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 19:288-292 (1955)
© 1955 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 Whittaker, C. W.
Right arrow Articles by Hoffman, W. M.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Whittaker, C. W.
Right arrow Articles by Hoffman, W. M.
Agricola
Right arrow Articles by Whittaker, C. W.
Right arrow Articles by Hoffman, W. M.

"Brown Mud" from the Aluminum Industry as a Soil Liming Material1

Colin W. Whittaker, W. H. Armiger, P. P. Chichilo and W. M. Hoffman2

ABSTRACT

"Brown mud" is a siliceous waste product resulting from the extraction of alumina from bauxite. Present production is estimated to exceed half a million tons annually, the disposal of which is a problem in the industry. When dry, the mud contains approximately SiO2 23, CaO 47, Fe2O3 10, TiO2 3.5, Al2O3 5.5, and Na2O 3.6%, and small amounts of other elements.

In a greenhouse study with sweetclover as the indicator crop, using acid Evesboro and Chester soils, the dried brown mud produced yields substantially equal to those obtained with equivalent amounts of other liming materials. Emergence counts and appearance of the crop gave no indications of any toxic effects from the use of the mud. The mud increased soil pH to values that were usually equal to or exceeding those produced by finely divided agricultural limestone and were sometimes equal to those produced with hydrated lime. The calcium concentration in the dried plant material increased as the liming rate increased in about the same manner with the mud as with the other liming materials. As might be expected, the sodium content of the crop tended to be higher where the mud was used. The potassium content of the crop was reduced to a greater extent by the mud than by either hydrated lime or limestone: this effect was probably also due to the sodium content of the mud. The data indicate that the dried mud is a satisfactory liming material.


NOTES

1 Contribution by the Soil and Water Conservation Research Branch, Agricultural Research Service, U. S. D. A. Beltsville, Md. Presented before Div. IV. Soil Science Society of America, St. Paul, Minn., Nov. 9, 1954.

2 The authors are grateful to John G. Cady for making the petrographic and X-ray examinations, to various staff members for chemical analysis and other assistance, and to the M. J. Grove Lime Co. for supplying the agricultural limestone.

Received for publication October 4, 1954.





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 © 1955 by the Soil Science Society of America.