Q.Describe the occurrence (with one named ore each for chromium, manganese and iron) and the general physical characteristics of the first-row transition metals.
Transition metals occur in the earth's crust chiefly as oxide, sulfide and mixed-oxide ores, rather than in the free (native) state, since most of them are reactive enough to combine with atmospheric oxygen and other elements over geological time.
Chromium occurs almost entirely as chromite, , an iron-chromium spinel oxide; this is the sole industrial starting material for the manufacture of potassium dichromate, covered in detail later in this chapter. Manganese occurs chiefly as pyrolusite, , the starting material for the manufacture of potassium permanganate. Iron, the most abundant transition metal, occurs very widely as haematite, , and magnetite, .
General physical characteristics. Transition metals are, with only a few exceptions (notably the distinctive colours of copper and gold), hard, lustrous, silvery-white or grey solids at room temperature. They have comparatively high melting and boiling points and high enthalpies of atomization, because the inner d electrons -- in addition to the outer s electrons -- participate in the delocalized metallic bonding that holds the solid metal lattice together; the more unpaired d electrons available for this bonding, the stronger the metallic bond tends to be. They are excellent conductors of heat and electricity, are mechanically strong, and -- because their atoms across a given period are all of fairly comparable size (the radius varying only modestly across the series, as developed in a later section) -- they readily form alloys with one another and with other metals: steel (iron with chromium, manganese, nickel and others), brass (copper and zinc) and bronze (copper and tin) are everyday examples of this alloy-forming tendency.
Chromium occurs as chromite, ; manganese as pyrolusite, ; iron as haematite, (and magnetite, ). Transition metals in general are hard, lustrous, high-melting solids, good conductors of heat and electricity, and readily form alloys with one another because of their broadly similar atomic sizes.
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