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| Alum-(K) is named from the
Latin word alumen for aluminum since it
is the potassium double sulfate of aluminum and the
-(K) suffix denotes that it is the K-dominant member
of the Alum Group.
| Discovered
in 1875;
IMA
status:
Valid (pre-IMA; Grandfathered) |
|
Chemistry
|
|
|
Chemical
Formula: |
KAl(SO4)2·12(H2O) |
|
Hydrated
Potassium Aluminum Sulfate |
Molecular
Weight: |
474.39 gm |
Composition: |
Potassium |
8.24 % |
K |
9.93 % |
K2O |
|
Aluminum |
5.69 % |
Al |
10.75 % |
Al2O3 |
|
Hydrogen |
5.10 % |
H |
45.57 % |
H2O |
|
Sulfur |
13.52 % |
S |
33.75 % |
SO3 |
|
Oxygen |
67.45 % |
O |
|
|
|
|
100.00 % |
|
100.00 % |
= TOTAL OXIDE |
|
|
Classification
|
|
|
Mineral
Classification: |
Sulfates
|
Strunz 8th
Ed. ID:
|
6/C.14-20
|
Nickel-Strunz 10th
Ed. ID:
|
7.CC.20
|
|
7 : SULFATES (selenates, tellurates, chromates, molybdates,
wolframates) C : Sulfates (selenates, etc.) without additional anions, with
H2O
C : With medium-sized and large cations
|
Related
to: |
Alum
Group. Sodium Alum - Zincovoltaite Series.
|
Members
of Group: |
Alum
Group: Alum-(K), Alum-(Na), Lanmuchangite, Tschermigite
|
Varieties: |
None
|
Synonyms: |
Native
Alum, Potassium Alum,
Potash Alum, Tawas
|
|
|
Crystal
Data
|
|
|
Crystallography:
|
Isometric
- Diploidal
|
Crystal
Habit:
|
Rarely
as tiny octahedral crystals, if precipitated from pure water solution; cubic from
alkaline solutions. Commonly stalactitic, columnar, granular, or massive efflorescences.
|
Twinning:
|
Very rare;
on {111}
|
|
|
Physical
Properties
|
|
|
Cleavage: |
{111}
Poor/Indistinct, Interrupted
|
Fracture: |
Conchoidal
|
Tenacity:
|
Brittle
|
Moh's
Hardness: |
2.0
- 2.5
|
Density:
|
1.757 (g/cm3)
|
Luminescence:
|
None
|
Radioactivity:
|
Barely
Detectable;
GRapi = 124.32 (Gamma Ray American Petroleum Institute Units)
|
Other: |
Soluble in water,
taste sweetish and astringent; deliquesces at 91º C
|
|
|
Optical
Properties
|
|
|
Color: |
Colorless,
White; Colorless in transmitted light
|
Transparency: |
Transparent
to Translucent |
Luster: |
Vitreous
|
Refractive
Index: |
1.456
Isotropic
|
Birefringence: |
None
(Isotropic); may be weakly anomalously birefringent
and sectored
|
Dispersion: |
n/a
|
Pleochroism: |
None
|
|
|
Occurances
|
|
|
Geological
Setting: |
Formed
from argillaceous rocks or coal containing oxidizing
pyrite or marcasite; may be a fumarolic or solfataric
precipitate. |
Common
Associations: |
Alunogen,
Gypsum, Epsomite, Melanterite, Pickeringite, Sulfur
|
Common
Impurities: |
None
|
Type
Locality: |
Possibly
Alum Grotto, Porto Levante, Vulcano Island, Eolie Islands
(Aeolian Islands), Lipari, Messina Province, Sicily,
Italy |
Year
Discovered: |
1875
|
View
mineral photos: |
Potassium
Alum
Mineral Photos and Locations |
|
|
More
Information
|
|
|
|
Mindat.org
Webmineral.com
|
|
|
Alum-(K) (also known as Potassium
Alum) is a sulfate
mineral that is very rarely available as a faceted gem.
It is a very unusual mineral in that it is both barely
radioactive
and water
soluble. It was originally named Potassium Alum
but was renamed to Alum-(K) by Mineralogical Record, v39 (2008), p131
to indicate that it is the K-dominant member of the
Alum Group. Alum-(K) is commonly used in water purification, leather tanning, and
fireproofing textiles. It also has cosmetic uses as an
ingredient in deodorant and as an aftershave treatment
due to its astringent
qualities.
There
are very few localities to find gem quality crystals
of Alum-(K). A few of these are the El Desierto mine, San Pablo de Napa, Daniel Campos
Province, Potosí Department, Bolivia; Alaunhöhle, near Dresden, Saxony, Germany;
Alum mine, Alum District, Esmeralda County, Nevada,
USA; Alum King Mine, Marysvale District (Marysvale Uranium
area), Piute County, Utah, USA.
|
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