Groundwater investigations in the Hattar industrial estate and its vicinity, Haripur district, Pakistan: An integrated approach

被引:15
|
作者
Nisar, Umair B. [1 ]
Khan, Muhammad J. [2 ]
Imran, Muhammad [3 ]
Khan, Muhammad R. [4 ]
Farooq, Muhammad [4 ]
Ehsan, Siddique A. [3 ]
Ahmad, Ashfaq [5 ]
Qazi, Hummad H. [6 ]
Rashid, Naim [7 ]
Manzoor, Tareq [8 ]
机构
[1] COMSATS Univ Islamabad, Ctr Climate Res & Dev CCRD, Islamabad, Pakistan
[2] Bahria Univ, Dept Earth & Environm Sci, Karachi Campus, Karachi, Pakistan
[3] COMSATS Univ Islamabad, Dept Phys, Lahore Campus, Lahore, Pakistan
[4] Univ Azad Jammu & Kashmir, Inst Geol, Muzaffarabad, Pakistan
[5] COMSATS Univ Islamabad, Dept Comp Sci, Lahore Campus, Lahore, Pakistan
[6] Univ Teknol, Innovat Engn Res Alliance, Skudai, Malaysia
[7] COMSATS Univ Islamabad, Dept Chem Engn, Lahore Campus, Lahore, Pakistan
[8] COMSATS Univ Islamabad, Energy Res Ctr, Lahore Campus, Lahore, Pakistan
关键词
Apparent resistivity; borehole; groundwater; hydro-chemical analysis; vertical electrical sounding;
D O I
10.48129/kjs.v48i1.7820
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The Hattar industrial estate in the Haripur district, Khyber Pakhtunkhwa (KPK), Pakistan, is investigated for the groundwater potential and aquifer vulnerability using vertical electrical sounding (VES) data, borehole logs, and hydrochemical analysis. A total of eight VES points were acquired in the Haripur region using Schlumberger configuration. The interpreted VES models are further constrained by four borehole logs to delineate comprehensive information of the thin lithological layers, subsurface layers configuration, and spatial extent in the area. A quantitative interpretation based on the VES and the borehole data suggests six main subsurface layers: (i) soil cover, (ii) gravel, (iii) clay, (iv) clay with gravel, (v) silty-clay, and (vi) sand with a boulder in the study area. A fence diagram is also generated to provide a detailed paleo-depositional model of the subsurface layers. The interpreted VES data is utilized to compute aquifer thickness, longitudinal conductance, and transverse resistance within the study area. The lateral extent and protective capacity for the aquifer were inferred from these measurements. The aquifer thickness is relatively low in the central and eastern parts ranging from 10 m to 11 m. The longitudinal conductance map shows values greater than 2 mhos from the central region to northern one. This is indicative of moderate to good protective capacity for the aquifer and is less vulnerable to infiltration of Hattar industrial polluted fluid. However, the values less than 0.19 mhos in the southwest and east are indicative of weak protective capacity with the risk of contamination. The hydrochemical analysis of the surface and subsurface water is carried out at eleven locations to identify the water quality within the study area. The chemical analysis of the water shows the presence of a high concentration of magnesium, bicarbonate, and chlorine away from the World Health Organization (WHO) standard.
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页码:106 / 115
页数:10
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