Abstract

Saturated hydraulic conductivity (Ks), among other soil hydraulic properties, is important and necessary in water and mass transport models and irrigation and drainage studies. Although this property can be measured directly, its measurement is difficult and very variable in space and time. Thus pedotransfer functions (PTFs) provide an alternative way to predict the Ks from easily available soil data. This study was done to predict the Ks in Khuzestan province, southwest Iran. Three Intelligence models including (radial basis function neural networks (RBFNN), multi layer perceptron neural networks (MLPNN)), adaptive neuro-fuzzy inference system (ANFIS) and multiple-linear regression (MLR) to predict the Ks were used. Input variable included sand, silt, and clay percents and bulk density. The total of 175 soil samples was divided into two groups as 130 for the training and 45 for the testing of PTFs. The results indicated that ANFIS and RBFNN are effective methods for Ks prediction and have better accuracy compared with the MLPNN and MLR models. The correlation between predicted and measured Ks values using ANFIS was better than artificial neural network (ANN). Mean square error values for ANFIS, ANN, and MLR were 0.005, 0.02, and 0.17, respectively, which shows that ANFIS model is a powerful tool and has better performance than ANN and MLR in prediction of Ks.

Highlights

  • Soil hydraulic properties such as saturated hydraulic conductivity (Ks) govern many soil hydrological processes; they are very important and even necessary in water and mass transport models and irrigation and drainage studies [1]

  • pedotransfer functions (PTFs) constructed by using artificial neural networks (ANN) have proven popular with many researchers

  • This paper presents the development and validation of PTFs for prediction of Ks from basic soil properties by using ANN and adaptive neurofuzzy inference system (ANFIS) models in Khuzestan province, southwest Iran

Read more

Summary

Introduction

Soil hydraulic properties such as saturated hydraulic conductivity (Ks) govern many soil hydrological processes; they are very important and even necessary in water and mass transport models and irrigation and drainage studies [1]. Direct measurement of soil hydraulic properties including Ks is costly and time-consuming and becomes impractical due to spatial and temporal variabilities when hydrologic predictions are needed for large areas. It requires sophisticated measurement devices and skilled operators [2]. “Pedotransfer function” was first introduced for empirical regression equations relating water and solute transport parameters to the basic soil properties that are available in soil survey [8].

Objectives
Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call