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Villyaellenite

A valid IMA mineral species
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About VillyaelleniteHide

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Villy Aellen
Formula:
(Mn,Ca)Mn2Ca2(AsO3OH)2(AsO4)2 · 4H2O
Colour:
Colorless, orange to light pink
Lustre:
Sub-Vitreous, Resinous
Hardness:
4
Specific Gravity:
3.20
Crystal System:
Monoclinic
Name:
Named by H. Sarp in 1984 after Villy Aellen, (1926, Neuchâtel, Switzerland - 2000), zoologist and former Director of the Natural History Museum of Geneva (Switzerland).
Isostructural with:
Compare giftgrubeite, the ordered (Ca:Mn = 3:2) intermediate member between villyaellenite and sainfeldite.

See also the closely related miguelromeroite. Note: The miguelromeroite samples from the Veta Negra mine, Chile, were originally labeled "villyaellenite".




Unique IdentifiersHide

Mindat ID:
4182
Long-form identifier:
mindat:1:1:4182:5

IMA Classification of VillyaelleniteHide

Approved
IMA Formula:
(Mn2+,Ca)Mn2+2Ca2(As5+O4)2(As5+O3OH)2·4H2O
Approval year:
1983
First published:
1984

Classification of VillyaelleniteHide

8.CB.10

8 : PHOSPHATES, ARSENATES, VANADATES
C : Phosphates without additional anions, with H2O
B : With only medium-sized cations, RO4:H2O = 1:1
39.2.1.3

39 : HYDRATED ACID PHOSPHATES,ARSENATES AND VANADATES
2 : (AB)5[HXO4]2[XO4]2.xH2O
20.8.20

20 : Arsenates (also arsenates with phosphate, but without other anions)
8 : Arsenates of Mn

Mineral SymbolsHide

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

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

Physical Properties of VillyaelleniteHide

Sub-Vitreous, Resinous
Transparency:
Transparent, Translucent
Colour:
Colorless, orange to light pink
Streak:
White
Hardness:
Tenacity:
Brittle
Cleavage:
Distinct/Good
{100} good
Density:
3.20 g/cm3 (Measured)    3.24 g/cm3 (Calculated)
Comment:
D as high as 3.72, Am Min (1988): 73:1172

Optical Data of VillyaelleniteHide

Type:
Biaxial (-)
RI values:
nα = 1.660 - 1.713 nβ = 1.670 - 1.723 nγ = 1.676 - 1.729
2V:
Measured: 70.5° to 76°, Calculated: 75° to 75.6°
Birefringence:
0.016
Max. Birefringence:
δ = 0.016
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. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
weak
Optical Extinction:
Y ^ c = 30°-40°.
Pleochroism:
Visible
Comments:
X=very pale orange pink, Y=exceedingly pale pink, Z=pale orange pink; Z>>X>Y.
Comments:
Higher optics may represent closeness to end-member.

Chemistry of VillyaelleniteHide

Mindat Formula:
(Mn,Ca)Mn2Ca2(AsO3OH)2(AsO4)2 · 4H2O
Element Weights:
Element% weight
O36.582 %
As34.261 %
Mn18.842 %
Ca9.164 %
H1.152 %

Calculated from ideal end-member formula.
O
As
Mn
Ca
H
Common Impurities:
Zn,Ca,Fe

Crystallography of VillyaelleniteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
B2/b
Setting:
C2/c
Cell Parameters:
a = 18.55 Å, b = 9.50 Å, c = 9.99 Å
β = 96.94°
Ratio:
a:b:c = 1.953 : 1 : 1.052
Unit Cell V:
1,747.59 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Rosettes of prismatic crystals, elongated || [001], tabular || {100}.

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
8.21 Å(50)
4.45 Å(30)
3.24 Å(50)
3.21 Å(100)
3.13 Å(30)
3.06 Å(70)
2.98 Å(40)
2.34 Å(30)
Comments:
ICDD 41-1455, also 37-444.

Geological Environment