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Paper Number: 113
3D
Numerical Groundwater Flow Modeling in Kohat Sub Basin, Northwest
Himalayan Fold & Thrust Belt Pakistan
Majid Khan
Institute of Geology and Geophysics, Chinese Academy of Sciences,
100029, P.R. China
Email: majidktk.000@gmail.com
Abstract
Groundwater has emerged as an exceedingly important water resource
and its increasing demand in agriculture, domestic and industrial uses
ranks it as a resource of strategic importance. Pakistan is blessed with
extensive groundwater resource, which has been built due to direct
recharge from natural precipitation, river flow, and the continued
seepage from the conveyance system of canals, distributaries,
watercourses and application losses in the irrigated lands during the
last 90 years. The present and future groundwater availability and
exploitation has been evaluated in an intermountain basin (Kohat Sub
basin) of Northwest Himalayan Fold & Thrust belt Pakistan by
developing 3D Numerical Groundwater flow models. Numerical Groundwater
Flow Modeling is used to characterize complex hydrological systems and
to predict future availability of fresh water resources. To support the
study some geophysical, hydrological and metrological data of entire
basin including canals and river flow was used. The finite-difference
groundwater modeling program (MODFLOW) developed by USGS was used for
simulating the three-dimensional groundwater flow of the Kohat Basin to
investigate different water management strategies, the output of
modeling program resulted in groundwater flow pattern which closely
resembles the natural flow pattern in the study area. The litholgical
succession of alluvial cover in the study area is very heterogeneous,
consequently three continuous layers of coarse sand, gravel sand mixed
facies and boulder sand respectively were selected for conceptual model
construction. The hydraulic heads of from nine observation wells were
used as initial conditions for steady State simulation, the model
successfully calibrated with 95% confidence interval and 0.99
correlation coefficient. The steady state model show that under no
stress condition the groundwater is flowing from northeast and northwest
to southeastern parts of the study area. In order to understand the
impact of stress periods on groundwater, the transient simulation was
run which successfully generated the heads for the predicted year 2018.
The groundwater withdrawal exceed the recharge, consequently the result
shows that water table has been dropped by 25 meters, the continues
withdrawal of groundwater and mismanagement may lead to critical
condition regarding water availability in the study area. It is thus
recommended to maintain the safe yield in vulnerable zones e.ge.
Northeastern and southern parts of the study area. The groundwater is
almost fresh with good quality; the only precaution is SAFE YIELD.
Keywords: Numerical Modeling, Groundwater Flow,
Kohat basin, Groundwater, MODFLOW
Note: The 3D Numerical Groundwater flow
Models for the first time have been constructed in the study area, it
provided very productive results and submitted the predictions to
Provincial Water Development Authority to work on the proposed
strategies resulted from Modeling results. Hope this would be very
helpful in future water exploration and exploitation in Kohat Sub Basin
of Pakistan.