Studying GPR's direct and reflected waves
As the transmitter and receiver (Tx and Rx, respectively) are located in close proximity during a typical ground‐penetrating radar (GPR) survey, the powerful signal generated by the Tx and which is then recorded by the Rx at various time delays, can be saturated at early times (i.e., this is the dir...
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Veröffentlicht in: | Near surface geophysics (Online) 2024-04, Vol.22 (2), p.161-174 |
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