Analysis of the Groundwater flow can help to understand future water potential. This study has explored the predicted groundwater flow dynamics with climate change and anthropogenic stress in Hormat-Golina Sub-basin. Groundwater flow modeling in this Sub-basin has provided information about groundwater quantity as well as the quality aspect for decision-makers about groundwater accessibility. The initial head measured values before and after irrigation season has varied to a maximum of 0.8 m. The groundwater head level before and after irrigation season was varying from 9.3 m to 8.26 m in the Southern boundary. The groundwater head was obtained from 41.5 m to 38.83 m in the northwestern of the Sub-basin. The maximum drawdown depth had found to 0.27 m and 2.6 m before and after irrigated season around the pumped wells. The increased pumping rate with decreased recharge rate was replying to the groundwater head at the end of 2021 decreased by 2.81 m in the northwestern boundary of the Sub-basin as compared as using constant pumping rate with recharge rate. While decreased pumping with increased recharge rate was replying to the groundwater head at the end of 2021 has increased by 2.23 m in the northwestern boundary of the Sub-basin as compared as using constant pumping rate. The impacts of climate change and human pressure on groundwater begot as the threats in those supply wells. Decreased pumping with increased recharge rate was accomplishing to restore and protect the groundwater resources, which is the best option for groundwater restoration and monitoring.
| Published in | Hydrology (Volume 9, Issue 2) |
| DOI | 10.11648/j.hyd.20210902.13 |
| Page(s) | 48-55 |
| Creative Commons |
This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited. |
| Copyright |
Copyright © The Author(s), 2024. Published by Science Publishing Group |
Groundwater Head, Irrigation, Climate Change, Hormat-Golina, Ethiopia
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APA Style
Mengesha Tesfaw, Tewodros Assefa Nigussie, Sirak Tekleab. (2021). Analysis of Groundwater Flow Modelling: The Case of Hormat-golina Sub-basin, Golina Basin, Ethiopia. Hydrology, 9(2), 48-55. https://doi.org/10.11648/j.hyd.20210902.13
ACS Style
Mengesha Tesfaw; Tewodros Assefa Nigussie; Sirak Tekleab. Analysis of Groundwater Flow Modelling: The Case of Hormat-golina Sub-basin, Golina Basin, Ethiopia. Hydrology. 2021, 9(2), 48-55. doi: 10.11648/j.hyd.20210902.13
AMA Style
Mengesha Tesfaw, Tewodros Assefa Nigussie, Sirak Tekleab. Analysis of Groundwater Flow Modelling: The Case of Hormat-golina Sub-basin, Golina Basin, Ethiopia. Hydrology. 2021;9(2):48-55. doi: 10.11648/j.hyd.20210902.13
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Download@article{10.11648/j.hyd.20210902.13,
author = {Mengesha Tesfaw and Tewodros Assefa Nigussie and Sirak Tekleab},
title = {Analysis of Groundwater Flow Modelling: The Case of Hormat-golina Sub-basin, Golina Basin, Ethiopia},
journal = {Hydrology},
volume = {9},
number = {2},
pages = {48-55},
doi = {10.11648/j.hyd.20210902.13},
url = {https://doi.org/10.11648/j.hyd.20210902.13},
eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.hyd.20210902.13},
abstract = {Analysis of the Groundwater flow can help to understand future water potential. This study has explored the predicted groundwater flow dynamics with climate change and anthropogenic stress in Hormat-Golina Sub-basin. Groundwater flow modeling in this Sub-basin has provided information about groundwater quantity as well as the quality aspect for decision-makers about groundwater accessibility. The initial head measured values before and after irrigation season has varied to a maximum of 0.8 m. The groundwater head level before and after irrigation season was varying from 9.3 m to 8.26 m in the Southern boundary. The groundwater head was obtained from 41.5 m to 38.83 m in the northwestern of the Sub-basin. The maximum drawdown depth had found to 0.27 m and 2.6 m before and after irrigated season around the pumped wells. The increased pumping rate with decreased recharge rate was replying to the groundwater head at the end of 2021 decreased by 2.81 m in the northwestern boundary of the Sub-basin as compared as using constant pumping rate with recharge rate. While decreased pumping with increased recharge rate was replying to the groundwater head at the end of 2021 has increased by 2.23 m in the northwestern boundary of the Sub-basin as compared as using constant pumping rate. The impacts of climate change and human pressure on groundwater begot as the threats in those supply wells. Decreased pumping with increased recharge rate was accomplishing to restore and protect the groundwater resources, which is the best option for groundwater restoration and monitoring.},
year = {2021}
}
TY - JOUR T1 - Analysis of Groundwater Flow Modelling: The Case of Hormat-golina Sub-basin, Golina Basin, Ethiopia AU - Mengesha Tesfaw AU - Tewodros Assefa Nigussie AU - Sirak Tekleab Y1 - 2021/06/04 PY - 2021 N1 - https://doi.org/10.11648/j.hyd.20210902.13 DO - 10.11648/j.hyd.20210902.13 T2 - Hydrology JF - Hydrology JO - Hydrology SP - 48 EP - 55 PB - Science Publishing Group SN - 2330-7617 UR - https://doi.org/10.11648/j.hyd.20210902.13 AB - Analysis of the Groundwater flow can help to understand future water potential. This study has explored the predicted groundwater flow dynamics with climate change and anthropogenic stress in Hormat-Golina Sub-basin. Groundwater flow modeling in this Sub-basin has provided information about groundwater quantity as well as the quality aspect for decision-makers about groundwater accessibility. The initial head measured values before and after irrigation season has varied to a maximum of 0.8 m. The groundwater head level before and after irrigation season was varying from 9.3 m to 8.26 m in the Southern boundary. The groundwater head was obtained from 41.5 m to 38.83 m in the northwestern of the Sub-basin. The maximum drawdown depth had found to 0.27 m and 2.6 m before and after irrigated season around the pumped wells. The increased pumping rate with decreased recharge rate was replying to the groundwater head at the end of 2021 decreased by 2.81 m in the northwestern boundary of the Sub-basin as compared as using constant pumping rate with recharge rate. While decreased pumping with increased recharge rate was replying to the groundwater head at the end of 2021 has increased by 2.23 m in the northwestern boundary of the Sub-basin as compared as using constant pumping rate. The impacts of climate change and human pressure on groundwater begot as the threats in those supply wells. Decreased pumping with increased recharge rate was accomplishing to restore and protect the groundwater resources, which is the best option for groundwater restoration and monitoring. VL - 9 IS - 2 ER -
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