相关实验视频
Updated: Jul 12, 2026

06:14
Simulating Imaging of Large Scale Radio Arrays on the Lunar Surface
Published on: July 30, 2020
概括
从月球样本中测量了来自宇宙射线相互作用的放射性. 太阳宇宙射线对月球土壤和岩石中观察到的三和放射性有着显著的贡献.
科学领域:
- 太空化学 太空化学
- 核地质物理学 核地质物理学
背景情况:
- 月球土壤和岩石含有由宇宙射线相互作用产生的放射性同位素.
- 了解这些放射性同位素有助于确定月球表面暴露年龄和宇宙辐射的来源.
研究的目的:
- 在月球样本中测量和的放射性.
- 用三和-3来计算月球曝光年龄.
- 为了区分来自银河系和太阳宇宙射线的贡献.
主要方法:
- 在月球土壤和岩石样本中测量和的放射性.
- 使用三--3和同位素数据计算暴露年龄.
主要成果:
- 月球土壤中的含量高于月球岩石中的含量.
- 从三和-3计算的暴露年龄在2.05亿年至3.75亿年之间.
- -37和-39的放射性比石质石更高,这表明暴露年龄更高.
- 至少有一半的观测到的放射性物质归因于太阳宇宙射线.
结论:
- 太阳宇宙射线在月球样本中产生放射性物质方面发挥着重要作用.
- 从不同同位素计算的暴露年龄的差异需要进一步调查.
- 月球样本为了解宇宙射线相互作用和太阳活动提供了宝贵的数据.
相关概念视频
Radioactive Decay and Radiometric Dating
Radioactivity is a spontaneous disintegration of an unstable nuclide and is a random process, as all the nuclei in the sample do not decay simultaneously. The number of disintegrations per unit time is called the activity (A), which is directly proportional to the number of nuclei in the sample. The decay constant (λ) is an average probability of decay per nucleus in unit time.
Isotopes and Radioisotopes
In the early 1900s, English chemist Frederick Soddy realized that an element could have atoms with different masses that were chemically indistinguishable. These different types are called isotopes — atoms of the same element that differ in mass. Isotopes differ in mass because they have different numbers of neutrons but are chemically identical because they have the same number of protons. Soddy was awarded the Nobel Prize in Chemistry in 1921 for this discovery.
An isotope containing more...
An isotope containing more...
Nuclear Transmutation
Nuclear transmutation is the conversion of one nuclide into another. It can occur by the radioactive decay of a nucleus, or the reaction of a nucleus with another particle. The first manmade nucleus was produced in Ernest Rutherford’s laboratory in 1919 by a transmutation reaction, the bombardment of one type of nuclei with other nuclei or with neutrons. Rutherford bombarded nitrogen-14 atoms with high-speed α particles from a natural radioactive isotope of radium and observed protons being...
Radioactivity and Nuclear Equations
Nuclear chemistry is the study of reactions that involve changes in nuclear structure. The nucleus of an atom is composed of protons and, except for hydrogen, neutrons. The number of protons in the nucleus is called the atomic number (Z) of the element, and the sum of the number of protons and the number of neutrons is the mass number (A). Atoms with the same atomic number but different mass numbers are isotopes of the same element.
A nuclide of an element has a specific number of protons and...
A nuclide of an element has a specific number of protons and...
Types of Radioactivity
The most common types of radioactivity are α decay, β decay, γ decay, neutron emission, and electron capture.
Alpha (α) decay is the emission of an α particle from the nucleus. For example, polonium-210 undergoes α decay:
Alpha (α) decay is the emission of an α particle from the nucleus. For example, polonium-210 undergoes α decay:
Nuclear Stability
Protons and neutrons, collectively called nucleons, are packed together tightly in a nucleus. With a radius of about 10−15 meters, a nucleus is quite small compared to the radius of the entire atom, which is about 10−10 meters. Nuclei are extremely dense compared to bulk matter, averaging 1.8 × 1014 grams per cubic centimeter. If the earth’s density were equal to the average nuclear density, the earth’s radius would be only about 200 meters.
To hold positively charged protons together in the...
To hold positively charged protons together in the...

