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 September 1968
Published in Agron J 60:493-495 (1968)
© 1968 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 Stevenson, C. K.
Right arrow Articles by Bates, T. E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Stevenson, C. K.
Right arrow Articles by Bates, T. E.
Agricola
Right arrow Articles by Stevenson, C. K.
Right arrow Articles by Bates, T. E.

Effect of Nitrogen to Phosphorus Atom Ratio of Ammonium Phosphates on Emergence of Wheat (Triticum vulgare)1

C. K. Stevenson and T. E. Bates2

Ammonium phosphates providing five N:P atom ratios (1.00, 1.25, 1.50, 1.75, and 2.00:1) were applied in solution in the row with wheat seed at planting in greenhouse experiments. The soils used were Oneida clay loam (CEC 18.3 meq/100 g) and Fox sandy loam (CEC 8.2 meq/100 g) each adjusted to pH levels ranging from 5.4 to 7.4. Soil pH, over the range studied, had no effect on emergence with any of the ammonium phosphate materials tested. Neither early nor final emergence changed when the N:P atom ratio was varied in the clay loam soil when the molarity of the fertilizer solution was held constant (equal rates of P but varying rates of N). In the sandy loam soil early emergence was markedly lower with high N:P atom ratio materials than with low ratio materials. Final emergence showed the same trend as early emergence with the sandy loam soil but differences between materials were much smaller. The difference in results between the two soils is attributed to the effect of cation exchange capacity on the toxicity of ammonia in the soil.


1 Contribution from the Department of Soil Science, Ontario Agricultural College, University of Guelph, Guelph, Ontario, from a thesis submitted by the senior author in partia fulfillment of the requirements for a M.Sc. degree. This research was supported by the Ontario Department of Agriculture and Food and by Cyanamid of Canada. Presented before Div. S-8, Soil Sci. Soc. Amer., August 1966 at Stillwater, Oklahoma.

2 Soils Specialist, Ridgetown College of Agricultural Technology, Ridgetown, Ontario, and Professor, University of Guelph.

Received for publication February 23, 1968.





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 © 1968 by the American Society of Agronomy.