SSSAJ
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 29 March 2006
Published in Soil Sci Soc Am J 70:832-843 (2006)
DOI: 10.2136/sssaj2004.0391
© 2006 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Abstract Freely available
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
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 Google Scholar
Google Scholar
Right arrow Articles by Mamedov, A. I.
Right arrow Articles by Levy, G. J.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Mamedov, A. I.
Right arrow Articles by Levy, G. J.
Agricola
Right arrow Articles by Mamedov, A. I.
Right arrow Articles by Levy, G. J.
Related Collections
Right arrow Soil Erosion
Right arrow Structure and Properties
Right arrow Runoff

Antecedent Moisture Content and Aging Duration Effects on Seal Formation and Erosion in Smectitic Soils

A. I. Mamedova,*, C. Huangb and G. J. Levya

a Institute of Soil, Water and Environmental Sciences, Agricultural Research Organization (ARO), The Volcani Center, P.O. Box 6, Bet-Dagan 50-250, Israel. A.I. Mamedov is currently at the National Soil Erosion Research Lab., USDA-ARS-MWA, West Lafayette, IN, 47907
b National Soil Erosion Research Lab., USDA-ARS-MWA, West Lafayette, IN, 47907


Figure 1
View larger version (45K):

[in a new window]
 
Fig. 1. Moisture content at the upper 6 mm of the soil samples as a function of the amount of water added and aging duration. For each soil, the bar indicates a single confidence interval at P < 0.05.

 

Figure 2
View larger version (47K):

[in a new window]
 
Fig. 2. Matric potential, expressed in pF units, at the upper 6 mm of the soil samples as a function of aging duration and the amount of water added. For each soil at a given aging duration, the bar indicates a single confidence interval at P < 0.05.

 

Figure 3
View larger version (59K):

[in a new window]
 
Fig. 3. Calculated runoff volumes from the 60-mm rain storms for the different aging periods as a function of soil type and amount of water added. For a giving aging period and within a soil type, columns labeled with same letter are not significantly different at P < 0.05. Within a soil, columns from left to right represent AMC derived from 0, 1, 2, 3, 4, 6, 8, and 16 mm of water added.

 

Figure 4
View larger version (59K):

[in a new window]
 
Fig. 4. Measured total soil loss from the 60-mm rain storms for the different aging periods, as a function of soil type and amount of water added. For a giving aging period and within a soil type, columns labeled with same letter are not significantly different at P < 0.05. Within a soil, columns from left to right represent AMC derived from 0, 1, 2, 3, 4, 6, 8, and 16 mm of water added.

 

Figure 5
View larger version (29K):

[in a new window]
 
Fig. 5. Effect of AMC (expressed as pF) on (a) runoff and (b) soil loss in 3- to 7-day aging duration. Runoff and soil loss data were fitted to the pF data by a polynom of the fourth order (r2 > 0.90, P < 0.01 in all cases). Bars indicate the least significant differences at P < 0.05. Means are significantly different where bars do not overlap.

 

Figure 6
View larger version (16K):

[in a new window]
 
Fig. 6. Lowest measured soil loss from each soil (for the 2–4 mm of water added treatments) as a function of clay content for a given aging duration. Bars indicate two standard errors.

 

Figure 7
View larger version (16K):

[in a new window]
 
Fig. 7. Relative runoff or soil loss, expressed as the ratio of runoff or soil loss at a given aging duration to the runoff or soil loss at no aging (0.01 d). The ratios were calculated for the average runoff or soil loss data obtained from the 2, 3, and 4 mm of water added treatments. Bars indicate two standard errors.

 





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 © 2006 by the Soil Science Society of America.