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Published online 1 May 2008
Published in Soil Sci Soc Am J 72:720-726 (2008)
DOI: 10.2136/sssaj2006.0296
© 2008 Soil Science Society of America
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Right arrow Soil pH
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Effects of Biological Nitrogen Reactions on Soil Lime Requirement Determined by Incubation

Min Liua, D. E. Kisselb,*, L. S. Sononb, M. L. Cabrerac and P. F. Vendrellb

a Kuo Testing Labs, Inc., 337 S. 1st Ave., Othello, WA 99344
b Agricultural and Environmental Services Labs, 2400 College Station Rd., Univ. of Georgia, Athens, GA 30602
c Dep. of Crop and Soil Sciences, 3111 Plant Sciences, Univ. of Georgia, Athens, GA 30602


Figure 1
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Fig. 1. Difference in pH in water between soil incubated with Ca(OH)2 and soil incubated with CaCO3 vs. time of incubation.

 

Figure 2
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Fig. 2. Difference in pH in water between the 3-d Ca(OH)2 and 60-d CaCO3 incubations vs. net H+.

 

Figure 3
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Fig. 3. Effects of initial electrical conductivity on pH depression by 0.01 mol L–1 CaCl2.

 

Figure 4
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Fig. 4. Difference between in pH in water and pH in 0.01 mol L–1 CaCl2 vs. electrical conductivity.

 

Figure 5
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Fig. 5. Difference in pH in water between the 3-d Ca(OH)2 and 60-d CaCO3 incubations vs. electrical conductivity after the 60-d CaCO3 incubation.

 





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The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2008 by the Soil Science Society of America.