Comment on paper ‘Stream depletion predictions using pumping test data from a heterogeneous stream-aquifer system (a case study from the Great Plains, USA)’ by Stefan J. Kollet and Vitaly A. Zlotnik, vol. 281: 96–114

2005 ◽  
Vol 313 (3-4) ◽  
pp. 153-157 ◽  
Author(s):  
Hilary Lough
2021 ◽  
Vol 126 ◽  
pp. 104871
Author(s):  
Waleed Saeed ◽  
Orfan Shouakar-Stash ◽  
André Unger ◽  
Warren W. Wood ◽  
Beth Parker

Author(s):  
Sonu Singh ◽  
Joseph Tripura

Abstract Groundwater conditions (GWCs) of an area depends on aquifer hydraulic parameters such as storativity () or storage coefficient (), transmissivity () and hydraulic conductivity (). It plays a key role concerning- groundwater flow modeling, well performance, solute and contaminants transports assessment and also for identification of areas for additional hydrologic testing. Specifically, the geologic formation of a regions control the porosity and permeability, however, in hilly terrain prospecting ground water potential is more challenging due to its limited extent and its occurrences that are usually confined to fractures and weathered rocks. The present study, aims at estimating the hydraulic parameters through pumping test analysis to assess aquifer system formation on hilly terrain from 16 bore wells. The aforesaid parameters were examined through a case study in some selective regions of Hamirpur district of Himachal Pradesh, India. The study area is controlled under two main geological horizons that is the post-tertiary and tertiary. The papers end with comparative results of hydraulic parameters and the aquifers system formation on different GWCs which may be helpful in the outlook of sustainable groundwater resource in the regions.


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