Quantitative high-resolution observations of soil water dynamics in a complicated architecture using time-lapse ground-penetrating radar

被引:29
作者
Klenk, P. [1 ]
Jaumann, S. [1 ]
Roth, K. [1 ]
机构
[1] Heidelberg Univ, Inst Environm Phys, D-69120 Heidelberg, Germany
关键词
WAVE-FORM INVERSION; FIELD-SCALE; HYDRAULIC CONDUCTIVITY; DOMAIN REFLECTOMETRY; PARAMETER-ESTIMATION; JOINT INVERSION; DISPERSIVE TE; ACTIVE LAYER; GPR; PERMITTIVITY;
D O I
10.5194/hess-19-1125-2015
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
High-resolution time-lapse ground-penetrating radar (GPR) observations of advancing and retreating water tables can yield a wealth of information about near-surface water content dynamics. In this study, we present and analyze a series of imbibition, drainage and infiltration experiments that have been carried out at our artificial ASSESS test site and observed with surface-based GPR. The test site features a complicated but known subsurface architecture constructed with three different kinds of sand. It allows the study of soil water dynamics with GPR under a wide range of different conditions. Here, we assess in particular (i) the feasibility of monitoring the dynamic shape of the capillary fringe reflection and (ii) the relative precision of monitoring soil water dynamics averaged over the whole vertical extent by evaluating the bottom reflection. The phenomenology of the GPR response of a dynamically changing capillary fringe is developed from a soil physical point of view. We then explain experimentally observed phenomena based on numerical simulations of both the water content dynamics and the expected GPR response.
引用
收藏
页码:1125 / 1139
页数:15
相关论文
共 56 条
[1]   Joint estimation of soil moisture profile and hydraulic parameters by ground- penetrating radar data assimilation with maximum likelihood ensemble filter [J].
Anh Phuong Tran ;
Vanclooster, Marnik ;
Zupanski, Milija ;
Lambot, Sebastien .
WATER RESOURCES RESEARCH, 2014, 50 (04) :3131-3146
[2]  
Annan AP, 2005, WTR SCI TEC LIBR, V50, P185
[3]   Effects of the transition zone above a water table on the reflection of GPR waves [J].
Bano, Maksim .
GEOPHYSICAL RESEARCH LETTERS, 2006, 33 (13)
[4]   The non-invasive characterization of pumping-induced dewatering using ground penetrating radar [J].
Bevan, MJ ;
Endres, AL ;
Rudolph, DL ;
Parkin, G .
JOURNAL OF HYDROLOGY, 2003, 281 (1-2) :55-69
[5]   HIGH DIELECTRIC-CONSTANT MICROWAVE PROBES FOR SENSING SOIL-MOISTURE [J].
BIRCHAK, JR ;
GARDNER, CG ;
HIPP, JE ;
VICTOR, JM .
PROCEEDINGS OF THE IEEE, 1974, 62 (01) :93-98
[6]   Potential of Wireless Sensor Networks for Measuring Soil Water Content Variability [J].
Bogena, H. R. ;
Herbst, M. ;
Huisman, J. A. ;
Rosenbaum, U. ;
Weuthen, A. ;
Vereecken, H. .
VADOSE ZONE JOURNAL, 2010, 9 (04) :1002-1013
[7]  
Bradford J, 2014, PROCEEDINGS OF THE 2014 15TH INTERNATIONAL CONFERENCE ON GROUND PENETRATING RADAR (GPR 2014), P232, DOI 10.1109/ICGPR.2014.6970420
[8]  
Brooks R. H., 1966, J. Irrig. Drain. Div, V92, DOI [10.1061/JRCEA4.0000425, DOI 10.1061/JRCEA4.0000425]
[9]  
Buchner JS, 2012, GEOPHYSICS, V77, pH45, DOI [10.1190/GEO2011-0467.1, 10.1190/geo2011-0467.1]
[10]   Coupled hydrogeophysical inversion of time-lapse surface GPR data to estimate hydraulic properties of a layered subsurface [J].
Busch, Sebastian ;
Weihermueller, Lutz ;
Huisman, Johan A. ;
Steelman, Colby M. ;
Endres, Anthony L. ;
Vereecken, Harry ;
van der Kruk, Jan .
WATER RESOURCES RESEARCH, 2013, 49 (12) :8480-8494