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Title: Studies of the mobility of uranium and thorium in Nevada Test Site tuff

Technical Report ·
DOI:https://doi.org/10.2172/138338· OSTI ID:138338
; ;  [1]
  1. Lawrence Berkeley Lab., CA (United States)

Hydro-geochemical processes must be understood if the movement of radionuclides away from a breached radioactive waste canister is to be modeled and predicted. In this respect, occurrences of uranium and thorium in hydrothermal systems are under investigation in tuff and in rhyolitic tuff that was heated to simulate the effects of introduction of radioactive waste. In these studies, high-resolution gamma spectrometry and fission-track radiography are coupled with observations of alteration mineralogy and thermal history to deduce the evidence of, or potential for movement of, U and Th in response to the thermal environment. Observations to date suggest that U was mobile in the vicinity of the heater but that localized reducing environments provided by Fe-Ti-Mn-oxide minerals concentrated U and thus attenuated its migration.

Research Organization:
Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
OSTI ID:
138338
Report Number(s):
LBL-29700; ON: DE92000647; TRN: JT9212%%580
Resource Relation:
Other Information: PBD: Jun 1991; Related Information: Is Part Of Earth Sciences Division annual report 1990; PB: 197 p.
Country of Publication:
United States
Language:
English