SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 31:390-393 (1967)
© 1967 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 Usherwood, N. R.
Right arrow Articles by Miller, J. R.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Usherwood, N. R.
Right arrow Articles by Miller, J. R.
Agricola
Right arrow Articles by Usherwood, N. R.
Right arrow Articles by Miller, J. R.

Effect of Soil pH on the Availability of Magnesium to Corn (Zea mays L.) from Magnesium Sulfate and High Magnesium Liming Materials1

Noble R. Usherwood and James R. Miller2

ABSTRACT

The effect of soil pH on the availability of Mg to corn from magnesium sulfate and several high Mg liming materials was studied in the greenhouse using a Keyport fine sandy loam soil. The soil pH was adjusted from 4.4 to 5.3, 5.7, 6.2, and 6.7 with CaCO2 containing less than 0.005% Mg. Magnesium was applied at rates of 0, 7.5, 15, 30, and 60 ppm of Mg as magnesium sulfate (9.9% Mg), coarse dolomitic limestone (12.0% Mg, 24% through a 100-mesh sieve), fine dolomitic limestone (12.4% Mg, 80% through a 100-mesh sieve), hydrated lime (18.7% Mg), and burnt lime (21.0% Mg). Corn (Zea mays L.) was grown for 30 days after emergence and the dry matter yields were determined. The plant tissue was analyzed for Mg.

With the exception of coarse dolomitic limestone the application of 7.5 to 15 ppm of Mg to the soil significantly (5% level) increased the dry matter yield of the corn, regardless of the Mg source of soil pH level. Higher Mg rates caused no further significant yield increase. In most cases, fine dolomitic limestone, hydrated lime, and burnt lime were as effective as magnesium sulfate for increasing corn yields, while coarse dolomitic lime-stone was often inferior to the other sources studied.

An increase in soil pH from 5.3 to 6.7 significantly decreased the uptake of Mg by corn from soil treated with coarse and fine dolomitic limestone but in most cases had no significant effect on Mg uptake from magnesium sulfate. Total Mg uptake from fine dolomitic limestone was significantly greater than from coarse dolomitic limestone applied at rates of 15, 30, and 60 ppm of Mg to soil of pH 5.3 to 6.7, but was usually significantly lower than Mg uptake from magnesium sulfate, hydrated lime, or burnt lime. Very little difference in total Mg uptake existed between magnesium sulfate and hydrated or burnt lime.


NOTES

1 Scientific article no. A1285 and contribution no. 3824 of the Maryland Agri. Exp. Sta., Dep. of Agronomy. Part of a dissertation submitted by the senior author in partial fulfillment of the requirements for the Ph.D. degree. Presented before Div. S-4 of the Soil Sci. Soc. of Amer., Nov. 2, 1965.

2 Research Assistant and Professor of Soils, respectively, Dep. of Agronomy, Univ. of Maryland. The senior author is currently Assistant Professor of Agronomy, Dep. of Agronomy and Agricultural Engineering, Univ. of Delaware.

Received for publication July 25, 1966. Accepted for publication February 20, 1967.







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 © 1967 by the Soil Science Society of America.