Symbol | Ti |
Atomnummer | 22 |
Gruppe | 4 (Titangruppe) |
Periode | 4 |
Blok | d |
Klassifikation | Overgangsmetal |
Udseende | Silvery grey-white metallic |
Farve | Sølv |
Antal protoner | 22 p+ |
Antal neutroner | 26 n0 |
Antal elektroner | 22 e- |
Fase ved STP | Fast |
Massefylde | 4.506 g/cm3 |
Atommasse | 47.8671 u |
Smeltepunkt | 1941 K 1667.85 °C 3034.13 °F |
Kogepunkt | 3560 K 3286.85 °C 5948.33 °F |
Fordampningsvarme | 425.2 kJ/mol |
Elektronegativitet (Pauling Scale) | 1.54 |
Elektronaffinitet | 7.289 kJ/mol |
Oxidationstrin | −2, −1, 0, +1, +2, +3, +4 (an amphoteric oxide) |
Ioniseringsenergier |
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Opdaget | William Gregor (1791) |
Første isolation | Jöns Jakob Berzelius (1825) |
Navngivet af | Martin Heinrich Klaproth (1795) |
Opdagelse af titan Titanium was discovered in 1791 by the clergyman and geologist William Gregor as an inclusion of a mineral in Cornwall, Great Britain. Gregor recognized the presence of a new element in ilmenite when he found black sand by a stream and noticed the sand was attracted by a magnet. Analyzing the sand, he determined the presence of two metal oxides: iron oxide (explaining the attraction to the magnet) and 45.25% of a white metallic oxide he could not identify. Realizing that the unidentified oxide contained a metal that did not match any known element, in 1791 Gregor reported his findings in both German and French science journals:Crell's Annalen and Observations et Mémoires sur la Physique. Around the same time, Franz-Joseph Müller von Reichenstein produced a similar substance, but could not identify it. The oxide was independently rediscovered in 1795 by Prussian chemist Martin Heinrich Klaproth in rutile from Boinik (the German name of Bajmócska), a village in Hungary (now Bojničky in Slovakia). Klaproth found that it contained a new element and named it for the Titans of Greek mythology. After hearing about Gregor's earlier discovery, he obtained a sample of manaccanite and confirmed that it contained titanium. |