Predicting soil infiltration rate using Artificial Neural Network

A. Ekhmaj
{"title":"Predicting soil infiltration rate using Artificial Neural Network","authors":"A. Ekhmaj","doi":"10.1109/ICEEA.2010.5596107","DOIUrl":null,"url":null,"abstract":"The infiltration rate is an important parameter in soil, hydrological, ecological and agricultural studies. It plays the main role as the input parameter in models for water flow and solute transport in the vadose zone. In this study, Multilayer Artificial Neural Network “ANN” using the backpropagation algorithm was selected to estimate the steady infiltration rate covering different types of Libyan soils. The activation function was selected LOGSIG in the middle and exit layers. The input data were the percentage of sand, silt and clay, bulk density, saturated hydraulic conductivity and the volumetric water content in soil at −10 kPa). The performance of the ANN models was evaluated against a set of data that never seen by the model during the training phase. Multivariable linear regression model (MLR) based on the percentage of silt, saturated hydraulic conductivity and volumetric water content in soil at −10 kPa was also developed to determine infiltration rate for evaluation purpose. The results obtained in this study showed a good agreement between the measured data and the ANN simulated. The values of mean absolute error and root mean square error were slightly smaller in ANN steady infiltration rate model compared to the developed Multivariable linear regression model to estimate the infiltration rate. Although the results of these comparisons encourage the using ANN in practice, it would be valuable to have large local soil database from many different sites, in order to make a stronger assessment of the ANN models.","PeriodicalId":262661,"journal":{"name":"2010 International Conference on Environmental Engineering and Applications","volume":"11 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2010-10-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"7","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"2010 International Conference on Environmental Engineering and Applications","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/ICEEA.2010.5596107","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 7

Abstract

The infiltration rate is an important parameter in soil, hydrological, ecological and agricultural studies. It plays the main role as the input parameter in models for water flow and solute transport in the vadose zone. In this study, Multilayer Artificial Neural Network “ANN” using the backpropagation algorithm was selected to estimate the steady infiltration rate covering different types of Libyan soils. The activation function was selected LOGSIG in the middle and exit layers. The input data were the percentage of sand, silt and clay, bulk density, saturated hydraulic conductivity and the volumetric water content in soil at −10 kPa). The performance of the ANN models was evaluated against a set of data that never seen by the model during the training phase. Multivariable linear regression model (MLR) based on the percentage of silt, saturated hydraulic conductivity and volumetric water content in soil at −10 kPa was also developed to determine infiltration rate for evaluation purpose. The results obtained in this study showed a good agreement between the measured data and the ANN simulated. The values of mean absolute error and root mean square error were slightly smaller in ANN steady infiltration rate model compared to the developed Multivariable linear regression model to estimate the infiltration rate. Although the results of these comparisons encourage the using ANN in practice, it would be valuable to have large local soil database from many different sites, in order to make a stronger assessment of the ANN models.
利用人工神经网络预测土壤入渗速率
入渗速率是土壤、水文、生态和农业研究中的一个重要参数。在气包带水流和溶质输运模型中,它作为输入参数起主要作用。在本研究中,采用反向传播算法的多层人工神经网络(ANN)来估计不同类型利比亚土壤的稳定入渗速率。在中间层和出口层选择LOGSIG激活函数。输入数据为- 10 kPa时土中砂、粉、粘土的百分比、容重、饱和导水率和体积含水量。人工神经网络模型的性能是根据一组模型在训练阶段从未见过的数据来评估的。此外,还建立了基于- 10 kPa时土壤中淤泥百分比、饱和水力导率和体积含水量的多变量线性回归模型(MLR),以确定入渗率。研究结果表明,实测数据与人工神经网络模拟结果吻合较好。与建立的多元线性回归模型相比,人工神经网络稳定入渗率模型的平均绝对误差和均方根误差略小。虽然这些比较的结果鼓励在实践中使用人工神经网络,但为了对人工神经网络模型进行更有力的评估,拥有来自许多不同地点的大型本地土壤数据库将是有价值的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信