|Name, Symbol, Number||Nickel, Ni, 28|
|Chemical series||Transition metals|
|Group, Period, Block||10 [?], 4 , d|
|Density, Hardness||8908 kg/m3, 4.0|
|Appearance||lustrous, metallic, silvery tinge|
|Atomic weight||58.6934 amu|
|Atomic radius (calc.)||135 (149) pm|
|Covalent radius||121 pm|
|van der Waals radius||163 pm|
|e- 's per energy level||2, 8, 16, 2|
|Oxidation states (Oxide)||2,3 (mildly basic)|
|Crystal structure||Cubic, face-centered|
|State of matter||solid (ferromagnetic)|
|Melting point||1728 K (2651 °F)|
|Boiling point||3186 K (5275 °F)|
|Molar volume||6.59 ×10-3 m3/mol|
|Heat of vaporization||370.4 kJ/mol|
|Heat of fusion||17.47 kJ/mol|
|Vapor pressure||237 Pa at 1726 K|
|Velocity of sound||4970 m/s at 293.15 K|
|Electronegativity||1.91 (Pauling scale)|
|Specific heat capacity||440 J/(kg*K)|
|Electrical conductivity||14.3 106/m ohm|
|Thermal conductivity||90.7 W/(m*K)|
|1st ionization potential||737.1 kJ/mol|
|2nd ionization potential||1753 kJ/mol|
|3rd ionization potential||3395 kJ/mol|
|4th ionization potential||5300 kJ/mol|
|Most Stable Isotopes|
|SI units & STP are used except where noted.|
Notable Characteristics Nickel is silvery white metal that takes on a high polish. It is of the iron group, and is hard, malleable, and ductile. It occurs combined with sulphur in millerite, with arsenic in the mineral niccolite, and with arsenic and sulphur in nickel glance.
On account of its permanence in air and inertness to oxidation, it is used in the smaller coins, for plating iron, brass, etc., for chemical apparatus, and in certain alloys, as german silver. It is magnetic, and is very frequently accompanied by cobalt, both being found in meteoric iron. It is chiefly valuable for the alloys it forms.
The most common oxidation_state of nickel is +2, though rarely, +1 and +3 Ni complexes are observed. Applications About 65% of the nickel consumed in the Western World is used to make austenitic stainless steel. Another 12% goes into superalloys. The remaining 23% of consumption is divided between alloy steels, rechargeable batteries, catalysts and other chemicals, coinage, foundry products, and plating.
Minerals containing nickel (e.g. kupfernickel, or false copper) were of value for coloring glass green. In 1751, Baron Axel Frederik Cronstedt was attempting to extract copper from kupfernickel (now called niccolite), and obtained instead a white metal that he called nickel.
The first nickel coin of the pure metal was made in 1881.
Biological Role Many but not all hydrogenases[?] contain nickel in addition to iron-sulfur clusters. Nickel centers are a common element in those hydrogenases whose function is to oxidize rather than evolve hydrogen. The nickel center appears to undergo changes in oxidation state, and evidence has been presented that the nickel center might be the active site of these enzymes.
A nickel-tetrapyrrole coenzyme, Co-F430, is present in the methyl CoM reductase and in methanogenic[?] bacteria. The tetrapyrrole is intermediate in structure between porphyrin and corrin. Changes in redox state, as well as changes in nickel coordination, have recently been observed.
There is also a nickel-containing carbon monoxide dehydrogenase. Little is known about the structure of the nickel site.
Occurrence The bulk of the nickel mined comes from two types of ore deposits. The first are laterites where the principal ore minerals are nickeliferous limonite [(Fe,Ni)O(OH)] and garnierite (a hydrous nickel silicate). The second are magmatic sulfide deposits where the principal ore mineral is pentlandite [(Ni,Fe)9S8].
In terms of supply, the Sudbury region of Ontario, Canada, produces about 30 percent of the world's supply of nickel. Other deposits are found in Russia, New Caledonia, Australia, Cuba, and Indonesia. However, most of the nickel on Earth is believed to be concentrated in the planet's core.
Isotopes Naturally occurring nickel is composed of 5 stable isotopes; 58-Ni, 60-Ni, 61-Ni, 62-Ni and 64-Ni with 58-Ni being the most abundant (68.077% natural abundance). 18 radioisotopes have been characterized with the most stable being 59-Ni with a half-life of 76,000 years, 63-Ni with a half-life of 100.1 years, and 56-Ni with a half-life of 6.077 days. All of the remaining radioactive isotopes have half-lifes that are less than 60 hours and the majority of these have half lifes that are less than 30 seconds. This element also has 1 meta state.
Nickel-59 is a long-lived cosmogenic radionuclide with a half-life of 76,000 years. 59Ni has found many applications in isotope geology[?]. 59Ni has been used to date the terrestrial age of meteorites and to determine abundances of extraterrestrial dust in ice and sediment. Nickel-60 is the daughter product of the extinct radionuclide 60Fe (half-life = 1.5 Myr). Because the extinct radionuclide 60Fe had such a long half-life, its persistence in solar_system materials at high enough concentrations may have generated observable variations in the isotopic composition of 60Ni. Therefore, the abundance of 60Ni present in extraterrestrial material may provide insight into the origin of the solar system and its early history.
Nickel carbonyl, [Ni(CO)4], is an extremely toxic gas.
Sensitized[?] individuals may show an allergy to nickel affecting their skin. The amount of nickel which is allowed in products which come into contact with human skin is regulated by the European Union. In 2002 a report in the journal Nature researchers found amounts of nickel being emitted by 1 and 2 euro coins far in excess of those standards. This is believed to be due to a galvanic reaction.