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Published online 8 June 2007
Published in Soil Sci Soc Am J 71:1095-1104 (2007)
DOI: 10.2136/sssaj2006.0156
© 2007 Soil Science Society of America
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Pore Shrinkage Dependency of Inorganic and Organic Soils on Wetting and Drying Cycles

X. Penga,*, R. Horna and A. Smuckerb

a Institute of Plant Nutrition and Soil Science, Christian-Albrechts Univ., Olshausenstrasse 40, 24118, Kiel, Germany
b Dep. of Crop and Soil Science, Michigan State Univ., East Lansing, MI 48824


Figure 1
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Fig. 1. Scanning electron micrograph features of the four investigated soils.

 

Figure 2
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Fig. 2. Changes in void ratio of the four soils on intensity, frequency, and sequence of wetting and drying cycles. Bars are the standard deviations. See Table 2 for treatment definitions.

 

Figure 3
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Fig. 3. Changes in moisture ratio of the four soils on intensity, frequency, and sequence of wetting and drying cycles. Bars are the standard deviations. See Table 2 for treatment definitions. See Table 2 for treatment definitions.

 

Figure 4
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Fig. 4. Distribution of large (>50 µm), medium (0.6–50 µm), and fine (<0.6 µm) pores of the four soils at saturation after wetting and drying cycles. Bars are the standard deviations. Different lowercase letters on the bars indicate significant difference of total pores between treatments at P < 0.05. See Table 2 for treatment definitions.

 

Figure 5
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Fig. 5. Coefficient of linear extensibility (COLE) of large (>50 µm), medium (0.6–50 µm), and fine (<0.6 µm) pores of the four soils after wetting and drying cycles. Bars are the standard deviations. Different lowercase letters on the bars indicate significant difference of total COLE between treatments at P < 0.05. See Table 2 for treatment definitions.

 

Figure 6
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Fig. 6. Shrinkage index of total large (>50 µm), medium (0.6–50 µm), and fine (<0.6 µm) pores of the four soils after wetting and drying cycles. Bars are the standard deviations. Different uppercase letters on the bars indicate significant difference between pore sizes at P < 0.05. Different lowercase letters on the bars indicate significant difference between treatments at P < 0.05. See Table 2 for treatment definitions.

 

Figure 7
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Fig. 7. The changes in the water potential vs. void ratio relationship of the four soils as a function of the intensity, frequency, and sequence of wetting and drying cycles. The whole dryness is composed of 0 to –1000 kPa water potential, air dryness for 2, 4, and 7 d, and oven dryness at 30, 60, and 105°C. Bars are the standard deviations. See Table 2 for treatment definitions.

 

Figure 8
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Fig. 8. Changes in the soil shrinkage curves of the four soils as a function of the intensity, frequency, and sequence of wetting and drying cycles. The dots are the lines fitted by Eq. [1]. See Table 2 for treatment definitions.

 





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