Abstract

Study regionSixteen different sites from two provinces (Lorestan and Illam) in the western part of Iran were considered for the field data measurement of cumulative infiltration, infiltration rate, and other effective variables that affect infiltration process. Study focusSoil infiltration is recognized as a fundamental process of the hydrologic cycle affecting surface runoff, soil erosion, and groundwater recharge. Hence, accurate prediction of the infiltration process is one of the most important tasks in hydrological science. As direct measurement is difficult and costly, and empirical models are inaccurate, the current study proposed a standalone, and optimized deep learning algorithm of a convolutional neural network (CNN) using gray wolf optimization (GWO), a genetic algorithm (GA), and an independent component analysis (ICA) for cumulative infiltration and infiltration rate prediction. First, 154 raw datasets were collected including the time of measuring; sand, clay, and silt percent; bulk density; soil moisture percent; infiltration rate; and cumulative infiltration using field survey. Next, 70 % of the dataset were used for model building and the remaining 30 % was used for model validation. Then, based on the correlation coefficient between input variables and outputs, different input combinations were constructed. Finally, the prediction power of each developed algorithm was evaluated using different visually-based (scatter plot, box plot and Taylor diagram) and quantitatively-based [root mean square error (RMSE), mean absolute error (MAE), the Nash-Sutcliffe efficiency (NSE), and percentage of bias (PBIAS)] metrics. New Hydrological Insights for the RegionFinding revealed that the time of measurement is more important for cumulative infiltration, while soil characteristics (i.e. silt content) are more significant in infiltration rate prediction. This shows that in the study area, silt parameter, which is the dominant constituent parameter, can control infiltration process more effectively. Effectiveness of the variables in the present study, in the order of importance are time, silt, clay, moisture content, sand, and bulk density. This can be related to the fact that most of study area is rangeland and thus, overgrazing leads to compaction of the silt soil that can lead to a slow infiltration process. Soil moisture content and bulk density are not highly effective in our study because these two factors do not significantly change across the study area. Findings demonstrated that the optimum input variable combination, is the one in which all input variables are considered. The results illustrated that CNN algorithms have a very high performance, while a metaheuristic algorithm enhanced the performance of a standalone CNN algorithm (from 7% to 28 %). The results also showed that a CNN-GWO algorithm outperformed the other algorithms, followed by CNN-ICA, CNN-GA, and CNN for both cumulative infiltration and infiltration rate prediction. All developed algorithms underestimated cumulative infiltration, while overestimating infiltration rates.

Highlights

  • The soil-water infiltration process plays a fundamental role in hydrology, pedology, hydrogeology, irrigation, and drainage systems (Kale and Sahoo, 2011; Mahapatra et al, 2020; Ghumman et al, 2018a)

  • The results showed that a convolutional neural network (CNN)-gray wolf optimization (GWO) algorithm outperformed the other algorithms, followed by CNNICA, CNN-genetic algorithm (GA), and CNN for both cumulative infiltration and infiltration rate prediction

  • Total amount of water that soil strata are able to absorb from rainfall or irrigation in a given time is considered as a cumulative infiltration (F(t)); the velocity of the water entering into the soil in a given period of time is defined as the infiltration rate; (f(t)) and the velocity of water entering into the soil in a specific amount of time is defined as an instantaneous infiltration rate (Hooshyar and Wang, 2016; Mahmood and Latif, 2003)

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Summary

Introduction

The soil-water infiltration process plays a fundamental role in hydrology, pedology, hydrogeology, irrigation, and drainage systems (Kale and Sahoo, 2011; Mahapatra et al, 2020; Ghumman et al, 2018a). The rate of water infiltration into soil is controlled by several factors such as the initial moisture conditions of the ground’s surface; rainfall in­ tensity; soil and water temperature; biological activities in the soil column; soil texture, porosity, and compactness; and surface cover conditions (Angelaki et al, 2013; Ma et al, 2015; Hooshyar and Wang, 2016). The movement of chemical contaminants through soil and into groundwater is mainly controlled by the water infiltration process and overall watershed management plans (Angelaki et al, 2004; Mahapatra et al, 2020). Quantifying the infiltration process is important in watershed management

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