概括
和等放射性元素揭示了岩起源的时间表. 它们的衰变产物跟踪地幔融化和地分化的过程,为火山岩石的形成提供了洞察力.
科学领域:
- 地质化学 地质化学
- 同位素地质学的同位素.
- 火山学 火山学是一门学科.
背景情况:
- 和的短寿命放射性衰变产物是地质过程的敏感指标.
- -238,-230和-226的放射性不平衡在火山岩中很常见.
研究的目的:
- 调查火山岩中的放射性不平衡和同位素如何限制岩石形成的时间表.
- 为了了解融化程度,速度和蒸汽存在对这些同位素特征的影响.
主要方法:
- 对放射性不平衡的分析,特别是-238,-230和-226.6之间的分析.
- 在火山样本中检查的同位素组成.
主要成果:
- 放射性不平衡在火山岩中很普遍,反映了岩起源过程.
- 地幔融化的程度和速度,以及蒸汽条件,显著影响观察到的不平衡和同位素.
- 地幔融化可以发生在几十万年内,而岩上升和分化发生在更短的时间范围内.
结论:
- 短寿命的-衰变产物对地幔融化和地分化的时间提供了关键的约束.
- 对这些元素的同位素分析有助于重建岩形成和喷发的复杂历史.
相关概念视频
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:
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.
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...
Biological Effects of Radiation
All radioactive nuclides emit high-energy particles or electromagnetic waves. When this radiation encounters living cells, it can cause heating, break chemical bonds, or ionize molecules. The most serious biological damage results when these radioactive emissions fragment or ionize molecules. For example, α and β particles emitted from nuclear decay reactions possess much higher energies than ordinary chemical bond energies. When these particles strike and penetrate matter, they produce ions...
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...


