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Published online 27 April 2006
Published in Vadose Zone J 5:554-563 (2006)
DOI: 10.2136/vzj2005.0083
© 2006 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Modeling the Relationship between Soil Bulk Density and the Water Retention Curve

S. Assouline*

Institute of Soil, Water and Environmental Sciences, A.R.O., the Volcani Center, P.O.B. 6, Bet Dagan 50250, Israel

Figure 1
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Fig. 1. The relationship between relative {alpha} and relative {rho} values. The solid and open circles represent the calibration and validation data, respectively. The dashed lines represent the 95% confidence limits of the fitted curve (Eq. [12]) (solid line) to the calibration data.

 

Figure 2
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Fig. 2. Plot of the power {omega} in Eq. [13] for each soil of the calibration data set vs. the corresponding silt/clay content ratio (solid circles) and the fitted expression (Eq. [14]) (solid line). The dashed lines represent the 95% confidence limits of the fitted curve; the open circles represent the validation data.

 

Figure 3
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Fig. 3. The relationship between the relative {psi}a and {rho} values. The solid and open circles represent the calibration and the validation data, respectively. The dashed lines represent the 95% confidence limits of the fitted curve (Eq. [15]) (solid line) to the calibration data.

 

Figure 4
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Fig. 4. Plot of the relationship between {lambda}, the pore size distribution index in Eq. [9], and {varepsilon}, the coefficient of variation characterizing the WRC (Eq. [4]). The "+" symbols represent the calibration data (Assouline, 2005). The dashed lines indicate the 95% confidence limits of the fitted curve (Eq. [16]) (solid line) to these data. The solid and open circles represent the calibration and the validation data in this study, respectively.

 

Figure 5
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Fig. 5. Reproduced WRCs (solid line) for different compaction levels of Columbia sandy loam and Touchet silt loam soils of the calibration data set, using Eq. [1] (top) and Eq. [9] (bottom), and the corresponding measured data (solid circles). The open circles and dashed line represent the soil at its initial bulk density, {rho}.

 

Figure 6
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Fig. 6. Predicted WRCs (solid line) of the mechanically compacted sandy loam soil of the validation data set using (a) Eq. [1] and (b) Eq. [9] compared with the corresponding measured data (solid circles). The open circles and dashed line represent the soils at their initial bulk density {rho}.

 

Figure 7
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Fig. 7. Predicted WRCs (solid line) of the untilled soils of the validation data set at {rho}c using (a) Eq. [1] and (b) Eq. [9], and the corresponding measured data (solid circles). The open circles and dashed line represent the tilled soils at {rho}.

 

Figure 8
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Fig. 8. Plot of the modulus of rupture, s, as a function of the silt/clay content ratio for the data set of Ibanga et al. (1980) (solid circles) and the fitted expression (Eq. [17]) (solid line). The dashed line represents the 95% confidence limits of the fitted curve.

 

Figure 9
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Fig. 9. (a) Pore size distributions for the uncompacted (dashed lines) and compacted (solid lines) sandy loam soil, derived from the WRC expressions in Eq. [1] and Eq. [9] and shown in Fig. (6). (b) Differences between the pore size distributions for the compacted and uncompacted sandy loam soil, presented in (a), for the WRC expressions in Eq. [1] (thicker line) and Eq. [9] (thinner line).

 





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