Oxidization zone of nickel-bearing hydrothermal mineral deposits, formed from H2O solution between 31.5 deg C and 53.5 deg C. Dimorphous with nickelhexahydrite.
IMA Status:
Valid Species (Pre-IMA) 1949
Locality:
Cottonwood Canyon, Nevada. Link to MinDat.org Location Data.
Name Origin:
Named for Jan Willem Retgers (1856-1896), Dutch physical chemist and chemical crystallographer.
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Physical Properties of Retgersite
Cleavage:
{001} Perfect
Color:
Dark green.
Density:
2.07
Fracture:
Brittle - Uneven - Very brittle fracture producing uneven fragments.
Hardness:
2.5 - Finger Nail
Luster:
Vitreous (Glassy)
Streak:
greenish white
Optical Properties of Retgersite
Gladstone-Dale:
CI meas= 0.011 (Superior) - where the CI = (1-KPDmeas/KC) CI calc= 0.016 (Superior) - where the CI = (1-KPDcalc/KC)
KPDcalc= 0.24,KPDmeas= 0.2411,KC= 0.2437 Ncalc = 1.5 - 1.51
Optical Data:
Uniaxial (-), e=1.4873, w=1.5109, bire=0.0236.
Calculated Properties of Retgersite
Electron Density:
Bulk Density (Electron Density)=2.14 gm/cc note: Specific Gravity of Retgersite =2.07 gm/cc.
Fermion Index:
Fermion Index = 0.0037371925 Boson Index = 0.9962628075
Photoelectric:
PERetgersite = 9.24 barns/electron U=PERetgersite x rElectron Density= 19.80 barns/cc.
Radioactivity:
GRapi = 0 (Gamma Ray American Petroleum Institute Units) Retgersite is Not Radioactive