Abstract

Soil erosion induced by rainfall is a critical problem in many regions in the world, particularly in tropical areas where the annual rainfall amount often exceeds 2000 mm. Predicting soil erosion is a challenging task, subjecting to variation of soil characteristics, slope, vegetation cover, land management, and weather condition. Conventional models based on the mechanism of soil erosion processes generally provide good results but are time-consuming due to calibration and validation. The goal of this study is to develop a machine learning model based on support vector machine (SVM) for soil erosion prediction. The SVM serves as the main prediction machinery establishing a nonlinear function that maps considered influencing factors to accurate predictions. In addition, in order to improve the accuracy of the model, the history-based adaptive differential evolution with linear population size reduction and population-wide inertia term (L-SHADE-PWI) is employed to find an optimal set of parameters for SVM. Thus, the proposed method, named L-SHADE-PWI-SVM, is an integration of machine learning and metaheuristic optimization. For the purpose of training and testing the method, a dataset consisting of 236 samples of soil erosion in Northwest Vietnam is collected with 10 influencing factors. The training set includes 90% of the original dataset; the rest of the dataset is reserved for assessing the generalization capability of the model. The experimental results indicate that the newly developed L-SHADE-PWI-SVM method is a competitive soil erosion predictor with superior performance statistics. Most importantly, L-SHADE-PWI-SVM can achieve a high classification accuracy rate of 92%, which is much better than that of backpropagation artificial neural network (87%) and radial basis function artificial neural network (78%).

Highlights

  • Soil erosion induced by water is the main culprit of the degradation of upland and mountain ecosystems [1]. e erosion process poses a threat to the capacity of the land to provide ecosystem services that are needed to reach the Sustainable Development Goal (SDG) target 15.3 [2]

  • Erefore, the current study aims at extending the body of knowledge by establishing soil erosion prediction models for tropical hilly regions based on an integration of the history-based adaptive differential evolution with linear population size reduction and population-wide inertia term (L-SHADE-PWI) metaheuristic and the support vector machine pattern classification method

  • Since the size of the collected dataset is moderate, the training/testing data ratio is selected to be 9/1 [110]. is means that 90% of the original dataset is used for model construction; the rest of the dataset is reserved for the model testing phase. e testing set is employed as novel data instance to verify the generalization of the constructed L-SHADE-PWI-support vector machine (SVM)

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Summary

Introduction

Soil erosion induced by water is the main culprit of the degradation of upland and mountain ecosystems [1]. e erosion process poses a threat to the capacity of the land to provide ecosystem services that are needed to reach the Sustainable Development Goal (SDG) target 15.3 [2]. Ere are many factors affecting erosion magnitude, namely, climate, soil type, soil structure, vegetation, and cropping on top and especially land management [5]. In tropical areas, such as Northwest Vietnam, soil erosion potential is high due to heavy rainfall and is currently accelerating under maize monocropping in the uplands [6, 7]. Many attempts have been tested worldwide: contour ploughing or contour farming using stone, wood, or vegetation barriers/ hedgerow; cover crop; minimum tillage or zero tillage; and mulching Such measures can be effective in different geographic and climatic conditions under various soil characteristics and land management systems. Land management is crucial in controlling erosion [11, 13,14,15,16]

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