Field mapping of wetting front using ground penetrating Radar under uniform and non-uniform wetting

dc.contributor.authorMimrose, DMSC
dc.contributor.authorGalagedara, LW
dc.contributor.authorParkin, GW
dc.date.accessioned2013-11-14T17:54:23Z
dc.date.available2013-11-14T17:54:23Z
dc.date.issued2013-11-14
dc.description.abstractThis research was carried out to develop 2D and 3D maps of a wetting front and to identify potential preferential flow areas using Ground Penetrating Radar (GPR). GPR grid data were collected during uniform and non-uniform wetting experiments. Maps were prepared for different depth profiles for each data set, collected at different time intervals after starting water application. The wetting front had reached a maximum depth of 0.45–0.50 m within 25 hours of continuous wetting based on 2D and 3D GPR images. In the uniform wetting experiments, potential preferential flow zones could be identified in 2D and 3D maps.en_US
dc.identifier.conferenceInternational Conference on Sustainable Built Environments 2010en_US
dc.identifier.emailmimrose124@gmail.comen_US
dc.identifier.emaillgalaged@pdn.ac.lken_US
dc.identifier.emailgparkin@uoguelph.caen_US
dc.identifier.placeEarl's Regency Hotel, Kandy.en_US
dc.identifier.proceedingSustainable Built Environmentsen_US
dc.identifier.urihttp://dl.lib.mrt.ac.lk/handle/123/9157
dc.identifier.year2010en_US
dc.language.isoenen_US
dc.subjectGround penetrating radaren_US
dc.subjectwetting fronten_US
dc.subjectpreferential flowen_US
dc.subjectwater contenten_US
dc.titleField mapping of wetting front using ground penetrating Radar under uniform and non-uniform wettingen_US
dc.typeConference-Full-texten_US

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