Abstract:
The available analytical solutions for upconing of saltwater
interface are based upon many restrictive assumptions which may not
always be satisfied. In the present study, an attempt has been made to
develop a numerical model for simulation of saltwater transport
occurring in consequence of pumping water from a partially penetrating
well. The well is assumed to tap only the freshwater zone and saltwater
is assumed to occur below the well screen. The model, accounting for
both convective and diffusive components of saltwater transport, is
based upon a numerical solution of the differential equations governing
the pressure distribution and the mass transport in a two-dimensional
axi-symmetric flow domain. While calculating the pressure distribution,
the variation of the specific weight and dynamic viscosity of fluid due
to time and space variation of saltwater concentration is accounted for.
The pressure distribution is computed by the finite difference employing
iterative alternating direction implicit explicit (IADJ.E) scheme. To
avoid numerical dispersion, computation of the total saltwater transport
is accomplished in three stages. First, the convective transport is
computed by the method of characteristics. The necessary velocities are
calculated from the precomputed pressure distribution. Subsequently, the
diffusive transport is computed by the finite difference employing
iterative alternating direction implicit explicit (IADIE) scheme.
Finally, the two transports are integrated to get the total transport.
Thus, the proposed model basically simulates the vertical and
radial movement of the saltwater during and subsequent to the closure of
IV
pumping. Such a simulation leads to estimates of spatially and
temporally distributed saltwater concentration in the aquifer and
temporally distributed saltwater concentration in the pumped water.
Further, the fractional saltwater settlement [i.e., the fraction of
saltwater lifted (during the pumping), settling down to the initial
position of the interface] at different discrete times since the closure
of the pumpage may also be estimated.
The model has been implicitly validated by comparing its
response with Bear and