“…-Determination of the wave propagation time to a known interface using single-offset surface GPR (Grote et al, 2003;Lunt et al, 2005;van Overmeeren et al, 1997;Weiler et al, 1998) -Detection of the velocity-dependent reflecting hyperbola of a buried object using single-offset surface GPR along a transect (Vellidis et al, 1990;Windsor et al, 2005) -Extraction of stacking velocity fields from multi-offset radar soundings at a fixed central location (common midpoint method) (Garambois et al, 2002;Greaves et al, 1996) -Determination of the ground-wave velocity for surface water content retrieval using multi-and single-offset surface GPR (Chanzy et al, 1996;Du and Rummel, 1994;Galagedara et al, 2003Galagedara et al, , 2005aGrote et al, 2003;Huisman et al, 2001Huisman et al, , 2002) -Determination of the surface reflection coefficient using single-offset offground GPR (Chanzy et al, 1996;Redman et al, 2002;Or, 2003, 2004) -Determination of the two-dimensional spatial distribution of water between boreholes using transmission tomography (Alumbaugh et al, 2002;Binley et al, 2001;Rucker and Ferre, 2005;Zhou et al, 2001) In particular, time-lapse GPR measurements have recently permitted to monitor soil water dynamics between boreholes and infer the soil hydraulic properties governing water flow (Binley et al, 2001;Cassiani and Binley, 2005;Kowalsky et al, 2005;Linde et al, 2006;Rucker and Ferré, 2004;Tsoflias et al, 2001). GPR can also be used to monitor remediation amendments and processes .…”