Beryllium-10 Mass Spectrometry with a Cyclotron
- 13 October 1978
- journal article
- research article
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 202 (4364) , 215-217
- https://doi.org/10.1126/science.202.4364.215
Abstract
The Grenoble cyclotron has been used as a mass spectrometer to measure ratios of beryllium-10 to beryllium-9 of 10 –8 , 10 –9 , and 10 –10 in standardized beryllium oxide samples. Similar measurements can be used to determine cosmogenic beryllium-10 (half-life, 1.5 × 10 6 years) profiles in various geophysical reservoirs such as sea sediments and polar ice. This procedure can be used either to date such samples or to give information about geophysical and astrophysical phenomena that have influenced the beryllium-10 production rate in the past.Keywords
This publication has 13 references indexed in Scilit:
- Heavy element mass spectroscopy with the Berkeley 88-inch cyclotronNuclear Instruments and Methods, 1978
- The10Be method of dating marine sediments — Comparison with the paleomagnetic methodEarth and Planetary Science Letters, 1977
- Carbon-14: Direct Detection at Natural ConcentrationsScience, 1977
- Analysis of causes for the beryllium-10 variations in deep sea sedimentsGeochimica et Cosmochimica Acta, 1977
- Radioisotope Dating with a CyclotronScience, 1977
- Sea Sediments, Cosmic Rays, and PulsarsNature, 1973
- Half-Life ofPhysical Review Letters, 1972
- Oxygen Isotope Profiles through the Antarctic and Greenland Ice SheetsNature, 1972
- Production cross sections of lithium and beryllium isotopes in 12C by high-energy protons and alpha particlesNuclear Physics A, 1971
- Mass-Spectrometric Measurement of Lithium, Beryllium, and Boron Isotopes Produced inby High-Energy Protons, and Some Astrophysical ImplicationsPhysical Review B, 1968