Stable isotope signatures of hydration water in secondary mineralization on UO2
Abstract
No abstract availableKeywords
Funding Information
- Office of Defense Nuclear Nonproliferation
- Lawrence Livermore National Laboratory (DE-AC52-07NA27344)
- U.S. Department of Energy
- National Nuclear Security Administration (LLNL-JRNL-812681)
This publication has 31 references indexed in Scilit:
- Isoscapes: Spatial Pattern in Isotopic BiogeochemistryAnnual Review of Earth and Planetary Sciences, 2010
- A detailed study of UO2 to U3O8 oxidation phases and the associated rate-limiting stepsJournal of Nuclear Materials, 2006
- Empirical Identification of Uranium Oxides and Fluorides Using Electron Energy-loss Spectroscopy in the Transmission Electron MicroscopeMicroscopy and Microanalysis, 1999
- A review of the oxidation of uranium dioxide at temperatures below 400°CJournal of Nuclear Materials, 1998
- The hydrogen and oxygen isotope geochemistry of pedogenic clay minerals: principles and theoretical backgroundGeoderma, 1998
- Stable isotope geochemistry of clay mineralsClay Minerals, 1996
- Retention and release of water by sintered uranium dioxideJournal of Nuclear Materials, 1982
- Deuterium and oxygen-18 correlation: Clay minerals and hydroxides in Quaternary soils compared to meteoric watersGeochimica et Cosmochimica Acta, 1971
- Stable isotopes in precipitationTellus, 1964
- The hydrogen content of atmospheric air at ground levelQuarterly Journal of the Royal Meteorological Society, 1957