Abstract

Leachate from a landfill can flow down and contaminate groundwater. Mathematical models are often used to describe groundwater flow, which can help designers to identify an appropriate location for a landfill area. We focused on simulation of hydraulic head of groundwater under landfill construction in a rural area. We used a partial differential equation model called two-dimensional vertically-averaged groundwater flow model to explain groundwater volume, in particular, to explain the hydraulic head of the groundwater which strongly affected the groundwater quality. We applied two alternating direction explicit methods to the groundwater flow model under general boundary conditions and rates of change of boundary conditions to obtain an approximate hydraulic head of groundwater. An alternating direction explicit method for all types of boundaries is used to find approximate solutions. The traditional alternative direction explicit method was modified to form our modified alternative direction explicit method. The results of all method are closed. The traditional alternative direction explicit method and the modified alternative direction explicit method led to more accurate solutions than forward time centered space in heterogeneous aquifer, two methods ensured that a stable solution of all interior points can be obtained by using a fine grid spacing.

Highlights

  • Pollutants in groundwater can alter an aquatic ecosystem

  • Nitrate decreases the ability of blood cells to carry oxygen, resulting in oxygen deficiency in some body parts that can be linked to blue baby syndrome [1]

  • Salinity contamination in groundwater in a rice field near a marine shrimp aquaculture farm can lead to poor crop production [2]-[3]

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Summary

Introduction

Pollutants in groundwater can alter an aquatic ecosystem. A major groundwater deterioration problem is contamination of chemicals and heavy metals. Groundwater may become contaminated by leaching of nitrate from fertilizer on agricultural fields and waste dumps in rural and urban areas. Ground water systems can be modeled by using partial differential equations, usually numerically solved by finite difference and finite element methods. An explicit finite difference scheme for solving nonlinear time-dependent equations can be applied to linear equations. This scheme has been proven to be second order accurate in time and unconditionally stable for arbitrary time step size [10]. We introduce a two-dimensional verticallyaveraged groundwater flow model It can determine the hydraulic head of groundwater in the considered area.We have compared our numerical solution,forward time centered space and alternating direction explicit method for all types of boundaries is used to find approximate solutions in homogeneous and heterogeneous aquifer

A Two-Dimensional Vertically Averaged Groundwater Flow Model
Initial Conditions
Explicit finite Difference Techniques
Modified Alternating Direction Explicit Method
Simulation 1
Simulation 2
Simulation 3
Results and Discussion
Full Text
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