泰勒雷霍夫的14C日期:铁器时代的时间表,法老和希伯来国王
Hendrik J Bruins1, Johannes van der Plicht, Amihai Mazar
1Ben-Gurion University of the Negev, Jacob Blaustein Institute for Desert Research, Department Man in the Desert, Sede Boker Campus, 84990, Israel. hjbruins@bgumail.bgu.ac.il
概括
以色列雷霍夫的放射性碳年代测定证实了法老肖申克一世 (希沙克) 在公元前925年左右的战役. 这项研究修订了铁器时代的年代表,并将埃及历史与圣经记载和爱琴海联系联系起来.
科学领域:
- 考古学科学 考古学科学
- 通过放射性碳测年法进行测年.
- 古代历史 古代历史 古代历史
背景情况:
- 法老肖申克一世 (希沙克) 的战役是公元前925年左右的一个关键历史事件.
- 埃及铭文和希伯来圣经都提到肖申克袭击以色列雷霍夫.
- 分层放射性碳测年方法为历史事件提供了独立的时间验证.
研究的目的:
- 在考古发现和历史记录之间建立精确的时间联系.
- 迄今为止,使用放射性碳分析对肖申克战役的考古层进行了测定.
- 修订该地区的铁器时代时间表,并将发现与其他古代文明相关联.
主要方法:
- 在以色列雷霍夫考古层的分层放射性碳测年.
- 对"所罗门"和"奥姆里德"时期的陶器风格的分析.
- 放射性碳年代与历史铭文和圣经文本的相关性.
主要成果:
- 一系列一致的放射性碳年代可追溯到公元前12世纪至公元前9世纪. 这是为雷霍夫工地获得的.
- 一个考古学层被成功地追溯到肖申克的战役.
- 这项研究表明",所罗门"和"奥姆里德"陶器之间存在相似之处.
- 放射性碳测年提供了与希腊和塞浦路斯的考古发现的相关性.
结论:
- 这些发现表明该地区的铁器时代时间表经过修订.
- 放射性碳测年提供了强有力的证据,证明肖申克的竞选活动影响了雷霍夫.
- 陶器分析支持年代相关性和地区之间的潜在文化交流.
相关概念视频
Isotopes
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, is a...
Global Climate Change
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
The Fossil Record
The fossil record documents only a small fraction of all organisms that have ever inhabited Earth. Fossilization is a rare process, and most organisms never become fossils. Moreover, the fossil record only exhibits fossils that have been discovered. Nevertheless, sedimentary rock fossils of long-lived, abundant, hard-bodied organisms dominate the fossil record. These fossils offer valuable information, such as an organism's physical form, behavior, and age. Studying the fossil record helps...
Elements: Chemical Symbols and Isotopes
A chemical symbol is an abbreviation used to indicate an element or an atom of an element. For example, the symbol for mercury is Hg. The same symbol is used to indicate one atom of mercury (microscopic domain) or to label a container of many atoms of the element mercury (macroscopic domain).
Some symbols are derived from the common English name of the element; others are abbreviations of the name in another language — Latin, Greek or German. For example, the symbol for aluminum (common name)...
Some symbols are derived from the common English name of the element; others are abbreviations of the name in another language — Latin, Greek or German. For example, the symbol for aluminum (common name)...
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...


