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

GroMoPo Metadata for SE Ghana crystalline aquifer 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 1.5 KB
Created: Feb 08, 2023 at 9:09 p.m.
Last updated: Feb 08, 2023 at 9:09 p.m.
Citation: See how to cite this resource
Sharing Status: Public
Views: 559
Downloads: 219
+1 Votes: Be the first one to 
 this.
Comments: No comments (yet)

Abstract

A conceptual groundwater flow model was developed for the crystalline aquifers in southeastern part of the Eastern region, Ghana. The objective was to determine approximate levels of groundwater recharge, estimate aquifer hydraulic parameters, and then test various scenarios of groundwater extraction under the current conditions of recharge. A steady state groundwater flow model has been calibrated against measured water levels of 19 wells in the area. The resulting recharge is estimated to range from 8.97 x 10(-5) m/d to 7.14 x 10(-4) m/d resulting in a basin wide average recharge of about 9.6% of total annual precipitation, which results in a basin wide quantitative recharge of about 2.4 million m(3)/d in the area. This compares to recharge estimated from the chloride mass balance of 7.6% of precipitation determined in this study. The general groundwater flow in the area has also been determined to conform to the general northeast-southwest structural grain of the country. The implication is that the general hydrogeology is controlled by post genetic structural entities imposed on the rocks to create ingresses for sufficient groundwater storage and transport. Calibrated aquifer hydraulic conductivities range between 0.99 m/d and over 19.4 m/d. There is a significant contribution of groundwater discharge to stream flow in the study area. Increasing groundwater extraction will have an effect on stream flow. This study finds that the current groundwater extraction levels represent only 0.17% of the annual recharge from precipitation, and that groundwater can sustain future increased groundwater demands from population growth and industrialization. (C) 2010 Elsevier Ltd. All rights reserved.

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
1 001 - 10 000 km sq Ghana
North Latitude
6.5000°
East Longitude
1.0000°
South Latitude
5.7500°
West Longitude
0.0000°

Content

Additional Metadata

Name Value
DOI 10.1016/j.jafrearsci.2010.10.005
Depth
Scale 1 001 - 10 000 km²
Layers 1
Purpose Groundwater resources
GroMoPo_ID 434
IsVerified True
Model Code MODFLOW
Model Link https://doi.org/10.1016/j.jafrearsci.2010.10.005
Model Time SS
Model Year 2011
Model Authors Yidana, SM; Ganyaglo, S; Banoeng-Yakubo, B; Akabzaa, T
Model Country Ghana
Data Available Report/paper only
Developer Email smyidana@ug.edu.gh
Dominant Geology Model focuses on multiple geologic materials
Developer Country Ghana
Publication Title A conceptual framework of groundwater flow in some crystalline aquifers in Southeastern Ghana
Original Developer No
Additional Information
Integration or Coupling None of the above
Evaluation or Calibration Static water levels
Geologic Data Availability No

How to Cite

GroMoPo, S. Ruzzante (2023). GroMoPo Metadata for SE Ghana crystalline aquifer model, HydroShare, http://www.hydroshare.org/resource/eeadceb91ccb4c5a901645acbdd9315a

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