SSSAJ Journal of Natural Resources and Life Sciences Education
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Published online 25 January 2008
Published in Soil Sci Soc Am J 72:412-423 (2008)
DOI: 10.2136/sssaj2006.0429
© 2008 Soil Science Society of America
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SOIL & WATER MANAGEMENT & CONSERVATION

Dynamics of Soil Surface Bulk Density: Role of Water Table Elevation and Rainfall Duration

B. Augearda,*, L. M. Bressonb, S. Assoulinec, C. Kaoa and M. Vauclind

a UR Cemagref, Hydrosystèmes et Bioprocédés, BP 44, 92163 Antony cedex, France
b UMR INRA/INAPG, Environnement et Grandes Cultures, 78850 Thiverval-Grignon, France
c Institute of Soil, Water and Environ. Sciences, Volcani Center, ARO, P.O.B. 6, Bet-Dagan 50250, Israel
d LTHE, UMR 5564 (CNRS, INPG, IRD, UJF), BP 53, 38041 Grenoble Cedex 9, France

* Corresponding author (benedicte.augeard{at}cemagref.fr).

Measurements of soil bulk density profiles combined with thin-section analysis have been suggested to assess the structural seedbed degradation caused by rainfall. The effects of water table elevation and rainfall duration on surface sealing and seedbed slumping were studied on a repacked silt loam soil. Two initial water table elevations (0.3 and 0.7 m below the soil surface) and three simulated rainfall durations (15, 30, and 40 min at 30.5 mm h–1 followed by 180 min at 7 mm h–1) were used. Seedbed bulk density profiles were generated using x-radiography of resin-impregnated soil slices. Macroporosity measurements using image analysis and thin-section observations showed that infilling of eroded particles in interaggregate voids and compaction of the infilled particles were the main sealing processes. Below the seal, the seedbed exhibited coalescence and welding of aggregates into larger units, which affected mainly macroporosity. A model of sealing, exponential decrease in bulk density with depth, and slumping, linear increase in bulk density with depth, adequately reproduced the measured bulk density profiles (regression RMSE range 0.057–0.106 Mg m–3). The change in surface bulk density increased with rainfall duration, whereas this factor did not significantly affect slumping. The highest initial water table elevation led to the highest soil surface and internal seedbed bulk densities. It was suggested that high values of soil water content led to a decrease in aggregate cohesion. Moreover, the number of wetting and drying cycles and the water content during these cycles were shown to increase the magnitude of slumping.

Abbreviations: HWT, high water table • LWT, low water table • RI, roughness index • UV, ultraviolet







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