概括
维克鲁站石中的酸盐结节的鲁比-测年揭示了47亿年的年龄. 这支持一个快速的太阳系形成时期,与其他铁石年龄估计形成鲜明对比.
科学领域:
- 地质化学 地质化学
- 宇宙化学 宇宙化学
- 同位素地球化学 同位素地球化学
背景情况:
- 石中的酸盐块为早期太阳系过程提供了洞察力.
- 鲁比- (Rb-Sr) 同位素系统学对于行星物质的测年至关重要.
研究的目的:
- 为了确定从Wekeroo站石中的酸盐块中和的同位素组成和度.
- 为了确定石的年龄,并推断出太阳系分化的时间.
主要方法:
- 卢比和度的同位素分析.
- 使用Sr{87}:Sr{86}和Rb/Sr比率构建一个的演变图.
- 使用同位时间约会方法计算石年龄.
主要成果:
- 的同位素比 (Sr(87):Sr(86)) 从0.729到0.768不等,与合体相比,显示了丰富度.
- 数据点形成一个同位素,产生了0.6960.702.6的初始Sr(87):Sr(86) 比率.
- 计算年龄为47亿年,与地球和石质石形成年龄一致.
结论:
- 维克鲁站石大约在47亿年前形成.
- 这个时代支持一个快速,狭窄的间隔,主要的太阳系化学和物理差异化.
- 来自其他铁石的Ar{40) -K{40) 年龄的差异凸显了对多样化的同位素研究的需要.
更多相关视频
09:45Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
Published on: July 24, 2016
09:41Isolation of Quartz Grains for Optically Stimulated Luminescence (OSL) Dating of Quaternary Sediments for Paleoenvironmental Research
Published on: August 2, 2021
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.
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...
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...
Microbes and Other Elemental Cycles
Microbial activity plays a pivotal role in the biogeochemical cycling of iron and manganese, especially at the redox gradients characteristic of stratified aquatic environments. These cycles are driven by microbial transformations between oxidized and reduced forms of the metals, allowing organisms to exploit them for metabolic energy and structural purposes.Iron Cycling Across Redox GradientsIn neutral, oxygen-rich surface waters, iron is predominantly found in its oxidized, insoluble ferric...
Atomic Mass
Atoms — and the protons, neutrons, and electrons that compose them — are extremely small. For example, a carbon atom weighs less than 2 × 10−23 g. When describing the properties of tiny objects such as atoms, we use appropriately small units of measure, such as the atomic mass unit (amu). The amu was originally defined based on hydrogen, the lightest element, then later in terms of oxygen. Since 1961, it has been defined with regard to the most abundant isotope of carbon, atoms of which are...
Conditions on Early Earth
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
