Raisbeck G M, Yiou F, Fruneau M, Loiseaux J M
Science. 1978 Oct 13;202(4364):215-7. doi: 10.1126/science.202.4364.215.
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 x 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.
格勒诺布尔回旋加速器已被用作质谱仪,用于测量标准化氧化铍样品中铍 - 10与铍 - 9的比率,分别为10的 - 8次方、10的 - 9次方和10的 - 10次方。类似的测量可用于确定各种地球物理储层(如海洋沉积物和极地冰)中的宇宙成因铍 - 10(半衰期为1.5×10的6次方年)分布。该方法可用于确定此类样品的年代,或提供有关过去影响铍 - 10生产率的地球物理和天体物理现象的信息。