The Implementation of 2-D Resistivity Method in Verifying Paleozoic Aquifer Properties at Bukit Chondong, Perlis (Malaysia)

Southeast Asian Conference on Geophysics

Maslinda, Umi^1 ; Nordiana, M.M.^1 ; Bery, A.A.^1 ; Afiq Saharudin, Muhamad^1 ; Hisham, Hazrul^1 ; Taqiuddin, Z.M.^1 ; Sulaiman, Nabila^1 ; Nur Amalina, M.K.A.^1 ; Nordiana, A.N.^1

Geophysics Section, School of Physics, Universiti Sains Malaysia, Penang

11800, Malaysia^1

关键词: Aquifer characteristics;    Aquifer properties;    Electrical insulators;    Geologic materials;    Geological information;    Interstitial water;    Subsurface distribution;    Water-bearing rocks;   

Others  :  https://iopscience.iop.org/article/10.1088/1755-1315/62/1/012042/pdf
DOI  :  10.1088/1755-1315/62/1/012042

来源: IOP

【 摘 要 】

The research was conducted using 2-D resistivity in verifying Paleozoic aquifer. Since most geologic materials behave as electrical insulators, surface measurements of earth resistivity are controlled by the electrolytic ability of interstitial water. The subsurface distribution of water is controlled by the porosity of the formations. The study area is at Bukit Chondong, Beseri, Perlis. Bukit Chondong is made of sedimentary rock which mostly is sandstone. Bukit Chondong is from uppermost of the Kubang Pasu Formation that represented by a thick unit of grey mudstone interbedded with sandstone. The Kubang Pasu Formation was influenced by shallow marine during the early age. Paleocurrent and fossils traces were found on the mudstone at the study area. The area is suspected to be a Paleozoic aquifer because the sandstone can be a productive aquifer with diffuse flow. The water movement in sandstone is through the fractures and joints. Most of the water stores and transmits in sandstone. The interbedded sandstone and mudstone is one of the aquifer characteristic. Sandstone and mudstone are water-bearing rocks and low-permeable rocks respectively. The data was processed according to the geological information of the study area since there was an outcrop. The study area have low resistivity value which both sandstone and mudstone give less than 800 Ohm-m due to the water content (Sulphide and clay).