Published online 26 April 2005
Published in Vadose Zone J 4:240-254 (2005)
DOI: 10.2136/vzj2004.0070
© 2005 Soil Science Society of America
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Intercomparison of Flow and Transport Models Applied to Vertical Drainage in Cropped Lysimeters
M. Herbsta,*,
W. Fialkiewiczb,
T. Chenc,
T. Pütza,
D. Thiéryb,
C. Mouvetb,
G. Vachaudd and
H. Vereeckena
a Agrosphere Institute ICG-IV, Forschungszentrum Jülich GmbH, D-52425 Jülich, Germany
b Bureau de Recherches Geologiques et Minieres, BRGM, Avenue Claude Guillemin F 45060 Orleans Cedex 02, France
c ISRN\DPRE\SERLAB\LMODE, CEN Cadarache 13115 St Paul-Lez-Durance, France
d Laboratoire d'etude des Transferts en Hydrologie et Environnement, LTHE (UMR CNRS 5546, UJF, INPG, IRD), BP53, 38041, Grenoble CX 09, France

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Fig. 1. Measured atmospheric conditions and calculated reference evapotranspiration rates during the experimental period.
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Fig. 3. Cumulative measured and predicted actual evapotranspiration rates. Bars indicate standard deviations of the measurements.
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Fig. 4. Measured and predicted soil moisture contents at two depths. Bars indicate standard deviations of the measurements.
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Fig. 5. Cumulative measured and predicted drainage rates. Bars indicate standard deviations of the measurements.
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Fig. 6. Measured and predicted soil temperatures at 10 cm depth.
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Fig. 7. Measured and predicted methabenzthiazuron (MBT) residues (applied MBT = 100%) (a) 252 d and (b) 627 d after application.
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Fig. 8. Precipitation and measured and predicted accumulated mass of methabenzthiazuron (MBT) in the drainage water. MBT application was at t = 0.
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Copyright © 2005 by the Soil Science Society of America.