Published online 26 May 2006
Published in Vadose Zone J 5:628-640 (2006)
DOI: 10.2136/vzj2005.0061
© 2006 Soil Science Society of America
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Estimation of the Unsaturated Hydraulic Conductivity of Peat Soils
Laboratory versus Field Data
K. Schwärzela,*,
J.
im
nekb,
H. Stoffregenc,
G. Wessolekc and
M. Th. van Genuchtend
a Institute of Soil Science and Site Ecology, Univ. of Technology, Dresden, Germany
b Dep. of Environmental Sciences, Univ. of California, Riverside, CA 92521 USA
c Institute of Ecology, Dep. of Soil Science and Soil Protection, Technical Univ. of Berlin, Germany
d USDA-ARS, George E. Brown, Jr. Salinity Lab., Riverside, CA 92521, USA

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Fig. 1. Schematic of the potential root water uptake distribution function.
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Fig. 2. Effect of tensiometer measurement precision on calculated unsaturated hydraulic conductivities.
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Fig. 4. Measured (open circles) and fitted (dashed lines) pressure heads (left) and water contents (right) for the lysimeter experiments without (top) and with (bottom) plants.
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Fig. 5. Hydraulic conductivity (left) and water retention (right) functions of the peat soil as determined from the lysimeter experiments using inverse parameter estimation and direct methods.
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Fig. 6. Observed (circles) and predicted (lines) pressure heads (left) and water contents (right) for the additional evaporation experiment using a lysimeter with plants. The different simulation scenarios are explained in Table 3.
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Copyright © 2006 by the Soil Science Society of America.