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 27:141-144 (1963)
© 1963 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 Miller, J. R.
Right arrow Articles by Reitemeier, R. F.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Miller, J. R.
Right arrow Articles by Reitemeier, R. F.
Agricola
Right arrow Articles by Miller, J. R.
Right arrow Articles by Reitemeier, R. F.

The Leaching of Radiostrontium and Radiocesium Through Soils1

J. R. Miller and R. F. Reitemeier2

ABSTRACT

Sr90 and Cs137 are hazardous, long-lived, nuclear fission products. Experiments were conducted in the greenhouse to determine their downward movement in soils under intensive leaching. The five soils (Norfolk, Hagerstown, Miami, Fort Collins, and Huntley series) selected for the investigation represented a wide range of soil properties, and the leaching treatments consisted of 30 inches and 300 inches of deionized water, 0.005N NaCl, and 0.005N CaCl2. There was little downward movement of Cs134 when the soils received the applications of deionized water, NaCl, or CaCl2. Radioactive assays of the soil columns showed that 96.6 to 100% of the Cs134 was in the surface two layers of the soil columns (average depth 1.4 inches) after 300 inches of leaching. In the leaching experiment with Sr, the CaCl2 produced the greatest movement of Sr89 and deionized water the least. The maximum distance Sr89 penetrated into the soils when leached with 30 inches of water was 1.3 inches, and with 300 inches of water the distance was 4.3 inches. In general, there was more movement of Sr89 in the Norfolk soil and least in the Huntley, with the other soils being intermediate.


NOTES

1 Contribution from the Soil and Water Conservation Research Division, Agricultural Research Service, USDA, Beltsville, Md. This research was supported by the U. S. Atomic Energy Commission. Presented before Div. I and II, Soil Science Society of America, Nov. 30, 1961, at St. Louis, Mo.

2 Formerly soil scientists, USDA. Currently Associate Professor of Soils, Department of Agronomy, University of Maryland, and Soil Scientist, Division of Biology and Medicine, U. S. Atomic Energy Commission, respectively.

Received for publication April 11, 1962. Accepted for publication June 26, 1962.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 1963 by the Soil Science Society of America.