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Prediction of Near-Saturated Hydraulic Conductivity in Three Podzolic Boreal Forest Soils

M. Mecke, C.J. Westman and H. Ilvesniemi

Dep. of Forest Ecology, Univ. of Helsinki, P.O. Box 24, FIN-00014, Helsinki, Finland



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Fig. 1 The coefficient of the exponential K({psi}) relationship, {alpha}, plotted against the coarse textural fraction. The eluvial horizon measurements and the measurements of Site 3a are excluded

 



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Fig. 2 Near-saturated hydraulic conductivity K(-0.35) as predicted by Model 1, when all four horizons are included: (a) Model 1a, all four predictor variables are used; (b) Model 1b, only the best predictor variable is used. For example, regression equation of Model 1a is , where a, b, c, d, and e are the constants given by Table 4

 



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Fig. 3 Near-saturated hydraulic conductivity K(-0.35) as predicted by Model 2, when all horizons except upper illuvial horizon are included: (a) Model 2a, all four predictor variables are used, (b) Model 2b, only the best predictor variable is used

 



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Fig. 4 Near-saturated hydraulic conductivity K(-0.35) as predicted by Model 3, when only the parent soil measurements are included: (a) Model 3a, all four predictor variables are used, (b) Model 3b, only the best predictor variable is used

 





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