Agronomy Journal Journal of Natural Resources and Life Sciences Education
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Published online 3 May 2006
Published in Agron J 98:823-829 (2006)
DOI: 10.2134/agronj2005.0305
© 2006 American Society of Agronomy
677 S. Segoe Rd., Madison, WI 53711 USA
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Using Information about Spatial Variability to Improve Estimates of Total Soil Carbon

A. N. Kravchenkoa,*, G. P. Robertsonb, S. S. Snapb and A. J. M. Smuckera

a Dep. of Crop and Soil Sciences, Michigan State Univ., East Lansing, MI 48824-1325
b W.K. Kellogg Biological Station and Dep. of Crop and Soil Sciences, Michigan State Univ., Hickory Corners, MI 49060-9516


Figure 1
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Fig. 1. Example of soil sample locations (solid circles) overlaid with a simulated experiment in one of the studied field sites.

 

Figure 2
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Fig. 2. Example of sample variograms for total soil C from three of the studied field sites and the variogram models fitted to the sample variograms by restricted maximum likelihood method in PROC MIXED (SAS). Model parameters are shown in Table 1.

 

Figure 3
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Fig. 3. Relationships between the number of replications and the difference in total soil C (%) between the treatments that can be detected as statistically significant via F-test for treatment effects with power of 0.80 and {alpha} of 0.05 using standard randomized complete block design (RCBD) analysis and random field analysis with correlated errors based on plot data (SA1) analysis with spatial correlation ranges of 15, 25, and 35 m.

 





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