SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 56:1898-1903 (1992)
© 1992 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Bissonnais, Y. L.
Right arrow Articles by Singer, M. J.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Bissonnais, Y. L.
Right arrow Articles by Singer, M. J.
Agricola
Right arrow Articles by Bissonnais, Y. L.
Right arrow Articles by Singer, M. J.

Crusting, Runoff, and Erosion Response to Soil Water Content and Successive Rainfalls

Yves Le Bissonnais

Service d'Etude des Sols et de la Carte Pédologique de France and Institut National de la Recherche Agronomique, Centre d'Orleans 45160, Ardon, France

Michael J. Singer*

Dep. of Land, Air, and Water Resources, Univ. of California, Davis, CA 95616

*Corresponding author.

ABSTRACT

Soil crusts reduce the water infiltration rate and may induce the erosion process by increasing runoff. We investigated the effects of initial soil water content and successive rainfalls on soil crusting, subsequent runoff, and erosion. Surface samples of Capay silty clay loam (fine, montmorillonitic, thermic Typic Chromoxerert) and Solano silt loam (fine-loamy, mixed, thermic Typic Natrixeralf) were packed into 0.37-m2 plots inclined at 9% slopes and subjected to simulated rainfall applied at 40 mm h–1 as 3.2-mm-diam. drops falling 2.5 m. Three successive 1-h rainfalls were applied to initially air dried or prewetted soils. Water splash, runoff, soil splash, and wash materials were collected at 5-min intervals. Post-rainfall photographs of crusted soil surfaces provided additional morphological evidence to support conclusions drawn from quantitative data. Prewetting reduced crust development, runoff, and erosion and the differences remained significant even during the third rainfall. For the initially air dry soils, erosion rates and runoff reached steady state after 25 mm of rain during the first rainfall, and were the same for the second and third rainfalls. For prewetted soils, runoff and erosion were lower, did not reach steady state during the first event, and increased during each subsequent rainfall. The infiltration rate for initially air dry soils was 20 times lower than for prewetted soils after 40 mm of the first rainfall, and remained 10 and 2 times lower after the second and third rain, respectively. The crust was still not completely developed on prewetted soils after 120 mm of cumulative rainfall.

Received for publication October 17, 1991.


This article has been cited by other articles:


Home page
Soil Sci.Home page
B. Augeard, L. M. Bresson, S. Assouline, C. Kao, and M. Vauclin
Dynamics of Soil Surface Bulk Density: Role of Water Table Elevation and Rainfall Duration
Soil Sci. Soc. Am. J., January 25, 2008; 72(2): 412 - 423.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
A. I. Mamedov, C. Huang, and G. J. Levy
Antecedent Moisture Content and Aging Duration Effects on Seal Formation and Erosion in Smectitic Soils
Soil Sci. Soc. Am. J., March 29, 2006; 70(3): 832 - 843.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
P. I. A. Kinnell
Sediment Transport by Medium to Large Drops Impacting Flows at Subterminal Velocity
Soil Sci. Soc. Am. J., May 6, 2005; 69(3): 902 - 905.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
M. Lado, M. Ben-Hur, and I. Shainberg
Soil Wetting and Texture Effects on Aggregate Stability, Seal Formation, and Erosion
Soil Sci. Soc. Am. J., November 1, 2004; 68(6): 1992 - 1999.
[Abstract] [Full Text] [PDF]


Home page
Vadose Zone JHome page
S. Assouline
Rainfall-Induced Soil Surface Sealing: A Critical Review of Observations, Conceptual Models, and Solutions
Vadose Zone J., May 1, 2004; 3(2): 570 - 591.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
G. J. Levy and A. I. Mamedov
High-Energy-Moisture-Characteristic Aggregate Stability as a Predictor for Seal Formation
Soil Sci. Soc. Am. J., September 1, 2002; 66(5): 1603 - 1609.
[Abstract] [Full Text] [PDF]


Home page
J. Environ. Qual.Home page
A.I. Mamedov, I. Shainberg, and G.J. Levy
Irrigation with Effluents: Effects of Prewetting Rate and Clay Content on Runoff and Soil Loss
J. Environ. Qual., November 1, 2001; 30(6): 2149 - 2156.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
L. M. Bresson, C. Koch, Y. Le Bissonnais, E. Barriuso, and V. Lecomte
Soil Surface Structure Stabilization by Municipal Waste Compost Application
Soil Sci. Soc. Am. J., November 1, 2001; 65(6): 1804 - 1811.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 1992 by the Soil Science Society of America.