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GroMoPo Metadata for North Oman Mountains hardrock aquifer model


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Created: Apr 13, 2023 at 2:15 p.m.
Last updated: Apr 13, 2023 at 2:15 p.m.
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Abstract

This study aims at modeling groundwater flow using MODFLOW in a transboundary hardrock-alluvium aquifer, located in northwestern Oman. A three-dimensional stratigraphic model of the study area representing the vertical and spatial extent of four principal hydro-geologic units (specifically, the Hawasina, ophiolite, Tertiary and alluvium) was generated using data collected from hundreds drilled borehole logs. Layer elevations and materials for four layers grid cells were taken from the generated stratigraphic model in which the materials and elevations were inherited from the stratigraphic model that encompasses the cell. This process led to accurate grid so that the developed groundwater conceptual model was mapped to simulate the groundwater flow and to estimate groundwater balance components and sustainable groundwater extraction for the October 1996 to September 2013 period. Results show that the long-term lateral groundwater flux ranging from 4.23 to 11.69 Mm(3)/year, with an average of 5.67 Mm(3)/year, drains from the fractured eastern ophiolite mountains into the alluvial zone. Moreover, the long-term regional groundwater sustainable groundwater extraction is 18.09 Mm(3)/year for 17 years, while it is, respectively, estimated as 14.51, 16.31, and 36.00 Mm(3)/year for dry, normal, and wet climate periods based on standardized precipitation index (SPI) climate condition. Considering a total difference in groundwater levels between eastern and western points of the study area on the order of 228 m and a 12-year monthly calibration period (October 1996 to September 2008), a root mean squared error (RMSE) in predicted groundwater elevation of 2.71 m is considered reasonable for the study area characterized by remarkable geological and hydrogeological diversity. A quantitative assessment of the groundwater balance components and particularly sustainable groundwater extraction for the different hydrological period would help decision makers to better understand the water resources in the Al-Buraimi region. In addition, it would assist decision makers to improve existing strategies to enhance the decision making for future developments.

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Oman, United Arab Emirates
North Latitude
24.6330°
East Longitude
56.2330°
South Latitude
24.0330°
West Longitude
55.7330°

Content

Additional Metadata

Name Value
DOI 10.3390/w9030161
Depth 700 meters
Scale 1 001 - 10 000 km²
Layers 4
Purpose Groundwater resources
GroMoPo_ID 2025
IsVerified True
Model Code MODFLOW
Model Link https://doi.org/10.3390/w9030161
Model Time 1996-2013
Model Year 2017
Creator Email sachawruzzante@gmail.com
Model Country Oman, United Arab Emirates
Data Available Report/paper only
Developer Email az.izady@gmail.com; osman@squ.edu.om; atajoodavi@gmail.com; mingjie@squ.edu.om
Dominant Geology Model focuses on multiple geologic materials
Developer Country Oman; Iran
Publication Title Groundwater Modeling and Sustainability of a Transboundary Hardrock-Alluvium Aquifer in North Oman Mountains
Original Developer No
Additional Information N/A
Integration or Coupling None of the above
Evaluation or Calibration Dynamic water levels
Geologic Data Availability No

How to Cite

GroMoPo, S. Ruzzante (2023). GroMoPo Metadata for North Oman Mountains hardrock aquifer model, HydroShare, http://www.hydroshare.org/resource/0e41c882612348f0bb51d942830fedbc

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

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

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