{"title":"Surface Ground-penetrating Radar monitoring of water infiltration inside a ring infiltrometer","authors":"E. Léger, A. Saintenoy","doi":"10.1109/ICGPR.2012.6254948","DOIUrl":null,"url":null,"abstract":"In this study, we test the use of a surface Ground-penetrating Radar (GPR) for monitoring the water infiltration using a single ring infiltrometer similar to the Muntz apparatus [1]. We performed an experiment in a natural Fontainebleau sand, with 1600 MHz antennae, using a 60-cm diameter metallic ring partially buried down to 10 cm. During the infiltration of a 5-cm layer of water and the following drainage, GPR traces are acquired every 5 s from a static position inside the ring. We performed gravimetric measurements on several soil samples, evaluated the retention curve function using a laboratory hanging water column and used hydrodynamical and electromagnetic simulations to help with the GPR data interpretation.","PeriodicalId":443640,"journal":{"name":"2012 14th International Conference on Ground Penetrating Radar (GPR)","volume":"625 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2012-06-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"2012 14th International Conference on Ground Penetrating Radar (GPR)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/ICGPR.2012.6254948","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 4
Abstract
In this study, we test the use of a surface Ground-penetrating Radar (GPR) for monitoring the water infiltration using a single ring infiltrometer similar to the Muntz apparatus [1]. We performed an experiment in a natural Fontainebleau sand, with 1600 MHz antennae, using a 60-cm diameter metallic ring partially buried down to 10 cm. During the infiltration of a 5-cm layer of water and the following drainage, GPR traces are acquired every 5 s from a static position inside the ring. We performed gravimetric measurements on several soil samples, evaluated the retention curve function using a laboratory hanging water column and used hydrodynamical and electromagnetic simulations to help with the GPR data interpretation.