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Published online 21 June 2006
Published in Soil Sci Soc Am J 70:1407-1414 (2006)
DOI: 10.2136/sssaj2005.0355
© 2006 Soil Science Society of America
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Organic Carbon Influences on Soil Particle Density and Rheological Properties

Humberto Blanco-Canquia,*, R. Lala, W. M. Postb, R. C. Izaurraldec and M. J. Shipitalod

a Carbon Management and Sequestration Center, FAES/OARDC, School of Natural Resources, The Ohio State Univ., 210 Kottman Hall, 2021 Coffey Rd., Columbus, OH 43210-1085
b Environmental Science Div., Oak Ridge National Lab., Oak Ridge, TN 37831
c Joint Global Change Research Inst., 8400 Baltimore Ave., Suite 201, College Park, MD 20740-2496
d USDA-ARS, North Appalachian Experimental Watershed, P.O. Box 488, Coshocton, OH 43812-0488


Figure 1
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Fig. 1. Mean soil particle density at three depths for moldboard plow (MP), no-till with no beef cattle manure (NT), no-till with beef cattle manure (NTm), pasture, and forest long-term management practices at the Northern Appalachian Experimental Watershed in Coshocton County, OH. The LSD bars at a given soil depth indicate the significance of particle density among the five management practices.

 

Figure 2
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Fig. 2. Mean soil organic C concentration at three depths for moldboard plow (MP), no-till with no beef cattle manure (NT), no-till with beef cattle manure (NTm), pasture, and forest long-term management practices at the Northern Appalachian Experimental Watershed in Coshocton County, OH. The LSD bars at a given soil depth indicate the significance of soil organic C concentration among the five management practices.

 

Figure 3
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Fig. 3. (A) Relationships of bulk and particle density of soil with SOC (soil organic carbon) concentration for the 0- to 10-cm depth and (B) depth distribution of bulk density under moldboard plow (MP), no-till with no beef cattle manure (NT), no-till with beef cattle manure (NTm), pasture, and forest long-term management practices at the Northern Appalachian Experimental Watershed in Coshocton County, OH. The LSD bars at a given soil depth indicate the significance of bulk density among the five management practices.

 

Figure 4
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Fig. 4. Total soil porosity using assumed (2.65 Mg m–3) and measured particle density for moldboard plow (MP), no-till with no beef cattle manure (NT), no-till with beef cattle manure (NTm), pasture, and forest long-term management practices at three depth intervals. Different letters within the same treatment indicate significant differences between the two porosities at the 0.05 probability level.

 

Figure 5
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Fig. 5. Soil water contents at the liquid limit (LL), plastic limit (PL), and plasticity index (PI) for three soil depths for moldboard plow (MP), no-till with no beef cattle manure (NT), no-till with beef cattle manure (NTm), pasture, and forest long-term management practices at the Northern Appalachian Experimental Watershed in Coshocton County, OH. The LSD bars at a given soil depth indicate the significance of LL, PL, and PI among the five management practices.

 

Figure 6
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Fig. 6. Liquid limit, plastic limit, and plasticity index as a function of soil organic carbon (SOC) concentration for the (A) 0- to-10-cm and (B) 10- to-20-cm soil depths across five long-term management practices at the Northern Appalachian Experimental Watershed in Coshocton County, OH. The r2 were all significant at the 0.001 probability level.

 





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