镧系元素,稀土元素

W. Wells, Vickie L. Wells
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引用次数: 13

摘要

镧系元素(或镧系元素)是一组原子序数从57到71的15种元素,其中有时包括钪(原子序数21)和钇(原子序数39)。镧系系是指在元素周期表的IIIB族列位中紧跟镧之后的一组化学元素。它们独特的原子特征是它们填满了4f电子亚层。实际上,只有那些原子序数为58-71的元素才是镧系元素。大多数化学家还把镧也包括在这个系列中,因为尽管它不填满4f亚壳层,但它的性质与镧系元素非常相似。元素钪和钇也被称为“稀土”,因为它们最初是与稀有矿物中的镧系元素一起被发现的,并作为氧化物或“地球”被分离出来。这些金属统称为稀土元素(ree)。然而,与许多其他元素相比,稀土其实并不稀有,除了只有放射性同位素的钷。钇、镧、铈和钕在地壳中的含量都比铅丰富。除了自然界中可能不存在的钷以外,其他元素的含量都比镉高。给出了相对丰度和原子序数。更常见的镧系化合物在第1节中列出。钪是一种银白色的金属化学元素,是元素周期表中第一个过渡金属系列的第一个成员。这个名字来源于斯堪的纳维亚半岛,在那里,这种元素是在矿物永长石和钆长石中发现的。1876年,l·f·尼尔森制备了约2g的高纯氧化钪。随后确定钪对应于门捷列夫根据元素周期表中的一个间隙所预测的元素“ekaboron”。钪少量存在于800多种矿物中,使海蓝宝石呈现蓝色。钇是四种化学元素中的一种(其他三种是铒、铽和镱),它是以瑞典一个盛产稀有矿物和稀土的村庄Ytterby命名的。钇是一种具有银色光泽的金属,其性质与稀土金属非常相似。它是第二系列过渡金属的第一个成员。钇存在于几种矿物中,主要由矿物材料xenotime产生。镧是一种白色的、可延展的金属;它是过渡金属第三系的第一个成员,也是稀土的第一个成员。镧与其他镧系元素一起存在于矿石独居石、氟碳铈矿和钇铝钇石以及其他矿物中。1839年,瑞典化学家Carl G. Mosander发现了它。科学家们已经制造出许多镧的放射性同位素。关键词:铈;氯化物;镝;铒;铕;钆;肾脏;镧系元素;镧;肝;肺;独居石;钕;硝酸盐;氧化物;钪;铽;镱;钇
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Lanthanides, Rare Earth Elements
The lanthanides (or lanthanons) are a group of 15 elements of atomic numbers from 57 through 71 in which scandium (atomic number 21) and yttrium (atomic number 39) are sometimes included. The lanthanide series proper is that group of chemical elements that follow lanthanum in its group IIIB column position of the periodic table. Their distinguishing atomic feature is that they fill the 4f electronic subshell. Actually, only those elements with atomic numbers 58–71 are lanthanides. Most chemists also include lanthanum in the series because, although it does not fill the 4f subshell, its properties are very much like those of the lanthanides. The elements scandium and yttrium are also known as the “rare earths” because they were originally discovered together with the lanthanides in rare minerals and isolated as oxides, or “earths.” Collectively, these metals are also called rare earth elements (REEs). In comparison with many other elements, however, the rare earths are not really rare, except for promethium, which has only radioactive isotopes. Yttrium, lanthanum, cerium, and neodymium are all more abundant than lead in the earth's crust. All except promethium, which probably does not occur in nature, are more abundant than cadmium. The relative abundance and atomic numbers are provided. The more common lanthanide compounds are listed in Section 1. Scandium is a silvery white metallic chemical element, the first member of the first transition-metal series in the periodic table. The name is derived from Scandinavia, where the element was discovered in the minerals euxenite and gadolinite. In 1876, L. F. Nilson prepared about 2 g of high purity scandium oxide. It was subsequently established that scandium corresponds to the element “ekaboron,” predicted by Mendeleyev on the basis of a gap in the periodic table. Scandium occurs in small quantities in more than 800 minerals and causes the blue color of aquamarine beryl. Yttrium is one of the four chemical elements (the others are erbium, terbium, and ytterbium) named after Ytterby, a village in Sweden that is rich in unusual minerals and rare earths. Yttrium is a metal with a silvery luster and properties closely resembling those of rare earth metals. It is the first member of the second series of transition metals. Yttrium is found in several minerals and is produced primarily from the ore material xenotime. Lanthanum is a white, malleable metal; it is the first member of the third series of transition metals, and the first of the rare earths. Lanthanum is found with other lanthanides in the ore minerals monazite, bastnaesite, and xenotime, and in other minerals. It was discovered in 1839 by the Swedish chemist Carl G. Mosander. Scientists have created many radioactive isotopes of lanthanum. Keywords: cerium; chlorides; dysprosium; erbium; europium; gadolinium; kidneys; lanthanides; lanthanum; liver; lungs; monazite; neodymium; nitrates; oxides; scandium; terbium; ytterbium; yttrium
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