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

GroMoPo Metadata for North Sinai 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 4:19 p.m.
Last updated: Feb 08, 2023 at 4:20 p.m.
Citation: See how to cite this resource
Sharing Status: Public
Views: 441
Downloads: 213
+1 Votes: Be the first one to 
 this.
Comments: No comments (yet)

Abstract

The management of coastal aquifers requires careful planning of withdrawal strategies for control and remediation of saltwater intrusion. Over exploitation of groundwater in coastal aquifers may result in intrusion of saltwater. Prediction and control of future saltwater distribution in coastal aquifer may be possible by simulating the processes with utilizing mathematical models. The groundwater resources in North Sinai area are affected by salt water up-coming due to over-pumping phenomenon beside seawater intrusion. The objective of this study was to apply mathematical modeling techniques for water resource management in salt-affected ecosystems. The study area is located in the northern coastal zone of Sinai Peninsula of Egypt and covers about 1750 km(2). The methodological approach to simulate the groundwater flow is based on the mathematical modeling techniques with applying 3-D finite element software (FEFLOW model). Three management scenarios are applied to predict the drawdown of groundwater levels under different extraction rates and seawater intrusion phenomenon. In addition, the methodology of seawater intrusion study and calibration was based on applying two-dimensional finite element simulation (SWI) code. The results of ground-water flow simulation show optimum groundwater extractions 26 x 10(6) m(3)/year from the cultivated areas. Moreover, simulation results indicate that the seawater/freshwater interface will migrate, after 15 years, at the distance of 5.5 km landward from its initial position if the present groundwater production policy (19 x 10(6) m(3)/year) continues operating in the area. To conserve the Quaternary Aquifer in North Sinai coastal Area (QANSA) storage for longer time, it is recommended to reduce the number of the pumping wells (<300 wells) as well as the initial and running time (does not exceed 10 h), and to achieve the objective of implementing the developing policy without any increase (500 m(3)/day/well). It is highly recommended to carry out geophysical exploration study and to construct monitoring network to verify the results of the applied model.

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Egypt
North Latitude
31.2547°
East Longitude
33.8158°
South Latitude
30.7298°
West Longitude
32.3577°

Content

Additional Metadata

Name Value
DOI 10.1134/S0097807815040053
Depth
Scale 1 001 - 10 000 km²
Layers 2
Purpose Groundwater resources;Salt water intrusion
GroMoPo_ID 347
IsVerified True
Model Code Feflow;SWI
Model Link https://doi.org/10.1134/S0097807815040053
Model Time
Model Year 2015
Model Authors Gad, MI; Khalaf, S
Model Country Egypt
Data Available Report/paper only
Developer Email drgad@yahoo.com; samykhalaf2005@yahoo.com
Dominant Geology Model focuses on multiple geologic materials
Developer Country Egypt
Publication Title Management of Groundwater Resources in Arid Areas Case Study: North Sinai, Egypt
Original Developer No
Additional Information
Integration or Coupling Solute transport
Evaluation or Calibration Dynamic water levels;Groundwater chemistry
Geologic Data Availability No

How to Cite

GroMoPo, K. Compare (2023). GroMoPo Metadata for North Sinai model, HydroShare, http://www.hydroshare.org/resource/d0f0e4653549493b8aa0cc7e38de0017

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