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This table of radioactive nuclides sorted by their half-lives is taken from Miller, who uses it to point out that only those radionuclides with half-lives greater than 80 million years are found in nature. The exceptions are those marked with "Yes-P" indicating that they are being produced in nature, but would otherwise be missing. The point of Miller's use was to make the case that the Earth is more than 80 million years old since all isotopes with shorter halflives are no longer found in nature. It is also evident that the Earth is not infinitely old because all the radioactive series would have decay. There are various ways of modeling the age of the Earth, and the values center around 4.5 billion years.
这张按半衰期排序的放射性核素表摘自Miller,他用此表指出,只有半衰期超过8000万年的放射性核素才能在自然界中找到。例外的是那些标记为'Yes-P'的,表明它们是在自然界中产生的,但若不考虑这种产生方式,它们将不会存在。Miller使用此表的目的是为了论证地球的年龄超过8000万年,因为所有半衰期更短的同位素都不再存在于自然界中。此外,也明显可以看出地球并非无限古老,因为所有放射系都会发生衰变。存在多种计算地球年龄的方法,所得数值大致集中在45亿年左右。
Beryllium-10 is found because it is continually produced by cosmic ray bombardment of the upper atmosphere. So very small amounts of this isotope are found in rainfall and sediment. Neptunium-237 is produced by cosmic ray bombardment of the moon. There are other short half-life isotopes found on the Earth from the natural radioactive series.
Note: Information about isotopes may be found in tables linked to the  Periodic table. Take the link to "Nuclear data" at the bottom of the display for any element.
注意:有关同位素的信息可在与元素周期表链接的表格中找到。如需任何元素的核数据,请点击显示底部的“核数据”链接。
铍-10的存在是因为它持续由宇宙射线轰击大气层而产生。因此,这种同位素在降雨和沉积物中可以发现少量。镎-237是由宇宙射线轰击月球而产生的。地球上还存在其他半衰期很短的同位素,这些同位素来自自然放射系。 |