定义Definition
电子俘获是质子过多的原子核吸收一个核外内层电子(通常是 K 层电子),使一个质子转变为中子并放出一个中微子的衰变方式。原子序数减 1,质量数不变,同时伴随特征 X 射线或俄歇电子的发射。
Electron capture is a decay mode in which a proton-rich nucleus absorbs one of its own inner-shell electrons, usually from the K shell, turning a proton into a neutron and emitting a neutrino. The atomic number falls by one, the mass number is unchanged, and characteristic X-rays or Auger electrons follow.
原理Principle
电子俘获与 β⁺ 衰变的结果相同,但不需要满足 1.022 MeV 的能量阈值,因此在衰变能较小的质子富余核中是唯一可能的方式。K 层电子最靠近原子核,被俘获的概率最大。内层出现空位后,外层电子跃迁填补,放出子原子的特征 X 射线或俄歇电子。由于涉及核外电子,电子俘获的速率会因化学环境略有变化(如 ⁷Be 在不同化合物中差约 0.1%),这是“衰变不受外界影响”的少数例外。
Electron capture gives the same result as β⁺ decay but needs no 1.022 MeV threshold, so for proton-rich nuclei with small decay energies it is the only option. K electrons, closest to the nucleus, are most likely to be captured. Outer electrons then fill the vacancy, emitting the daughter's characteristic X-rays or Auger electrons. Because it involves atomic electrons, the rate changes slightly with chemical environment (about 0.1% for ⁷Be in different compounds), a rare exception to the rule that decay is unaffected by external conditions.
发现Discovery
1935 年汤川秀树和坂田昌一从理论上预言了电子俘获。1937 年阿尔瓦雷斯在钒-48 衰变中观测到子体钛的特征 X 射线,首次实验证实了这一过程。
Hideki Yukawa and Shoichi Sakata predicted electron capture theoretically in 1935. In 1937 Luis Alvarez observed characteristic titanium X-rays from the decay of vanadium-48, the first experimental confirmation.
应用Applications
⁴⁰K 约 11% 通过电子俘获衰变为 ⁴⁰Ar,这是钾-氩测年的基础。¹²⁵I(电子俘获)用于放射免疫分析和近距离放疗;⁵⁵Fe 是常用的 X 射线校准源;¹¹¹In、²⁰¹Tl、⁶⁷Ga 用于单光子核医学显像。俄歇电子射程极短,正在研究用于细胞核靶向治疗。
About 11% of ⁴⁰K decays by electron capture to ⁴⁰Ar, the basis of potassium–argon dating. ¹²⁵I (an electron-capture nuclide) is used in radioimmunoassay and brachytherapy, ⁵⁵Fe is a standard X-ray calibration source, and ¹¹¹In, ²⁰¹Tl and ⁶⁷Ga are used for single-photon nuclear imaging. The very short range of Auger electrons is being explored for therapy targeted at cell nuclei.
反应Reactions
通常俘获 K 层电子,随后放出特征 X 射线。
Usually a K electron is captured, followed by characteristic X-rays.
钾-氩测年的依据
The basis of potassium–argon dating
铍-7,太阳中微子的重要来源
Beryllium-7, an important source of solar neutrinos
X 射线校准源
An X-ray calibration source
年表Timeline
- 1935
汤川秀树与坂田昌一预言电子俘获
Yukawa and Sakata predict electron capture
- 1937
阿尔瓦雷斯实验证实
Alvarez confirms it experimentally
- 1950s
钾-氩测年法建立
Potassium–argon dating is established