2018
DOI: 10.3390/rs10040639
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Application of Ground Penetrating Radar Supported by Mineralogical-Geochemical Methods for Mapping Unroofed Cave Sediments

Abstract: Ground penetrating radar (GPR) using a special unshielded 50 MHz Rough Terrain Antenna (RTA) in combination with a shielded 250 MHz antenna was used to study the capability of this geophysical method for detecting cave sediments. Allochthonous cave sediments found in the study area of Lanski vrh (W Slovenia) are now exposed on the karst surface in the so-called "unroofed caves" due to a general lowering of the surface (denudation of carbonate rocks) and can provide valuable evidence of the karst development. I… Show more

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Cited by 9 publications
(10 citation statements)
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“…The result of the time-lapse GPR for WF A′ in Fig. 3d represents that the average moisture contents ratio of sandstone (0–8 m) and clay (0–9 m) in the mining production stage are the smallest, which are 4.89% and 19.58%, respectively, while the ratio in the post-mining stage are basically the same as the unmined stage 15 . This GPR conclusion agrees with the electrical prospecting and seismic exploration results from the water loss that occur in near surface soil loosening caused by the mining effect.…”
Section: Resultsmentioning
confidence: 92%
See 1 more Smart Citation
“…The result of the time-lapse GPR for WF A′ in Fig. 3d represents that the average moisture contents ratio of sandstone (0–8 m) and clay (0–9 m) in the mining production stage are the smallest, which are 4.89% and 19.58%, respectively, while the ratio in the post-mining stage are basically the same as the unmined stage 15 . This GPR conclusion agrees with the electrical prospecting and seismic exploration results from the water loss that occur in near surface soil loosening caused by the mining effect.…”
Section: Resultsmentioning
confidence: 92%
“…GPR uses electromagnetic radiation to detect the reflected signals from the changes of the material properties, the voids and the cracks in the subsurface. The principle of GPR is similar to the seismology, except GPR methods implement electromagnetic energy rather than acoustic energy 14,15 ,Where V is the electromagnetic wave velocity. C is the velocity of electromagnetic wave propagation in vacuum.…”
Section: Methodsmentioning
confidence: 99%
“…The degree of weathering can be quantified by CIA, which is sensitive to the removal of alkalis such as calcium, sodium, and potassium from feldspars (Nesbiitt and Young, 1982). τ reflects chemical gains and losses during weathering based on the elemental concentrations of mobile and immobile elements in weathered and unweathered material (e.g., Brimhall et al, 1985;Chadwick et al, 1990); ε strain in a regolith is based on the density ρ (g cm −3 ) and immobile element concentrations of the weathered regolith in comparison to the unweathered bedrock indicating volumetric gain or loss (Brimhall and Dietrich, 1987).…”
Section: Data Compilationmentioning
confidence: 99%
“…Despite the accurate results produced from studies on karst cavities conducted using either geophysical [17][18][19][20] or remote sensing [21][22][23][24] methods, the fusion of the two techniques results in advantages in the acquisition, processing, and interpretation of geophysical data. Collecting spatial information on electrodes and surveyed points can particularly enhance sinkhole research.…”
Section: Introductionmentioning
confidence: 99%