Researcher Name (English)
Researcher Type
Dr Grade
Email
منصور عبدالله القرني
MANSOUR ABDULLAH Al-GARNI
Researcher
Files
File Name
Type
Description
21517.pdf
pdf
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