Scheikundige formule: / (cire organique / organic wax)
Familie: Organische materialen
Status:
Mineraal om tentoon te stellen: Nee
UV Type | Kleur | Intensiteit | Frequentie van de observatie |
---|---|---|---|
Lange Golven (365nm): | Gelig wit | Middelmatig | Korte Golven(254 nm): | Gelig wit | Zwak |
Andere kleuren lange golven: | Blauw wit , Groen wit , | ||
Andere kleuren korte golven: | Blauw wit , Groen wit , |
Daglicht foto
Ozocerite,
Borislaw, Russie;
Col. G.Barmarin; Photo: G. Barmarin
Lange golf foto (365nm)
Ozocerite, UVLW
Borislaw, Russie;
Col. G.Barmarin; Photo: G. Barmarin
Korte golf foto (254nm)
Ozocerite, UVSW
Borislaw, Russie;
Col. G.Barmarin; Photo: G. Barmarin
Natural paraffin wax of dark color. Mostly composed of alkanes: CnH2n+2 n=20 to 40; melt around 50-60°C. Natural hydrocarbon mixtures of ozocerite and hatchettite as well as the terpenoid minerals fichtelite (norabietane) and hartite (α-phyllocladane) seems to have a luminescence under UV LW. Some of these hydrocarbons occur in soil and peat environments of Holocene age. However, hartite occurs in lignite, in fossilised Glyptostrobus (Taxodiaceae) trees and in pelosiderites of the Bílina Miocene series (about 20 Ma); it represents the accumulated and crystallised product of diagenetic transformation of precursor biogenic terpenoids. Raman spectra of earth waxes investigated confirm their dominantly aliphatic character and oxidative degradation (related to weathering and/or subaerial alteration in museum cabinets). Some quartz from Middleville, Town of Newport, Herkimer Co., New York, USA contain yellow inclusions of ozocerite strongly fluorescent.
Voornaamste Activator: Organische stof intrinsieke
Pieks in het spectrum (nm):
Broad band centered around 607nm with curve change at 525nm, 567nm, 607nm and 649nm
Col. G. Barmarin; Spectre: G. Barmarin
(*)Gegevens zijn niet exhaustieve, ze zijn beperkt tot de meest belangrijke plaatsen voor fluorescentie
http://www.mindat.org/show.php?name=Ozocerite
http://webmineral.com/data/Ozocerite.shtml
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