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Real part of the spectral domain, zero-offset three-dimensional GPR Green's function in the complex plane of the integration variable. This function is integrated to estimate the soil electromagnetic properties from the GPR data using full-waveform inverse modeling. The approach is applied at the Agrosphere Institute to map the soil hydrogeophysical properties at the field scale. See “Remote Estimation of the Hydraulic Properties of a Sand Using Full-Waveform Integrated Hydrogeophysical Inversion of Time-Lapse, Off-Ground GPR Data,” p. 743–754, by Sébastien Lambot, Evert Slob, Jan Rhebergen, Olga Lopera, Khan Zaib Jadoon, and Harry Vereecken, one of the articles in this issue's special section on the Agrosphere Institute.