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

The atomic weight and isotopic composition of oxygen and their variation in nature

Conference ·
OSTI ID:5920809
There is a problem with the absolute abundance measurements of oxygen. One of these calibrated measurements is in error, either oxygen in air, or oxygen in (V-SMOW), Vienna's standard mean ocean water reference material. Nier's measurement in air is probably wrong by three times his quoted error and his ratio for /sup 18/O//sup 16/O should be 0.002053 and not 0.002044. Fortunately, this has only a minor effect on the atomic weight. However, this error raises doubts on all /sup 17/O)//sup 16/O values. Each /sup 17/O//sup 16/O is determined using an enrichment factor, relative to the value of /sup 17/O//sup 16/O in the standard, which is the square root of the enrichment factor for /sup 18/O//sup 16/O relative to the standard. All standards, including V-SMOW, have /sup 17/O//sup 16/O values which have been derived originally from Nier's measurement of oxygen in air. In addition, a review of the literature provides isotopic abundance variations in various sources of oxygen. 115 refs., 12 tabs.
Research Organization:
Brookhaven National Lab., Upton, NY (USA)
DOE Contract Number:
AC02-76CH00016
OSTI ID:
5920809
Report Number(s):
BNL-NCS-39950; CONF-8708105-4; ON: DE87014397
Country of Publication:
United States
Language:
English