“…Thus, the functional form can be written as q sc,i q sc;i ¼ f ðq s;i ; P c ; d a ; C u ; u c ; u sh ; g d ; g w ; Dg s ; UCS 0 Þ (9) where C u and u c ¼ cohesion and angle of internal friction for clay constituent of sediment mixture at optimum moisture content and g d ¼ its dry density, u sh ¼ angle of repose/internal friction of cohesionless constituent sediment present in the mixture. The parameters P c , C u , u c , u sh , Dg s , d a can be expressed into dimensionless form as (Ansari et al 2002(Ansari et al , 2003)…”