TY - JOUR
T1 - Sustainable groundwater management in an arid hardrock-alluvium Al-Fara aquifer, Oman
AU - Izady, A.
AU - Abdalla, O.
AU - Amerjeed, M.
AU - Chen, M.
AU - Al-Maktoumi, A.
AU - Kacimov, A. R.
PY - 2018/12/1
Y1 - 2018/12/1
N2 - Wadi Al-Fara catchment, located at the northwest of Oman, represents one
of the most promising areas for the sustainable agricultural and urban
developments. Groundwater resources have been substantially
overexploited to provide irrigation, industrial and domestic demands
leading to a dramatic decline of the water table in the coastal zone of
the catchment. This situation has compelled the initiation of
comprehensive mitigation strategies and tools for the sustainable
groundwater resources.
Understanding of the aquifer conditions and groundwater resources
availability are crucial steps towards their proper management.
Groundwater numerical modeling is an important tool to achieve the
stated steps. A three-dimensional stratigraphic model of the study area
representing the vertical and spatial extent of four principal
hydrogeological units was generated using data collected from 57 drilled
borehole logs. Layer elevations and materials for six 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 an accurate grid so that the
developed conceptual model was mapped to simulate the groundwater
dynamics from October 1993 to September 2013. A triad (stress period,
time step, and time unit) was specified as (monthly, monthly, and
daily), respectively. A regular mesh and a block centered finite
difference grid with 0.125 km2 cells (500×500 m) with a
total of 150 rows, 97 columns and 6 layers were considered.
Simulations showed a long-term water balance deficit as the abstraction
(51 Mm³/yr) exceeds natural recharge (31 Mm³/yr). Recharge
flux from the highland to the coastal zone is a major contributor (12
Mm³/yr) to water resources in the coastal plain, sustaining the
hydrological system along the southern margin by flow from the storage
in the adjoining highland-fractured aquifers.
The calibrated and validated model was used to conduct long-term
simulations (horizon 2013-2033) to examine the impact of four management
scenarios on the groundwater balance and groundwater level:
- Scenario 1: Evaluate the current aquifer depletion with no
interventions to 2033
- Scenario 2: Evaluate the aquifer condition with no recharge
- Scenario 3: Evaluate reduction of the current abstraction to achieve
the equilibrium condition
- Scenario 4: Evaluate aquifer's response to increase by 30% the pumping
rate in the future to cover the growing water demands
The results revealed that further development of the aquifer will result
in a serious imbalance between inflows and outflows leading to a
progressive rate of sea water intrusion and decline in the water table.
AB - Wadi Al-Fara catchment, located at the northwest of Oman, represents one
of the most promising areas for the sustainable agricultural and urban
developments. Groundwater resources have been substantially
overexploited to provide irrigation, industrial and domestic demands
leading to a dramatic decline of the water table in the coastal zone of
the catchment. This situation has compelled the initiation of
comprehensive mitigation strategies and tools for the sustainable
groundwater resources.
Understanding of the aquifer conditions and groundwater resources
availability are crucial steps towards their proper management.
Groundwater numerical modeling is an important tool to achieve the
stated steps. A three-dimensional stratigraphic model of the study area
representing the vertical and spatial extent of four principal
hydrogeological units was generated using data collected from 57 drilled
borehole logs. Layer elevations and materials for six 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 an accurate grid so that the
developed conceptual model was mapped to simulate the groundwater
dynamics from October 1993 to September 2013. A triad (stress period,
time step, and time unit) was specified as (monthly, monthly, and
daily), respectively. A regular mesh and a block centered finite
difference grid with 0.125 km2 cells (500×500 m) with a
total of 150 rows, 97 columns and 6 layers were considered.
Simulations showed a long-term water balance deficit as the abstraction
(51 Mm³/yr) exceeds natural recharge (31 Mm³/yr). Recharge
flux from the highland to the coastal zone is a major contributor (12
Mm³/yr) to water resources in the coastal plain, sustaining the
hydrological system along the southern margin by flow from the storage
in the adjoining highland-fractured aquifers.
The calibrated and validated model was used to conduct long-term
simulations (horizon 2013-2033) to examine the impact of four management
scenarios on the groundwater balance and groundwater level:
- Scenario 1: Evaluate the current aquifer depletion with no
interventions to 2033
- Scenario 2: Evaluate the aquifer condition with no recharge
- Scenario 3: Evaluate reduction of the current abstraction to achieve
the equilibrium condition
- Scenario 4: Evaluate aquifer's response to increase by 30% the pumping
rate in the future to cover the growing water demands
The results revealed that further development of the aquifer will result
in a serious imbalance between inflows and outflows leading to a
progressive rate of sea water intrusion and decline in the water table.
KW - 1812 Drought
KW - HYDROLOGYDE: 1829 Groundwater hydrology
KW - HYDROLOGYDE: 1880 Water management
KW - HYDROLOGYDE: 6309 Decision making under uncertainty
KW - POLICY SCIENCES
M3 - Article
VL - 34
JO - American Geophysical Union, Fall Meeting 2018
JF - American Geophysical Union, Fall Meeting 2018
ER -