Agronomy Journal Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 1 January 1970
Published in Agron J 62:106-112 (1970)
© 1970 American Society of Agronomy
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Pierre, W. H.
Right arrow Articles by Birchett, J. R.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Pierre, W. H.
Right arrow Articles by Birchett, J. R.
Agricola
Right arrow Articles by Pierre, W. H.
Right arrow Articles by Birchett, J. R.

Cation-Anion Balance in Crops as a Factor in Determining the Effect of Nitrogen Fertilizers on Soil Acidity1

W. H. Pierre, John Meisinger and J. R. Birchett2

The quantitative effect of crops on the acidity produced in soils from nitrification of NH,NO3 fertilizer was determined by growing oats and. buckwheat in the greenhouse and finding the amounts of CaCO3 necessary to bring the soils back to their original pH. Three crops of each plant species were grown, and the plants were analyzed for total N, nitrate-N, and excess base. Determinations of pH were made both in 0.01 M CaCl2 and in H2O, with modifications to eliminate errors due to soluble salts.

The acidity developed from NH4NO3 in uncropped soil was almost equal to the theoretical amount that should be developed by nitrification. Without the removal of soluble salts erroneous values were obtained. The increase in acidity due to N4NO3 when oats was grown lower than the theoretical value in the absence of a crop by 27%, and the increase in acidity with buckwheat was higher than the theoretical value by 87%. Analyses of the crops showed that the deviations from the theoretical increase in soil acidity from NH4NO3 fertilizer was quantitatively explained by the numbers of chemical equivalents of N and excess bases taken up by the crops, excess base being defined as total cations (Ca++ Mg++, K+ and Na+) — total anions (C1-, SO4-, and H2PO4-).

Key Words: Excess base • Excess base-N ratios • Salt effect on pH • pH in 0.01 M CaCl2-


1 Journal Paper No. J-6319 of the Iowa Agricultural and Home Economics Experiment Station, Ames, Iowa 50010. Project 1761.

2 Professor of Agronomy, Student Assistant, and Graduate Assistant, respectively.

Received for publication July 26, 1969.





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Crop Science Vadose Zone Journal
Journal of Natural Resources
and Life Sciences Education
Soil Science Society of America Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 1970 by the American Society of Agronomy.