Bilingual edition: English is preserved and Chinese follows each unit. Terminology uses the confirmed v20260916 glossary; automated semantic review remains traceable.
中英双语版:英文原文完整保留,中文紧随对应单元;术语采用 v20260916 确认表,自动语义审校结果可追溯。

Radioactive Nuclides by Half-Life

按半衰期分类的放射性核素
Nuclide
核素
Half-Life
(years)
半衰期(年)
Found
in Nature?
自然界中发现?
50V
6.0x1015
yes
是
144Nd
144Nd
2.4x1015
yes
是
174Hf
2.0x1015
yes
是
192Pt
1x1015
yes
是
115In
115 在
6.0x1014
yes
是
152Gd
1.08x1014
yes
是
123Te
1.2x1013
yes
是
190Pt
6.9x1011
yes
是
138La
1.12x1011
yes
是
147Sm
147Sm
1.06x1011
yes
是
87Rb
87瑞利球
4.88x1010
yes
是
187Re
4.3x1010
yes
是
176Lu
3.5x1010
yes
是
232Th
232Th
1.40x1010
yes
是
238U
4.47x109
yes
是
40K
1.25x109
yes
是
235U
7.04x810
yes
是
244Pu
244Pu
8.2x107
yes
是
146Sm
7.0x107
no
无
205Pb
205Pb
3.0x107
no
无
236U
2.39x107
yes-P
是的
129I
1.7x107
yes-P
是的
247Cm
1.60x107
no
无
182Hf
9.0x106
no
无
107Pd
107号元素
7x106
no
无
53Mn
53锰
3.7x106
yes-P
是的
135Cs
135Cs
3.0x106
no
无
97Tc
97Tc
2.6x106
no
无
237Np
237 Np(专名或术语)
2.14x106
yes-P
是的
150Gd
2.1x106
no
无
10Be
1.6x106
yes-P
是的
93Zr
93号元素
1.5.0x106
no
无
98Tc
1.5x106
no
无
153Dy
1x106
no
无

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。
Modeling the age of the Earth
地球年龄的建模
Index

Nuclear Tables

Reference
Miller
Ch 3
索引核表参考Miller第3章
 
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