翻訳と辞書 Words near each other ・ Isotopes of arsenic ・ Isotopes of astatine ・ Isotopes of barium ・ Isotopes of berkelium ・ Isotopes of beryllium ・ Isotopes of bismuth ・ Isotopes of bohrium ・ Isotopes of boron ・ Isotopes of bromine ・ Isotopes of cadmium ・ Isotopes of caesium ・ Isotopes of calcium ・ Isotopes of californium ・ Isotopes of carbon ・ Isotopes of cerium ・ Isotopes of chlorine ・ Isotopes of chromium ・ Isotopes of cobalt ・ Isotopes of copernicium ・ Isotopes of copper ・ Isotopes of curium ・ Isotopes of darmstadtium ・ Isotopes of dubnium ・ Isotopes of dysprosium ・ Isotopes of einsteinium ・ Isotopes of erbium ・ Isotopes of europium ・ Isotopes of fermium ・ Isotopes of flerovium ・ Isotopes of fluorine Dictionary Lists mini英和辞書 mini和英辞書 Webster 1913 Latin-English FOLDOC Wikipedia English ウィキペディア

翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Isotopes of chlorine ： ウィキペディア英語版 Isotopes of chlorine Chlorine (Cl) has 24 isotopes with mass numbers ranging from 22Cl to 51Cl and 2 isomers (34mCl and 38mCl). There are two principal stable isotopes, 35Cl (75.78%) and 37Cl (24.22%), found in the relative proportions of 37.89:12.11, respectively, giving chlorine a standard mass number of 35.453. The longest-lived radioactive isotope is 36Cl, which has a half-life of 301,000 years. All other isotopes have half-lives under 1 hour, many less than one second. The shortest-lived are 29Cl and 30Cl, with half-lives less than 20 and 30 nanoseconds, respectively—the half-life of 28Cl is unknown. Standard atomic mass: 35.453(2) u ==Chlorine-36 (36Cl)== (詳細はradioactive 36Cl exist in the environment, in a ratio of about 7×10−13 to 1 with stable isotopes. 36Cl is produced in the atmosphere by spallation of 36Ar by interactions with cosmic ray protons. In the subsurface environment, 36Cl is generated primarily as a result of neutron capture by 35Cl or muon capture by 40Ca. 36Cl decays to either 36S (1.9%) or to 36Ar (98.1%), with a combined half-life of 308,000 years. The half-life of this hydrophilic nonreactive isotope makes it suitable for geologic dating in the range of 60,000 to 1 million years. Additionally, large amounts of 36Cl were produced by irradiation of seawater during atmospheric detonations of nuclear weapons between 1952 and 1958. The residence time of 36Cl in the atmosphere is about 1 week. Thus, as an event marker of 1950s water in soil and ground water, 36Cl is also useful for dating waters less than 50 years before the present. 36Cl has seen use in other areas of the geological sciences, forecasts, and elements. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Isotopes of chlorine」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.