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Soil and Crop Response to Variable-Rate Liming for Two Michigan Fields

F.J. Pierce and D.D. Warncke

Crop and Soil Sci. Dep., Michigan State Univ., East Lansing, MI 48824 USA



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Fig. 1 Soil pH and lime requirement maps for the Durand and Plainwell fields sampled June, 1993. The experimental area is delineated by a rectangle on each map and consisted of nine replications arranged in a three by three pattern

 


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Fig. 2 Interpolated maps of lime requirement for the Durand field derived from three regular grid sampling scales: (a) 30.5, (b) 61, and (c) 91.5 m

 


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Fig. 3 Scatterplots of lime requirement (LR) measured on experimental plots vs. LR predicted by interpolation of grid points at scales of 30.5, 61, and 91.5 m for fields in Durand and Plainwell, MI. Each point represents one replication of each treatment in each of nine blocks. The 1:1 line is shown

 


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Fig. 4 Temporal variation in soil pH as affected by lime treatment for fields in Durand and Plainwell, MI, for the 0- to 10- and 10- to 20-cm depths

 


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Fig. 5 Soybean yield response in 1997 to soil pH measured in December 1996 for fields in Durand and Plainwell, MI, and normalized yield response for the two fields combined. Data were fitted to a linear-plateau model

 


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Fig. 6 Response of soil pH to lime applied according to lime requirement (LR) for fields in Durand and Plainwell, MI, at the last soil sampling date in December 1996

 


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Fig. 7 Change in soil pH in the surface 10 cm of soil from the Durand field for incubation time in response to agricultural lime and granulated lime at five rates of lime application

 





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Journal of Natural Resources
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Vadose Zone Journal
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The Plant Genome
Copyright © 2000 by the Soil Science Society of America.