Introductory Chapter: Magnesium Alloys

T. Tański, M. Król
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Abstract

Magnesium is an element constituting 2.74% of the Earth’s crust. It occurs in most countries in the form of various compounds and minerals. The most common ores are dolomites (MgCO3·CaCO3) and magnesites (MgCO3). Another mineral used for the magnesium production is carnallite. Magnesium is also included in serpentine. Oceans are a rich source of magnesium, which contain approx. 0.13% of the metal in the salt solution as MgCl2 and MgSO4. In 1808, the electrolysis of molten salts allowed Humphrey Davy, an English chemist, to extract pure active metals for the first time, including magnesium [4–6].
导论章:镁合金
镁元素占地壳的2.74%。它以各种化合物和矿物质的形式存在于大多数国家。最常见的矿石是白云石(MgCO3·CaCO3)和菱镁矿(MgCO3)。另一种用于生产镁的矿物是光卤石。蛇纹石中也含有镁。海洋是镁的丰富来源,含镁量约为。盐溶液中0.13%的金属以MgCl2和MgSO4的形式存在。1808年,熔融盐的电解使英国化学家Humphrey Davy首次提取出纯活性金属,其中包括镁[4-6]。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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