An Integrated Hydrogeophysical Approach for Unsaturated Zone Monitoring Using Time Domain Reflectometry, Electrical Resistivity Tomography and Ground Penetrating Radar

被引:4
作者
Papadopoulos, Alexandros [1 ]
Apostolopoulos, George [1 ]
Kallioras, Andreas [1 ]
机构
[1] Natl Tech Univ Athens, Sch Min & Met Engn, Athens 15772, Greece
关键词
infiltration experiment; vadose zone hydrology; soil moisture; TDR; geophysics; ERT; GPR; water movement; 3-D monitoring; time-lapse measurements; SOIL-WATER CONTENT; VADOSE ZONE; BOREHOLE RADAR; ELECTROMAGNETIC DETERMINATION; MOISTURE-CONTENT; SPATIOTEMPORAL DYNAMICS; HYDRAULIC PARAMETERS; PREFERENTIAL FLOW; SPATIAL VARIATION; SINGLE-RING;
D O I
10.3390/w16182559
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Continuous measurements of soil moisture in the deeper parts of the unsaturated zone remain an important challenge. This study examines the development of an integrated system for the continuous and 3-D monitoring of the vadose zone processes in a cost- and energy-efficient way. This system comprises TDR, ERT and GPR geophysical techniques. Their capacities to adequately image subsurface moisture changes with continuous and time-lapse measurements are assessed during an artificial infiltration experiment conducted in a characteristic urban site with anthropogenic fills and much compaction. A 3-D array was designed for each method to expand the information of a single TDR probe and obtain a broader image of the subsurface. Custom spatial TDR probes installed in boreholes made with a percussion drilling instrument were used for soil moisture measurements. Moisture profiles along the probes were estimated with a numerical one-dimensional inversion model and a standard calibration equation. High conductivity water used during all infiltration tests led to the detection of the flow by all techniques. Preferential flow was present throughout the experiment and imaged sufficiently by all methods. Overall, the integrated approach conceals each method's weaknesses and provides a reliable 3-D view of the subsurface. The results suggest that this approach can be used to monitor the unsaturated zone at even greater depths.
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页数:34
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