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. 2013 Aug;204-205:120–129. doi: 10.1016/j.geoderma.2013.04.015

Table 6.

Best predictor among environmental driving forces for the temporal change in soil hydraulic property parameters (r2 coefficient of determination, p significance of regression model, positive or negative sign in brackets indicates direction of influence).

Δproperty Best predictor (slope) r2 p
Δk(h) h = 0 cm Wet–dry cycle intensity (+) 0.43 0.03*
Δk(h) h = 0.5 cm Wet–dry cycle intensity (+) 0.54 0.01*
Δk(h) h = 2.5 cm Wet–dry cycle intensity (+) 0.37 0.05*
Δk(h) h = 7 cm Moisture trend (−) 0.21 0.15ns
Δk(h) h = 10 cm Moisture trend (−) 0.22 0.14ns
Δε Wet–dry cycle intensity (+) 0.44 0.03*
Δrm Wet–dry cycle intensity (+) 0.55 < 0.01**
Δσ Wet–dry cycle frequency (−) 0.59 0.01**
Δϕ Rainfall intensity (+) 0.46 0.04*

K(h) hydraulic conductivity, ε effective macroporostiy, rm median pore radius, σ pore radius standard deviation, ϕ total porosity.