The authors present both laboratory and in situ data that support that the available residual friction angle ðfr9Þs on a presheared sliding plane depends on effective stress and not on aging. This discussion presents an alternate reason for why ðfr9Þs depends on effective stress. It involves the adsorbed water layer (AWL) in clays and may also help explain the aging behavior. The discusser recently published a paper (Schmertmann 2012), based on extensive experimental results, which presents new concepts for the Mohr-Coulomb (M-C) components of mobilized shear resistance in clay. Two of these components, denoted Ic and Ia, appear to relate to the behavior of the AWL; a viscous, plastic, Ic component that does not depend on the effective stress, and therefore, behaves as a M-C cohesion; and a second viscous, plastic, Ia component that depends linearly on the effective stress, and therefore, behaves as a M-C friction with an angle denoted fa9. Fig. 15 in Schmertmann (2012), presented herein as Fig. 1, shows, versus the plasticity index, a range of 7–19 for fr9 surrounding a range of 8– 14 for fa9. These fr9 come from a mixture of secant and tangent values. The authors’ Fig. 1 shows a measured laboratory and mobilized field secant ðfr9Þs range of 7–21 from approximately 75 data points in 16 references. The similarity in fr9 ranges in these two figures, and how they surround fa9 may provide more evidence of the importance of fa9 and AWL behavior in fr9. The authors do not include a residual cohesion in their paper. If residual strength behavior results from the AWL behavior, then the residual secant friction angle ðfr9Þs used by the authors should include both the Ic cohesion and the Ia friction. Including both components gives Eq. (1)
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