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


     


Published in J Environ Qual 24:314-323 (1995)
© 1995 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 Litaor, M. I.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Litaor, M. I.
Agricola
Right arrow Articles by Litaor, M. I.

Uranium Isotopes Distribution in Soils at the Rocky Flats Plant, Colorado

M. Iggy Litaor*

Environmental Restoration Management, EG&G Rocky Flats Plant, Building 080, Golden, CO 80402-0464.

* Corresponding author.

ABSTRACT

Soils east of Rocky Flats Plant (RTF) near Golden, CO, are contaminated with U as a result of past waste-storage practices, accidental release of oils laden with U, and low-level airborne emissions. A spatial analysis of three U isotopes was conducted to determine the concentration and distribution pattern of U contamination. Soils were sampled from 118 plots of 1.01- or 4.05-ha by compositing 25 evenly spaced samples from the top 0.64 cm. Uranium-234 activity ranged from 25.9 to 92.8 Bq kg–1, U-235 activity ranged from 0.1 to 25.1 Bq kg–1, whereas U-238 activity ranged from 30.7 kg–1 to 286 Bq kg–1. Geostatistical techniques were used to model the spatial dependency and construct isopleth maps showing U isotope distributions. Spatial correlation was not observed for U-234. This implies that U-234 is randomly distributed in the soil environment east of RFP. Uranium-235 exhibited a spotty and localized concentration pattern with no clear relationship between known burial and spill sites, and the present distribution of U-235 in the soils. Proposed wind-dispersal mechanisms were not consistent with the spatial distribution of U isotopes. Most of the observed activities of U-234 and U-235 were well within the natural range of U isotopes in soils. The lack of similarity in spatial distribution between Pu-239 + 240 and U isotopes probably resulted from the higher solubility and teachability of U isotopes compared with Pu-239 + 240 in the soil system. Although U-238 exhibited a pattern of localized spatial distribution, most of its observed activity was well within the natural range of U-238 activity in soils.


Received for publication March 8, 1994.





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
Soil Science Society of America Journal Journal of Plant Registrations The Plant Genome
Copyright © 1995 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.