The study is conducted to focus on the subsurface geological and hydrological mapping for groundwater presence in the area located Nooriabad of the Jamshoro district left side of M-9 Motorway toward Karachi, Sindh, Pakistan. Vertical electrical sounding (VES) is carried out by using the Schlumberger electrode array method with ranging from 02 to 300 m. IPI2win software is used on the collected data of VES to interpret with qualitatively that indicated the four distinct lithological units demarcated as clay, sandy clay, shale and alluvium or weathered layer of Tiyon formation and limestone and fractured sandstone beds of the Laki formation of Eocene age. On the collected VES data, it is concluded that the first and second layer of soil is 16 m thick and composed of shale to clay beds and alluvium having the apparent resistivity between 05 and 15 Ωm. With increasing depth from 50 to 100 m, it is interpreted that there are fractured sandstone and limestone beds with average resistivity ranges between 15 to 60 Ωm. Further, processed the data and generated pseudo-section, apparent resistivity section and statistical curve by using software IPI2win to interpret the apparent resistivity map at 50, 60, 70 and 80 m are correlated with the hydrogeology and geology of the area. The results are interpreted that the good aquifer zones are present in the 50–100-m-thick limestone and fractured sandstone beds having interconnection with clay. Accumulation of groundwater is found by controlling the physiography and geological structure of the study area.
2
Dostęp do pełnego tekstu na zewnętrznej witrynie WWW
The study was conducted to assess the groundwater potential at Haji Rehmatullah Palari village aquifer, Union Council Sari of Kalu Khuhar along M-9 Motorway near Nooriabad, Sindh, Pakistan, through vertical electrical sounding (VES) by using Schlumberger electrode array method with 02–210 m. The collected data of 12 VES were interpreted by using IPI2win software. Monsoon rainfall period is very short, which starts from July to September (every year in Pakistan). Average rainfall is 150 mm with variation of 25 mm, in some year zero rainfall. During summer season, the evaporation and transpiration rate are about 70%, while the infiltration rate is 15%. Kalu Nadi (hill torrent) is the only source of recharge of this aquifer that depends on the rainfall. Lithological logs interpreted that mostly aquifers are present in sandstone lithology of Nari Formation which hold these freshwater aquifers having minimum 50 m thickness and have great potential for freshwater exploitation. Lithological logs interpreted that mostly aquifers persist in sandstone lithology of Nari Formation which hold the freshwater. Totally, five tube wells were installed at this aquifer and discharging the freshwater of about 98.55 million gallons per year and rapidly depleting the aquifers. Water business is also observed at this aquifer which was breaking influenced on the aquifer without considering the agricultural development to protect the environment. The aquifer is under pressure to drawdown and may suffer with its quantity and quality, if this trend continues.
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.