“…The anchor uplift capacity is derived from the equilibrium of a rigid soil body delineated by a given failure surface. At shallow depths, the failure surface is a soil wedge reaching the surface, whose boundary may be assumed to be a straight line, either vertical or inclined, (Meyerhof and Adams 1968, Ghaly et al 1991, Giampa et al 2017 or a log-spiral (Murray and Geddes 1987, Saeedy 1987, Hanna et al 2007 propagating from the plate to the soil surface ( Figure 1Figure 1). At greater depths, a flow around mechanism has been proposed, consisting of a deep wedge that does not reach the ground surface (Meyerhof andAdams 1968, Ghaly et al 1991).…”