Abstract

Soil saturated hydraulic conductivity is considered one of the physical soil properties that is very important in modeling of water movement and environmental studies. This study aimed to compare the performance of Multi-Layer Perceptron (MLP) and Radial Basis Function (RBF) in neural networks for estimation of the soil saturated hydraulic conductivity. For this, the data of 27 drilled cased borehole permeameter with three kinds of geometry water flow through the soils and the soil texture properties were used as the input parameters for models. The effectiveness of neural networks to estimate the soil saturated hydraulic conductivity were calculated and compared based on mean squared error (MSE), root mean squared error (RMSE) and coefficient determination (R2). According to the above indicators, for all three types of drilled cased borehole permeameter surveyed in this study, the results show MLP neural networks had better performance than RBF neural networks in estimation of the soil saturated hydraulic conductivity and for wells with the horizontal, vertical and horizontal-vertical flow, which the amount of coefficient determination were respectively for all of them 0.94, 0.97 and 0.85.

Highlights

  • Water can move through soil as saturated flow, unsaturated flow, or vapor flow

  • The results showed that the Multi-Layer Perceptron (MLP) neural networks are able to estimate the saturated hydraulic conductivity with high accuracy

  • The data intended for Cased borehole permeameter with the horizontally, vertically and horizontally – vertically of flow, MLP and Radial Basis Function (RBF) neural network structure was formed

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Summary

Introduction

Water can move through soil as saturated flow, unsaturated flow, or vapor flow. Saturated flow takes place when the soil pores are completely filled (or saturated) with water. Saturated hydraulic conductivity describes the speed of movement of water through saturated soil, as well as evaluating and modeling of water, salts and transfer of pollutants to groundwater and environmental studies is widely used and very important. Having information about this parameter for understanding unsaturated zone and development of scientific management in maintaining agricultural productivity and reducing the negative environmental impacts is necessary (Nosrati Karizak et al, 1391, Kurvar et al, 1983, Rinoldzo and Top, 2008). In order to estimate the saturated hydraulic conductivity, numerical solution of the equations that is presented by Philip and modified by Reynolds is difficult and time consuming (Asadollahzadeh, 2013)

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