Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...
This resource contains some files/folders that have non-preferred characters in their name. Show non-conforming files/folders.
This resource contains content types with files that need to be updated to match with metadata changes. Show content type files that need updating.
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 3.7 KB | |
Created: | Apr 13, 2023 at 2:15 p.m. | |
Last updated: | Apr 13, 2023 at 2:15 p.m. | |
Citation: | See how to cite this resource |
Sharing Status: | Public |
---|---|
Views: | 513 |
Downloads: | 163 |
+1 Votes: | Be the first one to this. |
Comments: | No comments (yet) |
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
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
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
Comments
There are currently no comments
New Comment