[Minerals] [Gems] [Sale Items] [Gold Rings] [Big Stuff] [Main Page] Shop early for Holiday Season and get the best stuff. You can put it on layaway for up to six weeks! General Arapovite Information(U,Th)(Ca,Na)2(K1-x[ ]x)Si8O20•H2O, x=0.5 |
Molecular Weight = 897.66 gm |
|
Potassium 3.70 % K 4.46 % K2O |
|
Sodium 1.87 % Na 2.52 % Na2O |
|
Calcium 5.76 % Ca 8.06 % CaO |
|
Europium 0.17 % Eu 0.20 % Eu2O3 |
|
Lanthanum 0.15 % La 0.18 % La2O3 |
|
Cerium 0.47 % Ce 0.55 % Ce2O3 |
|
Samarium 0.17 % Sm 0.19 % Sm2O3 |
|
Dysprosium 0.18 % Dy 0.21 % Dy2O3 |
|
Thorium 9.31 % Th 10.59 % ThO2 |
|
Uranium 14.58 % U 16.54 % UO2 |
|
Silicon 25.03 % Si 53.55 % SiO2 |
|
Hydrogen 0.20 % H 1.79 % H2O |
|
Lead 0.69 % Pb 0.75 % PbO |
|
Neodymium 0.48 % Nd 0.56 % Nd2O3 |
|
Oxygen 37.23 % O |
|
______ ______ |
|
100.00 % 100.14 % = TOTAL OXIDE |
U0.55Th0.36Pb0.03Ce0.03Nd0.03La0.01Sm0.01Eu0.01Dy0.01Ca1.29Na0.73K0.85Si8O20·0.89(H2O) |
Steacyite group (4-membered double ring structure [Si8O20] unit. U4+ analogue of turkestanite and the U4+-Ca analogue of steacyite. |
Approved IMA 2004 (Dana # Added) |
Moraine of the Dara-i-Pioz glacier, the Alai mountain ridge, Tien-Shan Mountains, northern Tajikistan. Link to MinDat.org Location Data. |
Named for Yu. A. Arapov (1907-1988), a famous geologist and author of many works on the geochemistry, mineralogy and petrology of Middle Asia. |
IMA2003-046 |
| | Arapovite Image
|
|
Arapovite Crystallographya:c = 1:1.95171 |
a = 7.6506, c = 14.9318, Z = 2; V = 873.98 Den(Calc)= 3.41 |
Tetragonal - Ditetragonal DipyramidalH-M Symbol (4/m 2/m 2/m) Space Group: P 4/mcc |
By Intensity(I/Io): 3.37(1)(120), 2.64(0.64)(024), 3.31(0.58)(014),2.161(0.45)(224), 5.28(0.38)(012), 1.644(0.3)(242), 2.016(0.29)(232), 5.34(0.23)(100), 1.821(0.21)(234), |
|
Mouse
|
| Physical Properties of ArapoviteNone |
Dark green. |
Transparent |
Conchoidal - Fractures developed in brittle materials characterized by smoothly curving surfaces, (e.g. quartz). |
Inclusions - Generally found as inclusions in other minerals. |
Intergrown Crystals - Occurs as intergrown crystalline aggregates |
5.5-6 - Knife Blade-Orthoclase |
Vitreous - Resinous |
| Optical Properties of Arapovite CI calc= 0.033 (Excellent) - where the CI = (1-KPDcalc/KC) |
KPDcalc= 0.1796,KC= 0.1857 Ncalc = 1.63 Uniaxial (-), e=1.61, w=1.615, bire=0.0050. |
| Calculated Properties of ArapoviteBulk Density (Electron Density)=3.21 gm/cc |
note: Specific Gravity of Arapovite =3.41 gm/cc. Fermion Index = 0.01 |
Boson Index = 0.99 PEArapovite = 582.34 barns/electron |
U=PEArapovite x relectron=1,868.69 barns/cc. |
GRapi = 1,356,695.84 (Gamma Ray American Petroleum Institute Units)
Arapovite is Radioactive as defined in 49 CFR 173.403. Greater than 70 Bq / gram. Estimated Maximum U.S. Postal Shipping Size
(10 mRem/hr limit, Unshielded 10 cm box)
22.42 ± 5.60 grams of pure Arapovite .
Weight of pure Arapovite in grams (gm) and Calculated Diameter of a Sphere with a Density of 3.41 gm/cc.* | Arapovite Classification63.01.01.04 (63)Cyclosilicate Condensed Rings |
|
(63.01)4-membered rings |
|
(63.01.01)Steacyite Group |
|
|
|
|
09.CH.10 09 - SILICATES (Germanates) |
|
09.C - Cyclosilicates |
|
09.CH -[Si4O12]8- 4-membered double rings |
|
|
|
|
| Other Arapovite InformationNAME( CanMin, 42:1005) PHYS. PROP.(CanMin, 42:1005) |
Links to other databases for Arapovite : |
1 - Am. Min. Crystal Structure Database 2 - Athena 3 - Google Images 4 - Google Scholar 5 - MinDAT 6 - MinMax(Deutsch) 7 - MinMax(English) 8 - Mineralienatlas (Deutsch) 9 - QUT Mineral Atlas 10 - Ruff.Info Search for Arapovite using: Visit our Advertisers for Arapovite : AA Mineral SpecimensB & L Fine Minerals Crystalarium.com Dan Weinrich Fine Minerals Dan Weinrich Auctions Dakota Matrix Desert Winds Gems and Minerals Excalibur Minerals Exceptional Minerals Fabre Minerals Heliodor John Betts Fine Minerals Mason's Minerals Mineral News Mineral of the Month Club Wrights Rock Shop Translate Arapovite Mineral Data : Ask about Arapovite here : Print or Cut-and-Paste your Arapovite Specimen Label here :
| |
|
| | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||