Temporal Monitoring of the Soil Freeze-Thaw Cycles over a Snow-Covered Surface by Using Air-Launched Ground-Penetrating Radar

We tested an off-ground ground-penetrating radar (GPR) system at a fixed location over a bare agricultural field to monitor the soil freeze-thaw cycles over a snow-covered surface. The GPR system consisted of a monostatic horn antenna combined with a vector network analyzer, providing an ultra-wideb...

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Main Authors: Khan Zaib Jadoon, Lutz Weihermüller, Matthew F. McCabe, Davood Moghadas, Harry Vereecken, Sebastíen Lambot
Format: Article
Language:English
Published: MDPI AG 2015-09-01
Series:Remote Sensing
Subjects:
Online Access:http://www.mdpi.com/2072-4292/7/9/12041
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author Khan Zaib Jadoon
Lutz Weihermüller
Matthew F. McCabe
Davood Moghadas
Harry Vereecken
Sebastíen Lambot
author_facet Khan Zaib Jadoon
Lutz Weihermüller
Matthew F. McCabe
Davood Moghadas
Harry Vereecken
Sebastíen Lambot
author_sort Khan Zaib Jadoon
collection DOAJ
description We tested an off-ground ground-penetrating radar (GPR) system at a fixed location over a bare agricultural field to monitor the soil freeze-thaw cycles over a snow-covered surface. The GPR system consisted of a monostatic horn antenna combined with a vector network analyzer, providing an ultra-wideband stepped-frequency continuous-wave radar. An antenna calibration experiment was performed to filter antenna and back scattered effects from the raw GPR data. Near the GPR setup, sensors were installed in the soil to monitor the dynamics of soil temperature and dielectric permittivity at different depths. The soil permittivity was retrieved via inversion of time domain GPR data focused on the surface reflection. Significant effects of soil dynamics were observed in the time-lapse GPR, temperature and dielectric permittivity measurements. In particular, five freeze and thaw events were clearly detectable, indicating that the GPR signals respond to the contrast between the dielectric permittivity of frozen and thawed soil. The GPR-derived permittivity was in good agreement with sensor observations. Overall, the off-ground nature of the GPR system permits non-invasive time-lapse observation of the soil freeze-thaw dynamics without disturbing the structure of the snow cover. The proposed method shows promise for the real-time mapping and monitoring of the shallow frozen layer at the field scale.
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spelling doaj.art-1c00121bda0d46b390c7d41a33df00732022-12-21T18:35:24ZengMDPI AGRemote Sensing2072-42922015-09-0179120411205610.3390/rs70912041rs70912041Temporal Monitoring of the Soil Freeze-Thaw Cycles over a Snow-Covered Surface by Using Air-Launched Ground-Penetrating RadarKhan Zaib Jadoon0Lutz Weihermüller1Matthew F. McCabe2Davood Moghadas3Harry Vereecken4Sebastíen Lambot5Division of Biological and Environmental Sciences and Engineering, King Abdullah University of Science and Technology, 23955-6900 Thuwal, Saudi ArabiaAgrosphere (IBG-3), Forschungszentrum Jlich GmbH, 52425 Juelich, GermanyDivision of Biological and Environmental Sciences and Engineering, King Abdullah University of Science and Technology, 23955-6900 Thuwal, Saudi ArabiaFederal Institute for Geosciences and Natural Resources (BGR), Stilleweg 2, 30655 Hannover, GermanyAgrosphere (IBG-3), Forschungszentrum Jlich GmbH, 52425 Juelich, GermanyEarth and Life Institute, Universite Catholique de Louvain, Croix du Sud, 2 box L7.05.02, Louvain-la-Neuve B-1348, BelgiumWe tested an off-ground ground-penetrating radar (GPR) system at a fixed location over a bare agricultural field to monitor the soil freeze-thaw cycles over a snow-covered surface. The GPR system consisted of a monostatic horn antenna combined with a vector network analyzer, providing an ultra-wideband stepped-frequency continuous-wave radar. An antenna calibration experiment was performed to filter antenna and back scattered effects from the raw GPR data. Near the GPR setup, sensors were installed in the soil to monitor the dynamics of soil temperature and dielectric permittivity at different depths. The soil permittivity was retrieved via inversion of time domain GPR data focused on the surface reflection. Significant effects of soil dynamics were observed in the time-lapse GPR, temperature and dielectric permittivity measurements. In particular, five freeze and thaw events were clearly detectable, indicating that the GPR signals respond to the contrast between the dielectric permittivity of frozen and thawed soil. The GPR-derived permittivity was in good agreement with sensor observations. Overall, the off-ground nature of the GPR system permits non-invasive time-lapse observation of the soil freeze-thaw dynamics without disturbing the structure of the snow cover. The proposed method shows promise for the real-time mapping and monitoring of the shallow frozen layer at the field scale.http://www.mdpi.com/2072-4292/7/9/12041ground-penetrating radarfreeze-thaw cyclesseasonal snow coverinversion
spellingShingle Khan Zaib Jadoon
Lutz Weihermüller
Matthew F. McCabe
Davood Moghadas
Harry Vereecken
Sebastíen Lambot
Temporal Monitoring of the Soil Freeze-Thaw Cycles over a Snow-Covered Surface by Using Air-Launched Ground-Penetrating Radar
Remote Sensing
ground-penetrating radar
freeze-thaw cycles
seasonal snow cover
inversion
title Temporal Monitoring of the Soil Freeze-Thaw Cycles over a Snow-Covered Surface by Using Air-Launched Ground-Penetrating Radar
title_full Temporal Monitoring of the Soil Freeze-Thaw Cycles over a Snow-Covered Surface by Using Air-Launched Ground-Penetrating Radar
title_fullStr Temporal Monitoring of the Soil Freeze-Thaw Cycles over a Snow-Covered Surface by Using Air-Launched Ground-Penetrating Radar
title_full_unstemmed Temporal Monitoring of the Soil Freeze-Thaw Cycles over a Snow-Covered Surface by Using Air-Launched Ground-Penetrating Radar
title_short Temporal Monitoring of the Soil Freeze-Thaw Cycles over a Snow-Covered Surface by Using Air-Launched Ground-Penetrating Radar
title_sort temporal monitoring of the soil freeze thaw cycles over a snow covered surface by using air launched ground penetrating radar
topic ground-penetrating radar
freeze-thaw cycles
seasonal snow cover
inversion
url http://www.mdpi.com/2072-4292/7/9/12041
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