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Following a recently developed general framework for direct push system decomposition we analyze two different DC resistivity direct push probes with regard to their sensor interface.
Technical and experimental design of direct push probes follow often those of established borehole probes.
In near surface sedimentary exploration direct push technology has become popular for geophysical logging.
By using direct push sensor systems it is possible to measure in-situ parameters with high vertical resolution.
Most of the available direct push sensor systems are largely based on empirical testing and consecutively evaluated under field conditions.
Approaches suitable to identify specific characteristics and problems of direct push sensor systems have not been established, yet.
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In direct comparison the applied direct push-based Water Content Profiler proved to be a suitable alternative to neutron probe technology for measuring the vertical water content distribution.
For field evaluation direct push-profiling was performed at three different test sites under different hydrogeological settings and varying degree of sediment heterogeneity and compared with results obtained from gravimetric analysis of soil cores and neutron probe measurements.
Commonly applied tools for the investigation of vertical soil water content distribution in hydrogeological field investigations are: gravimetric laboratory analyses of soil samples, logging a cased borehole using a tool with a radioactive source (neutron probe), or yet less well established, direct push-based moisture sensor probes.
Temperature dissipation data was also compared to Direct-Push-derived high-resolution (hydro- geological data.
Current in-well or direct-push field measurement techniques allow for relatively quick determination of general conductivity profiles with depth.
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