Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

The depletion of radioisotopes from the Columbia River by natural processes

Technical Report ·
OSTI ID:5917679
Ten radioisotopes were introduced into the Columbia River in effluent water from the Hanford reactors. An average depletion of 35% was measured between the reactor outfalls and the Pasco and Kennewick water plants. This depletion is a self-purification that may be an important factor in estimating exposures resulting from domestic use of this water. Variations in radioisotope loss from sample to sample and studies of the amounts of radioisotopes associated with the filterable solids in the river indicated that incorporation in sediments may account for a large part of the depletion. Since this incorporation will depend on the solids content of the river, it is to be expected that the self-purification of the river will vary with stream conditions. The values reported here are thus representative only of the conditions existing during the period of these studies. A study of amount of loss of four radioisotopes to the river from Pasco to Vancouver, Washington, indicates that Cr/sup 51/ and Zn/sup 65/ should be prominent in river sediments. Analyses of one river mud sample confirmed these isotopes as the major radioactive contaminants. 12 refs., 1 fig., 19 tabs.
Research Organization:
General Electric Co., Richland, WA (USA). Hanford Atomic Products Operation
DOE Contract Number:
AC06-76RL01830
OSTI ID:
5917679
Report Number(s):
HW-52908; ON: DE88001918
Country of Publication:
United States
Language:
English

Similar Records

Removal of radioisotopes from the Columbia River by natural processes
Technical Report · Mon Apr 09 23:00:00 EST 1962 · OSTI ID:5716289

THE REMOVAL OF RADIOISOTOPES FROM THE COLUMBIA RIVER BY NATURAL PROCESSES
Technical Report · Mon Apr 09 23:00:00 EST 1962 · OSTI ID:4764349

Radioactivity levels of the Columbia River below Richland, Washington for the period January, February, March 1955
Technical Report · Mon Jul 18 00:00:00 EDT 1955 · OSTI ID:5999024