Studies of fresh and fossil tracks in meteoritic hypersthene

R.K. Bull, S.A. Durrani
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引用次数: 6

Abstract

From measurements of the total recordable lengths of fossil tracks and freshly-produced Fe ion tracks in meteoritic hypersthene, the abundance of Fe relative to all VH ions (20 ≦ Z ≦ 28) in the time-averaged cosmic-ray flux is found to be ≈ 0.35. After allowance is made for the effects of fragmentation of nuclei at a depth of ≈ 11 cm within the meteorite, this value is found to be in broad agreement with presentday measurements.

These crystals have been irradiated with a number of heavy ions with a view to calibrating them for the identification of VVH cosmic rays by measurement of track-etch velocity, VT, as a function of residual range. A good fit to the calibration data is obtained by using a value for the constant K in the primary-ionization equation of 10.5 (±0.5). The relationship between VT and primary ionization J appears to be approximately linear.

陨石变质岩中新鲜足迹和化石足迹的研究
通过测量陨石超细铁中化石痕迹和新产生的铁离子痕迹的总可记录长度,发现在时间平均宇宙射线通量中,铁相对于所有VH离子(20≦Z≦28)的丰度为≈0.35。在考虑到陨石内部约11厘米深度的核碎裂的影响后,发现这个值与目前的测量结果基本一致。用一些重离子照射这些晶体,目的是通过测量轨迹蚀刻速度VT作为残余范围的函数来校准它们,以便识别超高频宇宙射线。利用初电离方程中常数K的值为10.5(±0.5),得到了与标定数据很好的拟合。VT与初离J之间的关系近似为线性关系。
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