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Magnesium oxide (Mg O), or magnesia, is a white hygroscopic solid mineral that occurs naturally as periclase and is a source of magnesium (see also oxide). It has an empirical formula of MgO and consists of a lattice of Mg 2+ ions and O 2− ions held together by ionic bonding .
Magnesium oxide and other magnesium compounds are also used in the agricultural, chemical, and construction industries. Magnesium oxide from calcination is used as an electrical insulator in fire-resistant cables. [15] Other applications include: Magnesium hydride is under investigation as a way to store hydrogen.
Lewis structure of a water molecule. Lewis structures – also called Lewis dot formulas, Lewis dot structures, electron dot structures, or Lewis electron dot structures (LEDs) – are diagrams that show the bonding between atoms of a molecule, as well as the lone pairs of electrons that may exist in the molecule.
In both, magnesium oxide is the precursor to magnesium metal. The magnesium oxide is produced as a solid solution with calcium oxide by calcining the mineral dolomite, which is a solid solution of calcium and magnesium carbonates: CaCO 3 ·MgCO 3 → MgO·CaO + 2 CO 2. Reduction occurs at high temperatures with silicon.
The structure of MgO 2 has been calculated as a triangular shape with the O 2 molecule binding side-on to the magnesium. This arrangement is a result of the Mg + donating charge to the oxygen and creating a Mg 2+ O 2 2−. The bond between to O 2 and the magnesium atom has an approximate dissociation energy of 90 kJ mol −1. [1]
Magnesium fluoride is an ionically bonded inorganic compound with the formula Mg F 2. The compound is a colorless to white crystalline salt and is transparent over a wide range of wavelengths , with commercial uses in optics that are also used in space telescopes .
The concept originated with Gilbert N. Lewis who studied chemical bonding. In 1923, Lewis wrote An acid substance is one which can employ an electron lone pair from another molecule in completing the stable group of one of its own atoms. [2] [17] The Brønsted–Lowry acid–base theory was published in the same year. The two theories are ...
The oxide layer can also be broken up using ultrasound, using a stirring rod to scratch the oxidized layer off, [6] or by adding a few drops of iodine or 1,2-Diiodoethane. Another option is to use sublimed magnesium or magnesium anthracene. [7] "Rieke magnesium" is prepared by a reduction of an anhydrous magnesium chloride with an potassium: