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  • Article - 3 May 2013
    Magnesium is a silvery-white metal used as an alloy element for aluminum, lead, zinc and other nonferrous alloys. Magnesium QH21A-T6 alloy is pressure tight, and has good castability, high yield...
  • Article - 2 May 2013
    Magnesium is among the most abundantly available elements in the earth’s crust. It has a silvery-white appearance and is commonly alloyed with aluminum, zinc, lead and other non-ferrous metals.
  • Article - 13 Aug 2013
    Magnesium is the eighth most abundant element present in the earth’s crust, most of it is dissolved in sea water. Application of magnesium is restricted by its property to be easily ignited (both in...
  • Article - 16 Jul 2013
    Magnesium is a silvery-white metal that is used as an alloy element for lead, aluminum, zinc, and other non-ferrous alloys. Magnesium alloys have high impact resistance, low inertia, and good damping...
  • Article - 16 Jul 2013
    Magnesium is a silvery-white metal that is used as an alloy element for zinc, lead, aluminum, and other non-ferrous alloys. Magnesium alloys are light weight with high machinability.
  • Article - 13 Aug 2013
    Magnesium is found in about 60 minerals. However, minerals like olivine, talc, carnallite, brucite, magnesite and dolomite are only of commercial importance. The metal derived its name from the Greek...
  • Article - 19 Apr 2013
    Silver sulfide is a dense black solid that is insoluble in all solvents, but is degraded by strong acids. It features a covalent bond, as it is made up of silver and sulfur.
  • Article - 14 Aug 2013
    Aluminum arsenide is a semiconductor material that has almost the same lattice constant as that of gallium arsenide. It can form a superlattice with gallium arsenide which results in its semiconductor...
  • Article - 22 Aug 2013
    Silver gallium sulfide has high short wavelength transparency edging at 550nm, excellent bulk quality across the transmission range, except for residual e-ray absorption centered at 1.8µm. Surface...
  • Article - 21 Aug 2013
    Copper (II) oxide is a higher oxide of copper and belongs to the monoclinic crystal system. It occurs as a black solid with an ionic structure that melts above 1200°C with some loss of oxygen.

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