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Fig. 8. (a) Log–log relationship of I/( ${theta}$ _s – ${theta}$ _i)^1/2 and the pore-size distribution index ( ${lambda}$ ) for the 11 textural-class mean soils at 20 cm h^–1 rainfall intensity and an initial pressure head of –1500 kPa; (b) Log-log relationship of I/( ${theta}$ _s– ${theta}$ _i)^1/2 and the pore-size distribution index ( ${lambda}$ ) for the 11 textural-class mean soils at 2.5 cm h^–1 rainfall intensity and an initial pressure head of –1500 kPa.