JEQ Grow Your Career With ASA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in J Environ Qual 11:134-141 (1982)
© 1982 American Society of Agronomy, Crop Science Society of America, and 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
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Hoffman, F. O.
Right arrow Articles by Lucas, D. M.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Hoffman, F. O.
Right arrow Articles by Lucas, D. M.
Agricola
Right arrow Articles by Hoffman, F. O.
Right arrow Articles by Lucas, D. M.

Interception and Retention of Technetium by Vegetation and Soil1

F. Owen Hoffman2, Charles T. Garten, Jr.3, John W. Huckabee4 and Deborah M. Lucas3

ABSTRACT

Field experiments were performed to quantify the initial interception and retention of technetium (Tc) by herbaceous vegetation as a consequence of direct deposition and uptake from soil. A simulated rain containing a solution of 95mTcO4 was applied to plots of bare soil and plots with standing vegetation. Vegetation emerging in the bare-soil plots obtained Tc predominantly from root uptake. Vegetation standing during the initial application obtained Tc from both direct foliar interception and root uptake. For the plots with standing vegetation, the estimated initial interception fraction (r) ranged from 0.079 to 0.17. The mass interception factor (r/Yv) ranged from 0.65 to 1.1 m2/kg. The retention of Tc by vegetation receiving direct foliar contamination varied with environmental half-times (Tw) ranging from 15.9 to 18.7 days. Adjusting for the effects of growth dilution increased the values of Tw (range 21.6–28.7 days). For vegetation emerging from the plots of initial bare soil, retention was equivalent to a Tw of 43 days. These data indicated that uptake of Tc from soil diminished with time and that Tc was removed from plant tissue. In soil, a downward movement was evident, because Tc in the top 2 cm decreased with time and concentrations at lower soil depths (6–8 and 14–15 cm) increased with time. The application of these data to predict steady-state concentrations of Tc in vegetation resulting from continuous deposition does not differ substantially from predictions based on the use of generic-default parameter values recommended in Regulatory Guide 1.109 of the U.S. Nuclear Regulatory Commission (1977).

Key Words: pertechnetate • radioecology • environmental assessment


NOTES

1 Research sponsored by the Office of Health and Environ. Res., U.S. Dep. of Energy under contract W-7405-eng-26 with Union Carbide Corporation, Oak Ridge Natl. Lab., Oak Ridge, TN 37830.

2 Research Staff Member, Health and Safety Res. Div., Oak Ridge Natl. Lab., and Graduate Program in Ecology, University of Tennessee, Knoxville, TN 37996-1100.

3 Research Associate and Research Technician, respectively, Environ. Sci. Div., Oak Ridge Natl. Lab.

4 Project Manager, Environmental Assessment Department, Electric Power Research Institute, Palo Alto, CA 94303.

Received for publication February 13, 1981.





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
Soil Science Society of America Journal
Copyright © 1982 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.