Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...

GroMoPo Metadata for Chaj Doab MODFLOW model


Authors:
Owners: This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) for information on this resource.
Type: Resource
Storage: The size of this resource is 1.6 KB
Created: Feb 08, 2023 at 8:18 p.m.
Last updated: Feb 08, 2023 at 8:18 p.m.
Citation: See how to cite this resource
Sharing Status: Public
Views: 303
Downloads: 187
+1 Votes: Be the first one to 
 this.
Comments: No comments (yet)

Abstract

The estimation of the groundwater (GW) potential in irrigated areas is crucial for the sustainable management of water resources in order to ensure its sustainable use. This study was conducted in a selected area of the Chaj doab, Punjab, Pakistan, to quantify the impacts of the pumping and the recharge on the aquifer therein. To that end, a groundwater flow model (MODFLOW) and a groundwater recharge model (WetSpass) were coupled to assess the conditions of the aquifer. The model was calibrated manually on twelve-year data (2003-2014) against the observed groundwater levels, and it was validated with five-year data (2015-2019). Three main scenarios (divided into ten subscenarios) were simulated for the future prediction of the groundwater: Scenario-I (to assess the impact of the pumping if the prevailing conditions of the years from 2003 to 2019 were to continue until 2035); Scenario-II (to assess the impact of the pumping on the aquifer by increasing the pumping capacity by 25, 50, 75, and 100% for the coming 10 years); and Scenario-III (to assess the impact on the aquifer of the decrease in the average groundwater recharge from the river by 50% by following the same pumping trend). The Scenario-I results show that there would be an 18.1 m decrease in the groundwater table at the end of the year 2035. The Scenario-II results predict decreases in the water table by 2.0, 5.5, 9.8, and 14.3 m in the year 2029 as a result of increases in the pumping capacity of 25, 50, 75, and 100%, respectively. The results of Scenario-III show that, with the decrease in the recharge from the rainfall, there would be a 0.7 m decrease in the water table, and that, from open-water bodies, there would be a 2.4 m decrease in the water table. These results are very helpful for determining the recharge and discharge potential of the aquifer.

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Pakistan
North Latitude
30.3968°
East Longitude
73.5877°
South Latitude
29.8136°
West Longitude
72.3750°

Content

Additional Metadata

Name Value
DOI 10.3390/su14084421
Depth 107
Scale
Layers 3
Purpose
GroMoPo_ID 406
IsVerified True
Model Code MODFLOW
Model Link https://doi.org/10.3390/su14084421
Model Time 2013-2019
Model Year 2022
Model Authors Aslam, M; Arshad, M; Singh, VP; Shahid, MA
Model Country Pakistan
Data Available Report/paper only
Developer Email 2011ag2757@uaf.edu.pk; arsmrz@yahoo.com; vsingh@tamu.edu; muhammad.shahid@uaf.edu.pk
Dominant Geology Model focuses on multiple geologic materials
Developer Country Pakistan; USA
Publication Title Hydrological Modeling of Aquifer's Recharge and Discharge Potential by Coupling WetSpass and MODFLOW for the Chaj Doab, Pakistan
Original Developer No
Additional Information
Integration or Coupling Surface water;Water use
Evaluation or Calibration Static water levels
Geologic Data Availability No

How to Cite

GroMoPo, D. Kretschmer (2023). GroMoPo Metadata for Chaj Doab MODFLOW model, HydroShare, http://www.hydroshare.org/resource/b84751c69ad04f66ac4fb85ded99cc76

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/
CC-BY

Comments

There are currently no comments

New Comment

required