Fig. 2
From: Investigation into the PSD characteristics of internally unstable soils susceptible to suffosion

F-H/F curve of soil T-0 by Moffat, et al.7. H is defined as the weight fraction of particles ranging between d to 4d.
From: Investigation into the PSD characteristics of internally unstable soils susceptible to suffosion
F-H/F curve of soil T-0 by Moffat, et al.7. H is defined as the weight fraction of particles ranging between d to 4d.