Scandium

Calcium - Scandium - Titanium Sc Y       Full table
General
Name, Symbol, Number	Scandium, Sc, 21
Chemical series	Transition metals
Group, Period, Block	3[?], 4 , d
Density, Hardness	2985 kg/m3, U/K
Appearance	Silvery white
Atomic Properties
Atomic weight	44.955910 amu
Atomic radius (calc.)	160 (184) pm
Covalent radius	144 pm
van der Waals radius	no data
Electron configuration	[Ar]3d1 4s2
e- 's per energy level	2, 8, 9, 2
Oxidation states (Oxide)	3 (weak base)
Crystal structure	Hexagonal
Physical Properties
State of matter	Solid (__)
Melting point	1814 K (2806 °F)
Boiling point	3103 K (5126 °F)
Molar volume	15.00 ×10-3 m3/mol
Heat of vaporization	314.2 kJ/mol
Heat of fusion	14.1 kJ/mol
Vapor pressure	22.1 Pa at 1812 K
Speed of sound	no data m/s at 293.15 K
Miscellaneous
Electronegativity	1.36 (Pauling scale)
Specific heat capacity	568 J/(kg*K)
Electrical conductivity	1.77 106/m ohm
Thermal conductivity	15.8 W/(m*K)
1st ionization potential	633.1 kJ/mol
2nd ionization potential	1235.0 kJ/mol
3rd ionization potential	2388.6 kJ/mol
4th ionization potential	7090.6 kJ/mol
5th ionization potential	8843 kJ/mol
6th ionization potential	10679 kJ/mol
7th ionization potential	13310 kJ/mol
8th ionization potential	15250 kJ/mol
9th ionization potential	17370 kJ/mol
10th ionization potential	21726 kJ/mol
Most Stable Isotopes
iso NA half-life DM DE MeV DP 45Sc 100% Sc is stable with 24 neutrons 46Sc {syn.} 83.79 days β- 2.367 46Ti
SI units & STP are used except where noted.

Scandium is a chemical element in the periodic table that has the symbol Sc and atomic number 21. A soft, silvery, white transition element, scandium occurs in rare minerals from Scandinavia and is is sometimes classified along with with yttrium and the lanthanides as a rare earth.

Table of contents 1 Notable Characteristics 2 Applications 3 History 4 Occurrence 5 Isotopes 6 Precautions 7 External Links

Notable Characteristics Scandium is a rare, soft, silvery, trivalent, very light metallic element that develops a slightly yellowish or pinkish cast when exposed to air. This element resembles yttrium and rare earth metals more than it resembles aluminum or titanium (which are closer on the periodic table). The most common oxidation state of scandium is +3 and this metal is not attacked by a 1:1 mixture of HNO₃ and 48% HF. Applications Approximately 20 kg of scandium (as Sc₂O₃) are used annually in the United States to make high-intensity lights. The radioactive isotope Sc-46 is used in oil refinery crackers as a tracing agent. When scandium iodide[?] is added to mercury vapor lamps[?] a highly efficient artificial sunlight-like light source is produced which is used in indoor or night-time color televisions. Scandium also has a much higher melting point than aluminum, and has been studied for possible use in spacecrafts. History Scandium (Latin Scandia meaning "Scandinavia") was discovered by Lars Fredrick Nilson[?] in 1879 while he and his team were looking for rare earth metals. Nilson used spectrum analysis to find the new element within the minerals euxenite and gadolinite. To isolate the element he processed 10 kilograms of euxenite with other rare-earth residues to obtain about 2 grams of very pure scandium oxide[?] (Sc₂O₃).

Dmitri Mendeleev, in 1869, predicted the existence and some properties of this element, which he called ekaboron, using his periodic law[?]. Per Theodor Cleve[?] discovered scandium oxide at about the same time as Nilson but unlike Nilson, Cleve determined that scandium was identical to ekaboron.

In 1937 metallic scandium was prepared for the first time by electrolysis of a eutectic melt of potassium, lithium, and scandium chlorides[?] at 700 to 800° C. Tungsten wire in a pool of liquid zinc were the electrodes in a graphite crucible. The first pound of 99% pure scandium metal wasn't produced until 1960. Occurrence Rare minerals from Scandinavia and Malagasy such as thortveitite, euxenite and gadolinite are the only known concentrated sources of this element (which is never found as a free metal).

Element 21 is the 23rd most abundant element in the sun and similar stars but on earth it is only the 50th most abundant element. Scandium is distributed widely on earth, occurring in trace quantities in over 800 minerals. The blue color of the aquamarine variety of beryl is thought to be caused by scandium. It is an important part of the rare mineral thortveitite and is found in residues that remain after tungsten is extracted from Zinnwald wolframite[?].

Thortveitite is the primary source of scandium with uranium mill tailings by-products also being an important source. Pure scandium is commercially produced by reducing scandium fluoride[?] with calcium metal. Isotopes Naturally occurring scandium is composed of 1 stable isotope Sc-45. 13 radioisotopes have been characterized with the most stable being Sc-46 with a half-life of 83.79 days, Sc-47 with a half-life of 3.3492 days, and Sc-48 with a half-life of 43.67 hours. All of the remaining radioactive isotopes have half-lifes that are less than 4 hours and the majority of these have half lifes that are less than 2 minutes. This element also has 5 meta states with the most stable being Scm-44 (t_½ 58.6 h).

The isotopes of scandium range in atomic weight from 39.978 amu (Sc-40) to 53.963 amu (Sc-54). The primary decay mode before the only stable isotope, Sc-45, is electron capture and the primary mode after is beta emission. The primary decay products before Sc-45 are element 20 (calcium) isotopes and the primary products after are element 22 (titanium) isotopes. Precautions Scandium metal powder is combustible and presents a fire hazard[?].

External Links

• WebElements.com - Scandium (http://www.webelements.com/webelements/elements/text/Sc/index)
• EnvironmentalChemistry.com - Scandium (http://environmentalchemistry.com/yogi/periodic/Sc)