小型高分辨率~3He/~4He质谱计的离子光学

  • 摘要: <正> 一、前言 地球上氦同位素组成有三个层次:地幔氦、地壳氦和大气氦。地幔氦是地球生成时保留下来的原生氦,~3He含量高,~3He/~4He比值约10~(-5);地壳氦是地壳中铀、钍等放射性元素蜕变过程中生成的,~3He/~4He比值约10~(-7)~10~(-8);大气氦是在地幔氦与地壳氦不断地向

     

    Abstract: To measure the isotopic abundance ratio of ~3He and ~4He in samples by massspectrometers is an important detection mean for helium isotope geochemistryresearch. A symmetrically arranged tandem ~3He/~4He mass spectrometer is describedin the paper. The front stage, used to analyse ~3He (including HD and H_3) and~4He, is a homogeneous analysing magnet with a bending angle of 90° and abending radius of 6 cm. The end stage, used to analyse ~3He, HD and H_3, is anon-homogeneous analysing magnet with a bending angle of 180°, a bending radiusof 15 cm and a magnetic field gradient of 0.75. Because of the use of the non-zero second order coefficient β and curved entrance face of the later magnet foreliminating second order aberrations, the resolving power of the system is notablyimprbved, and theoretically reaches about 3800.

     

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