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Published online 11 January 2008
Published in Soil Sci Soc Am J 72:25-32 (2008)
DOI: 10.2136/sssaj2006.0232
© 2008 Soil Science Society of America
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Scaling Soil Water Characteristics of Golf Course and Athletic Field Sands from Particle-Size Distribution

Lalit M. Aryaa,*, Daniel C. Bowmanb, Bir B. Thapab and D. Keith Casselc

a 770 El Caballo Dr., Oceanside, CA 92057
b Crop Science Dep., North Carolina State Univ., Raleigh, NC 27695
c Soil Science Dep., North Carolina State Univ., Raleigh, NC 27695


Figure 1
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Fig. 1. Conceptual representation of the structure in the ith particle-size fraction, assembled in the form of a cube: (a) natural state of packing, (b) cubic, close-packed, consisting of uniform-size spherical particles, and (c) an enlarged subsection of the cross-sectional area of (b). The value of Li(c) in (b) can be estimated as follows: bulk volume of the assemblage = (2Rini1/3)3 = 8Ri3ni; solid volume of ni particles = (4{pi}Ri3ni)/3; pore volume in assemblage = 8Ri3ni – (4{pi}Ri3ni)/3; Area ABCD = 4Ri2; area (a + b + c + d) = 4(0.25{pi}Ri2) = {pi}Ri2; cross-sectional area of a single pore = 0.858Ri2. Therefore, if the total pore volume is represented by a single cylindrical pore, the total pore length, Li(c) is 3.811Ri3ni/0.858Ri2 = 4.44Rini. For variable definitions, see the Appendix.

 

Figure 2
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Fig. 2. Relationship between log ni{alpha}i vs. logni and logLi(n) vs. logLi(c) for Commercial sand 2.

 

Figure 3
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Fig. 3. Relationship between (a) log ni{alpha}i vs. logni for sands with no clay or silt, (b) log ni{alpha}i vs. logni for sands with minor amounts of clay and silt, (c) logLi(n) vs. logLi(c) for sands with no clay or silt, and (d) logLi(n) vs. logLi(c) for sands with minor amounts of clay and silt. Note: Each figure represents pooled data for seven sand materials.

 

Figure 4
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Fig. 4. Experimental and predicted soil water characteristic for Bunker sand: (a) best-fit parameters, (b) Parameters a, b (Eq. [9]) and c, d (Eq. [11]) altered by +10% of their best-fit values, (c) Parameters a, b and c, d altered by –10% of their best-fit values, and (d) best-fit mean parameters for the sand materials with no clay or silt.

 

Figure 5
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Fig. 5. Comparison of predicted pressure heads using Eq. [9] and [11].

 





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