“…Over the past decades, GPR has been employed to resolve various geological and engineering issues, including, among others, soil water content measures (Galagedara, Parkin, & Redman, ; Grote, Anger, Kelly, Hubbard, & Rubin, ; Huisman & Bouten, ; Huisman, Sperl, Bouten, & Verstraten, ; van Overmeeren, Sariowan, & Gehrels, ; Weiler, Steenhuis, Boll, & Kung, ), soil moisture mapping at the field scale (Grote, Hubbard, & Rubin, ; Minet, Bogaert, Vanclooster, & Lambot, ; Weihermüller, Huisman, Lambot, Herbst, & Vereecken, ), and identification of near‐surface structures and seepage paths (Birken & Versteeg, ; Klenk, Jaumann, & Roth, ; Neal, ; Su, Xu, Geng, & Liang, ; Trinks, Wachsmuth, & Stümpel, ). Regarding the application of GPR in rock massifs, its main uses are related to the identification of major discontinuities and fractures, particularly in karst environments (Chamberlain, Sellers, Proctor, & Coard, ; Deparis, Garambois, & Hantz, ; Garcia‐Garcia, Valls‐Ayuso, Benlloch‐Marco, & Valcuende‐Paya, ; Grandjean & Gourry, ; Pueyo Anchuela, Casas‐Sainz, Soriano, & Pocoví‐Juan, ); for less clear features and structures, the contrast of GPR images along with direct observations allows calibration and validation of the results (Fernandes, Medeiros, Bezerra, Oliveira, & Cazarin, ; Longoni et al, ; Pipan, Forte, Guangyou, & Finetti, ).…”