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Published online 18 July 2005
Published in Vadose Zone J 4:573-586 (2005)
DOI: 10.2136/vzj2004.0152
© 2005 Soil Science Society of America
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Water and Solute Transport in a Cultivated Silt Loam Soil

1. Field Observations

Y. Coqueta,*, C. Coutadeura, C. Labata, P. Vachiera, M. Th. van Genuchtenc, J. Roger-Estradeb and J. Simunekd

a UMR INRA/INAPG Environment and Arable Crops, Institut National de la Recherche Agronomique/Institut National Agronomique Paris-Grignon, B.P. 01, 78850 Thiverval-Grignon, France
b UMR INRA/INAPG Agronomy, Institut National de la Recherche Agronomique/Institut National Agronomique Paris-Grignon, B.P. 01, 78850 Thiverval-Grignon, France
c USDA-ARS, George E. Brown, Jr. Salinity Lab., 450 West Big Springs Road, Riverside, CA 92507
d Dep. of Environmental Sciences, Univ. of California, Riverside, CA 92521



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Fig. 1. Soil profiles showing the partitioning of the tilled layer. Compacted {Delta} soil is delineated by solid white lines. Boundaries between the seedbed and the plow layer are indicated by a solid black line. Accumulations of organic matter residues are surrounded by dotted white lines. (A) Soil profile that was sampled for bromide. (B) Soil profile where time domain reflectometry (TDR) probes and tensiometers were installed. Note that the bending of the pictures is due to uncorrected parallax effects and not to actual topography.

 


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Fig. 2. (a) Locations of time domain reflectometry (TDR) probes (large circles) and tensiometers (small squares) within the soil profile. The enlarged pictures show the position of the TDR probes and tensiometers in relation to the structure of the plow layer. Solid white lines delineate compacted {Delta} soil as well as the boundary between the seedbed and the plow layer. Accumulations of organic matter residues are delineated by dotted white lines. (b) Locations of the samples taken from the soil for bromide measurements.

 


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Fig. 3. Vertical cross-section showing the installation of the time domain reflectometry (TDR) probes and tensiometers. The cross-section is perpendicular to the main direction of the installation trench and parallel to the moving direction of the farm machinery.

 


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Fig. 4. Time domain reflectometry (TDR) probe responses to infiltration.

 


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Fig. 5. Tensiometer responses to infiltration.

 


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Fig. 6. Water redistribution within the soil profile as recorded with time domain reflectometry (TDR) probes. Vertical bars mark end of infiltration.

 


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Fig. 7. Water redistribution within the soil profile as recorded with tensiometers. Vertical bars mark end of infiltration.

 


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Fig. 8. Observed bromide concentrations within the soil profile in terms of (a) point values, and (b) an interpolated map of concentrations. Enlargements are shown at the bottom of the figure.

 


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Fig. 9. Average bromide concentration profiles (a) under the left wheel track, (b) between the wheel tracks, and (c) under the right wheel track. Fitted analytical solutions of the one dimensional advection–dispersion equation are shown as solid black lines. Fitted values of soil dispersivity ({lambda}) are also indicated.

 





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