Hydro-geophysical investigation of groundwater resources potential in Dashti-e-Archi alluvial aquifer, Northeastern Afghanistan

Groundwater is the primary source of water for drinking, domestic use, and agricultural in northern Afghanistan. However, due to over four decades of political instability, the region’s groundwater resources remain poorly understood. Identifying optimal locations for water supply schemes considering...

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Main Authors: Rohullah Sediqi, Mansoor Mudaser, Vladimir B. Zalishchak, Abdulhalim Zaryab
Format: Article
Language:English
Published: Elsevier 2025-12-01
Series:Results in Earth Sciences
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Online Access:http://www.sciencedirect.com/science/article/pii/S221171482500055X
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author Rohullah Sediqi
Mansoor Mudaser
Vladimir B. Zalishchak
Abdulhalim Zaryab
author_facet Rohullah Sediqi
Mansoor Mudaser
Vladimir B. Zalishchak
Abdulhalim Zaryab
author_sort Rohullah Sediqi
collection DOAJ
description Groundwater is the primary source of water for drinking, domestic use, and agricultural in northern Afghanistan. However, due to over four decades of political instability, the region’s groundwater resources remain poorly understood. Identifying optimal locations for water supply schemes considering both quantity and quality is further complicated by the widespread presence of fine-grained materials. This study employed vertical Electrical Sounding (VES) using the Schlumberger configuration in the village of Arbab Rahim Dolat Zai, located in the Dasht-e-Archi district of Kunduz Province. The VES data were interpreted using IPI2Win and ZONDIP1D software. Among the surveyed sites, only the VES1 was identified as optimal, enabling consistent drilling penetration through all five geo-electric layers. Of the five strata, the fourth located at depths of 33–120 ± 10 m and composed primarily of sand, silt and gravel interbedded with clay were recognized as the principal aquifers. These findings were corroborated by lithological logs, validating the reliability of the geophysical interpretations. Additionally, the Thiem and Dupuit equations were applied to analyses steady-state groundwater flow, facilitating the estimation of hydraulic conductivity and transmissivity. The results provide valuable insights to support policymakers and engineers in the sustainable and effectively management groundwater resources in northern Afghanistan.
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issn 2211-7148
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spelling doaj-art-943f17b328e94dff89d45abea7dd51132025-08-20T03:28:38ZengElsevierResults in Earth Sciences2211-71482025-12-01310011310.1016/j.rines.2025.100113Hydro-geophysical investigation of groundwater resources potential in Dashti-e-Archi alluvial aquifer, Northeastern AfghanistanRohullah Sediqi0Mansoor Mudaser1Vladimir B. Zalishchak2Abdulhalim Zaryab3Department of Information Technology in Subsoil Use, Faculty of Geology, Far Eastern Federal University, Vladivostok 690091, RussiaDepartment of Rural Water Supply and Sanitation Program, Ministry of Rural Rehabilitation and Development, Kabul 1001, AfghanistanDepartment of Information Technology in Subsoil Use, Faculty of Geology, Far Eastern Federal University, Vladivostok 690091, RussiaDepartment of Engineering Geology and Hydrogeology, Faculty of Geology and Mines, Polytechnic University, Kabul, Afghanistan; Corresponding author.Groundwater is the primary source of water for drinking, domestic use, and agricultural in northern Afghanistan. However, due to over four decades of political instability, the region’s groundwater resources remain poorly understood. Identifying optimal locations for water supply schemes considering both quantity and quality is further complicated by the widespread presence of fine-grained materials. This study employed vertical Electrical Sounding (VES) using the Schlumberger configuration in the village of Arbab Rahim Dolat Zai, located in the Dasht-e-Archi district of Kunduz Province. The VES data were interpreted using IPI2Win and ZONDIP1D software. Among the surveyed sites, only the VES1 was identified as optimal, enabling consistent drilling penetration through all five geo-electric layers. Of the five strata, the fourth located at depths of 33–120 ± 10 m and composed primarily of sand, silt and gravel interbedded with clay were recognized as the principal aquifers. These findings were corroborated by lithological logs, validating the reliability of the geophysical interpretations. Additionally, the Thiem and Dupuit equations were applied to analyses steady-state groundwater flow, facilitating the estimation of hydraulic conductivity and transmissivity. The results provide valuable insights to support policymakers and engineers in the sustainable and effectively management groundwater resources in northern Afghanistan.http://www.sciencedirect.com/science/article/pii/S221171482500055XGroundwaterGeo-electrical surveyAlluvial aquiferHydraulic conductivity
spellingShingle Rohullah Sediqi
Mansoor Mudaser
Vladimir B. Zalishchak
Abdulhalim Zaryab
Hydro-geophysical investigation of groundwater resources potential in Dashti-e-Archi alluvial aquifer, Northeastern Afghanistan
Results in Earth Sciences
Groundwater
Geo-electrical survey
Alluvial aquifer
Hydraulic conductivity
title Hydro-geophysical investigation of groundwater resources potential in Dashti-e-Archi alluvial aquifer, Northeastern Afghanistan
title_full Hydro-geophysical investigation of groundwater resources potential in Dashti-e-Archi alluvial aquifer, Northeastern Afghanistan
title_fullStr Hydro-geophysical investigation of groundwater resources potential in Dashti-e-Archi alluvial aquifer, Northeastern Afghanistan
title_full_unstemmed Hydro-geophysical investigation of groundwater resources potential in Dashti-e-Archi alluvial aquifer, Northeastern Afghanistan
title_short Hydro-geophysical investigation of groundwater resources potential in Dashti-e-Archi alluvial aquifer, Northeastern Afghanistan
title_sort hydro geophysical investigation of groundwater resources potential in dashti e archi alluvial aquifer northeastern afghanistan
topic Groundwater
Geo-electrical survey
Alluvial aquifer
Hydraulic conductivity
url http://www.sciencedirect.com/science/article/pii/S221171482500055X
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AT vladimirbzalishchak hydrogeophysicalinvestigationofgroundwaterresourcespotentialindashtiearchialluvialaquifernortheasternafghanistan
AT abdulhalimzaryab hydrogeophysicalinvestigationofgroundwaterresourcespotentialindashtiearchialluvialaquifernortheasternafghanistan