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Published online 27 February 2006
Published in Soil Sci Soc Am J 70:620-630 (2006)
DOI: 10.2136/sssaj2004.0355
© 2006 Soil Science Society of America
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Surface-Soil Properties and Water Contents across Two Watersheds with Contrasting Tillage Histories

M. D. Tomer*, C. A. Cambardella, D. E. James and T. B. Moorman

USDA-ARS, National Soil Tilth Lab., 2150 Pammel Dr. Ames, IA50011


Figure 1
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Fig. 1. Map of watersheds 1 and 3 (CW1 and RW3), showing sampling locations. Excluded areas include roadways, buffers, waterways, and areas in different ownership or management.

 

Figure 2
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Fig. 2. Plots of terrain characteristics at sampling locations in CW1 and RW3 show the two watersheds are similar in terms of topographic exposure (A) and soil wetness (B).

 

Figure 3
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Fig. 3. Plots of slope and organic carbon (OC) in watersheds CW1 and RW3, with regression equations fit to the data. The greater amount of OC in RW3 caused a significant difference in intercept values.

 

Figure 4
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Fig. 4. Plot of average surface-soil {theta} measured on four dates in CW1 and RW3 versus the F ratio, which indicates the significance of the difference between watersheds after landscape-position effects were removed. RW3 had significantly larger {theta} on dates when {theta} exceeded 33%.

 

Figure 5
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Fig. 5. Plots of organic C (OC) and soil water contents on two dates in watersheds CW1 and RW3. Correlation coefficients were consistently significant in RW3 (P < 0.01), and consistently nonsignificant in CW1 (P > 0.05).

 

Figure 6
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Fig. 6. Soil water retention curves for the conventionally tilled (CW1) and ridge-tilled (RW3) watersheds, as estimated by pedotransfer functions. Watershed means for {theta}s and b (Eq. [1], Table 8) were used to plot these curves. Plotted points place the mean {theta} values for four dates of monitoring in both watersheds, indicating soil water potentials were similar between watersheds. Inset: predicted differences in {theta} between watersheds are greatest when soils are wet, and similar to those detected (Table 5).

 





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