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Kanemite

A valid IMA mineral species
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About KanemiteHide

Formula:
HNaSi2O5 · 3H2O
Colour:
Colorless to cloudy white; light tan possibly due to inclusions
Lustre:
Sub-Vitreous, Resinous, Waxy, Greasy
Hardness:
4
Specific Gravity:
1.93
Crystal System:
Orthorhombic
Name:
Named in 1972 by Gilbert Maglione and Z. Johan after the type locality at Andajia, Kanem (Khanem) Region, Lake Chad, Chad.
Cleaved aggregates may appear similar to gypsum.

May dehydrate to Unnamed (Kanemite-related mineral).


Unique IdentifiersHide

Mindat ID:
2152
Long-form identifier:
mindat:1:1:2152:0

IMA Classification of KanemiteHide

Approved
IMA Formula:
NaSi2O4(OH) · 3H2O
First published:
1972

Classification of KanemiteHide

9.EF.25

9 : SILICATES (Germanates)
E : Phyllosilicates
F : Single nets with 6-membered rings, connected by M[4], M[8], etc.
73.1.5.1

73 : PHYLLOSILICATES Condensed Tetrahedral Sheets
1 : Condensed Tetrahedral Sheets with double layers

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference
KnmIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of KanemiteHide

Sub-Vitreous, Resinous, Waxy, Greasy
Transparency:
Transparent
Colour:
Colorless to cloudy white; light tan possibly due to inclusions
Streak:
White
Hardness:
Hardness Data:
Measured
Tenacity:
Brittle
Cleavage:
Perfect
{010} perfect; {100} good
Density:
1.93 g/cm3 (Measured)    1.933 g/cm3 (Calculated)

Optical Data of KanemiteHide

Type:
Biaxial (-)
RI values:
nα = 1.451(2) nβ = 1.470(2) nγ = 1.478(2)
2V:
Measured: 46° , Calculated: 64°
Birefringence:
0.027
Max. Birefringence:
δ = 0.027
Based on recorded range of RI values above.

Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.

Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.

Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars.

Surface Relief:
Moderate
Dispersion:
r > v distinct
Optical Extinction:
parallel, XYZ = bac
Pleochroism:
Non-pleochroic

Chemistry of KanemiteHide

Mindat Formula:
HNaSi2O5 · 3H2O
Element Weights:
Element% weight
O59.752 %
Si26.222 %
Na10.732 %
H3.294 %

Calculated from ideal end-member formula.
Common Impurities:
Al,Ca,K

Crystallography of KanemiteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm (2/m 2/m 2/m) - Dipyramidal
Space Group:
Pnma
Cell Parameters:
a = 7.282 Å, b = 20.507 Å, c = 4.956 Å
Ratio:
a:b:c = 0.355 : 1 : 0.242
Unit Cell V:
740.09 ų (Calculated from Unit Cell)
Z:
4
Comment:
Pnmb

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0002274KanemiteGarvie L A J, Devouard B, Groy T L, Camara F, Buseck P R (1999) Crystal structure of kanemite, NaHSi2O5.3H2O, from the Aris phonolite, Namibia American Mineralogist 84 1170-117519990293
0006765KanemiteVortmann S, Rius J, Marler B, Gies H (1999) Structure solution from powder data of the hydrous layer silicate kanemite, a precursor of the industrial ion exchanger SKS-6 European Journal of Mineralogy 11 125-13419990293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
10.3 Å(100)
4.01 Å(100)
3.44 Å(90)
3.16 Å(70)
3.09 Å(70)
2.48 Å(80)
2.39 Å(60)
2.00 Å(50)
Comments:
Originally described as monoclinic.

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
25 : Evaporites (prebiotic)
Stage 4b: Highly evolved igneous rocks>3.0
35 : Ultra-alkali and agpaitic igneous rocks
Geological Setting:
Evaoprites

Type Occurrence of KanemiteHide

General Appearance of Type Material:
Spherical aggregates, generally < 0.3 mm. The surface of the aggregates may show etched to incised surface markings.
Place of Conservation of Type Material:
National School of Mines, Paris, France.
National Museum of Natural History, Washington, D.C., USA, 123219, 142501.
Geological Setting of Type Material:
Interdunary depression. Evaporite.
Associated Minerals at Type Locality:

Synonyms of KanemiteHide

Other Language Names for KanemiteHide

Dutch:Kanemiet
German:Kanemit
Spanish:Kanemita

Common AssociatesHide

Associated Minerals Based on Photo Data:
4 photos of Kanemite associated with TuperssuatsiaiteFe3+Fe3+2(Na◻)◻2Si8O20(OH)2(H2O)4 · 2H2O
3 photos of Kanemite associated with NatroliteNa2Al2Si3O10 · 2H2O
2 photos of Kanemite associated with VilliaumiteNaF
1 photo of Kanemite associated with Unnamed (Fe-analogue of Zakharovite)Na4Fe5Si10O24(OH)6 · 6H2O
1 photo of Kanemite associated with CryoliteNa2NaAlF6

Related Minerals - Strunz-mindat GroupingHide

9.EF.05PetaliteLiAl(Si4O10)Mon. 2/m : P2/b
9.EF.10SanborniteBaSi2O5Orth. mmm (2/m 2/m 2/m)
9.EF.15SearlesiteNa(H2BSi2O7)Mon. 2 : P21
9.EF.20SilinaiteNaLiSi2O5 · 2H2OMon. 2/m
9.EF.30Yakovenchukite-(Y)K3NaCaY2[Si12O30] · 4H2OOrth. mmm (2/m 2/m 2/m) : Pcca

Fluorescence of KanemiteHide

Not fluorescent

Other InformationHide

Notes:
Dilute HCl removes sodium, leaving a hydrated silica.
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

Internet Links for KanemiteHide

References for KanemiteHide

Reference List:

Localities for KanemiteHide

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.

Locality ListHide

- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).

All localities listed without proper references should be considered as questionable.
Chad (TL)
 
  • Lac Region
Johan et al. (1972)
India
 
  • Madhya Pradesh
    • Betul Belt
Shukla et al. (2021)
Kenya
 
  • Baringo County
Périnet et al. (1982)
Namibia
 
  • Khomas Region
    • Windhoek Rural
      • Aris
... +3 other references
Russia
 
  • Murmansk Oblast
    • Lovozersky District
Pekov (2000)
        • Umbozero mine
Igor Pekov analysis
 
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