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


     


Published in Soil Sci Soc Am J 23:47-50 (1959)
© 1959 Soil Science Society of America
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 DeMent, J. D.
Right arrow Articles by Bradford, B. N.
Right arrow Search for Related Content
PubMed
Right arrow Articles by DeMent, J. D.
Right arrow Articles by Bradford, B. N.
Agricola
Right arrow Articles by DeMent, J. D.
Right arrow Articles by Bradford, B. N.

A Method for Measuring Short-Term Nutrient Absorption by Plants: II. Potassium1

Jack D. DeMent, George Stanford and B. N. Bradford2

ABSTRACT

The method previously reported for measuring short-term P absorption by plants has been adapted to studies of K uptake in relation to various factors. K-deficient oat or corn plants, grown in sand cultures, were placed in contact with soil or soil-fertilizer mixtures for periods of 1 to 14 days. Recovery in oat tops from applications of 10 to 120 mg. K ranged from 25 to 7% in 3 days to 63 to 30% in 14 days. When K content of roots in sand and in soil also was taken into account, 14-day recoveries from 30- and 120-mg. K additions were 85 and 43% respectively. Despite the wide range in K content of plants, growth differences among treatments were not apparent for at least the first week, as had previously been observed in studies with P.

Unfertilized soils supplied significant amounts of K to plants in 3 days. At 7 days, rather wide differences in K content of plants were evident among soils, indicating the possible utility of the method in assessing the K status of soils. Moisture contents of soils were important in relation to K uptake. Moisture equivalent for each soil appeared to be the near-optimum level.

Availabilities of K in potassium calcium pyrophosphate (KCP), potassium metaphosphate (KMP), and KCl to corn plants were compared in soil and sand. During 1- and 3-day absorption periods, KCl was more available than KMP and KCP in both media. The data suggest that contact with soil increased dissolution of the KMP and KCP. KCl was less available in soil than in sand.

Very high correlations were found between uptake of K by tops and whole plants for a wide range of K rates, absorption periods, and soils. Thus, K content of plant tops is a suitable criterion for assessing relative effects of treatments on K nutrition of the plants.


NOTES

1 Contribution from the Soils and Fertilizer Research Branch, Division of Agricultural Relations, Tennessee Valley Authority, Wilson Dam, Ala.

2 Agronomists and Analytical Chemist, respectively.

Received for publication June 19, 1958. Accepted for publication September 25, 1958.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Journal of
Environmental Quality
Copyright © 1959 by the Soil Science Society of America.