Determination of Groundwater Storage Variation, Deficit, and Abstraction in Afghanistan and the Assessment of the Evolution of Vadose Zone in Kabul City
Mohammad Taqi Daqiq, Ravi Sharma, Anuradha Karunakalage, Suresh Kannaujiya
Abstract
Groundwater is Afghanistan’s main water supply resource, but the insufficient information and mismanagement of the surface and groundwater system have resulted in an alarming shortage of this precious resource. The monthly groundwater storage variation (ΔGWS) has been calculated in (mm) with a trend (mm/month) for the time interval of April 2002 to October 2021 using the Gravity Recovery And Climate Experiment (GRACE) dataset for five major river basins of Afghanistan. A maximum and a minimum deseasonalized ΔGWS are observed at Amu Darya (246 mm to -253 mm) and Hari Rud (89 mm to -102 mm) basins, respectively. Subsequently, the Groundwater Storage Deficit (GWSD) and GWSD Index (GWSDI) were calculated, and a negative GWSDI value signified the groundwater drought. Analysis of the Groundwater Storage Abstraction (GWS <sub xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">abs</sub> ) has also been carried out for the entire country. The estimated GWS <sub xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">abs</sub> trend gives a maximum value of 12.60 mm/year in the Northeast and Southwest parts of the country. A Spatio-temporal analysis showed the maximum GWS <sub xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">abs</sub> variation up to 23.12 mm in 2021. Two phases of land deformation were determined in Kabul City using the Interferometric Synthetic Aperture Radar (InSAR) technique. In phase-I (2015-2017), there is a gentle negative trend (-20.66 mm/year in Upper Kabul and -18.54 mm/year in Lower Kabul), but in phase-II (2018-2020), a high negative trend (-151.34 mm/year in Upper Kabul and -145.32 mm/year in Lower Kabul). Overall, the entire country is experiencing a severe groundwater decline, apparently from the interplay of hydroclimatic and anthropogenic factors, which are most dominant in the southern and western parts of Afghanistan.