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

Fig. 3.

Fig. 3

Temporal variability of near saturated and saturated soil hydraulic conductivity at different pressure heads. Statistical comparison indicates if changes between two consecutive measurement dates are significant at p < 0.05 (ns. non-significant, * significant at p < 0.05, ** significant at p < 0.01).