scholarly journals Study of Ground water Groundwater Potentiality and Sea Water Intrusion Along along the Coastal Plain, Wadi Thuwal, KSA- A Case Study Based on DC Resistivity

Author(s):  
Mansour A. Al-Garni ◽  
Hamdy I.E. Hassanein

The present study mainly aims to outline zones that have groundwater potentiality with good quality and those which are affected by sea water intrusion. The electrical resistivity data were acquired over an area of about 170 km2 of a coastal plain, Wadi Thuwal, which is bounded by the Red Sea in the west and the volcanic hills in the east.  In such an area, resistivity measurements, using n-layering model, reveal generally reveal a wide range of resistivity values which do not reflect the reality. Hence, the statistical analysis has to be involved to overcome this problem and to make the final interpretation reliable.  In our case, the n-layer models were modified to another statistical geoelectric models (SLM), consisting of  a number of layers equivalent to the stratigraphic layering beneath each VES site. The modified models were used to outline the depth to the bed rock, groundwater accumulation zones and  water table as well as to define the effect of sea water intrusion through the study area. Check alignment above  

2020 ◽  
Author(s):  
Wenfu Chen

<p>Temperature depth profiles has been applied on many topics, e.g. climate change, groundwater velocity and saltwater-groundwater interface. In this study, temperature depth profiles are used to identify the origin of groundwater salinization in Pingtung coastal plain, southern Taiwan. Some monitoring wells in the coastal area have reached salty groundwater. Even some of the deeper aquifers, down to 300 m are saltwater. There are two arguments for the origin of those saltwater. One theory is those saltwater were Holocene transgression relics. The other theory is that those saltwater were sea water intrusion due to over-pumping of groundwater. Using the measured temperature depth profiles, a 2D numerical model is developed to simulate the heat transfer of sea water intrusion. The preliminary results show that the cause of salinization is not likely by the modern sea water intrusion. The sea water below a depth of 100 m is a cooler source and the intrusion of sea water should decrease temperature in aquifer. However, the measured temperature data of those salty aquifer are higher.</p>


2012 ◽  
Vol 18 (3) ◽  
pp. 215-223 ◽  
Author(s):  
Ganesh D. Kale ◽  
B.K. Samtani ◽  
Shaileshkumar B. Patel ◽  
Hasmukh Patel ◽  
Nitisha J. Anajwala ◽  
...  

2021 ◽  
Vol 708 (1) ◽  
pp. 012002
Author(s):  
R S Yuliatmoko ◽  
T Kurniawan ◽  
B Sunardi ◽  
T Hardy ◽  
A A Martha ◽  
...  

Engineering ◽  
2021 ◽  
Vol 13 (07) ◽  
pp. 388-398
Author(s):  
Dorcas Mutheu Musingi ◽  
Michael Mbindyo Munywoki ◽  
Benjamin Musyimi Musingi

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