液体Sr-Y来源的年龄测定
Hanna Vasylyeva1, Ivan Mironyuk2, Mykola Strilchuk3
1Uzhhorod National University, Uzhhorod, Ukraine.
概括
这项研究引入了一种新的方法,用于测定-90 (Sr) 的年龄,使用二氧化 (TiO2) 吸附剂来分离-90 (Zr). 这种技术与ICP-MS相结合,可以准确地确定Sr-Y源的年龄.
科学领域:
- 放射化学 放射化学是指辐射化学.
- 分析化学 分析化学
- 材料科学 材料科学 材料科学
背景情况:
- 精确的放射性源的年龄约定,如90Sr对于核废物管理和环境监测至关重要.
- 从 (Sr) 和 (Y) 分离 (Zr) 是确定Sr-Y源的年龄的一个关键挑战.
研究的目的:
- 为了研究离子的选择性吸附,使用化学修饰的TiO2吸附剂进行年龄测定,Sr.
- 开发和验证一种方法来分离90Zr和90Sr-90Y的液体来源.
- 通过化学分离获得的年龄测定结果与混合液晶闪光计数 (LSC) 和诱导合等离子体质谱法 (ICP-MS) 方法的结果进行比较.
主要方法:
- 选择性吸附离子使用化学改性TiO2基吸附剂.
- 使用诱导联等离子体质谱法 (ICP-MS) 分析阴离子度.
- 通过同位素分离和LSC和ICP-MS测量的联合测定Sr-Y来源的年代.
主要成果:
- 通过TiO2吸附剂,首次证明了90Zr和90Sr从液体90Sr-90Y来源中的分离.
- 成功测量了90Zr/90Sr比,以确定液体源的年龄.
- 在化学分离的年龄测定结果和LSC-ICP-MS组合方法之间取得了很好的一致性,证实了交叉验证.
结论:
- 化学修饰的TiO2吸附剂在90Sr的选择性吸附中是有效的.
- 开发的化学分离方法与LSC和ICP-MS一起,为Sr-Y来源提供可靠和交叉验证的年龄确定.
- 结合分析技术可以提高对放射性源年龄测定结果的信心.
相关概念视频
Radioactive Decay and Radiometric Dating
34.3K
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.
34.3K
Isotopes and Radioisotopes
8.6K
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...
An isotope containing...
8.6K
Nuclear Stability
19.0K
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...
To hold positively charged protons together...
19.0K
Isotopes
56.9K
Elements have a set number of protons that determines their atomic number (Z). For example, all atoms with eight protons are oxygen; however, the number of neutrons can vary for atoms of the same element. 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 called isotopes. Elements can have multiple isotopes, for example, carbon-12, carbon-13, and carbon-14.
An element's atomic mass, or weight,...
An element's atomic mass, or weight,...
56.9K
Imaging Studies II: Positron Emission Tomography and Scintigraphy
158
Positron Emission Tomography (PET) is a medical imaging technique that provides crucial insights into the body's physiological functions at a molecular level. It is an indispensable resource for diagnosing, staging, and monitoring various illnesses, notably cancer, neurological disorders, and cardiovascular conditions.
Fundamental Principles of PET
Fundamental Principles of PET
158
Nuclear Transmutation
17.6K
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...
17.6K


