Heinrichite
A valid IMA mineral species - grandfathered
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About Heinrichite
Formula:
Ba(UO2)2(AsO4)2 · 10H2O
Hardness:
2½
Crystal System:
Monoclinic
Member of:
Name:
Named in honor of Eberhardt "Abe" William Heinrich (10 February 1918, Braunschweig, Germany - 8 July 1991, Ann Arbor, Michigan, USA), mineralogist at the University of Michigan, USA.
Autunite Group.
Unstable at room temperature and dehydrates fairly rapidly to metaheinrichite (Walenta, 1965) which may be fully transparent. Most of the specimens shown on the photos here are probably metaheinrichite.
Unstable at room temperature and dehydrates fairly rapidly to metaheinrichite (Walenta, 1965) which may be fully transparent. Most of the specimens shown on the photos here are probably metaheinrichite.
Unique Identifiers
Mindat ID:
1848
Long-form identifier:
mindat:1:1:1848:3
Classification of Heinrichite
IMA Classification of Heinrichite
Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Ba(U6+O2)2(As5+O4)2·10H2O
First published:
1958
Type description reference:
8.EB.05
8 : PHOSPHATES, ARSENATES, VANADATES
E : Uranyl phosphates and arsenates
B : UO2:RO4 = 1:1
8 : PHOSPHATES, ARSENATES, VANADATES
E : Uranyl phosphates and arsenates
B : UO2:RO4 = 1:1
40.2a.4.1
40 : HYDRATED NORMAL PHOSPHATES,ARSENATES AND VANADATES
2a : AB2(XO4)2·xH2O, containing (UO2)2+
40 : HYDRATED NORMAL PHOSPHATES,ARSENATES AND VANADATES
2a : AB2(XO4)2·xH2O, containing (UO2)2+
20.7.12
20 : Arsenates (also arsenates with phosphate, but without other anions)
7 : Arsenates of U
20 : Arsenates (also arsenates with phosphate, but without other anions)
7 : Arsenates of U
Mineral Symbols
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Hrc | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Heinrichite
Hardness:
2½ on Mohs scale
Optical Data of Heinrichite
Type:
Uniaxial (-)
RI values:
nω = 1.605 nε = 1.573
Max. Birefringence:
δ = 0.032
Based on recorded range of RI values above.
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.
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:
Moderate (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).
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 uniaxial interference figure - the conoscopic
(convergent-light, Bertrand-lens-in) view, for a grain cut with the optic axis
centred and vertical. The coloured rings are isochromatics, computed with the
same physics as the Michel-Lévy bar above; the dark cross is the isogyre.
For a genuinely uniaxial mineral viewed this way, that cross stays perfectly stationary if you rotate the stage - unlike a biaxial mineral, where it splits apart on rotation. That invariance is itself the standard diagnostic test for telling uniaxial and biaxial minerals apart at the microscope.
For a genuinely uniaxial mineral viewed this way, that cross stays perfectly stationary if you rotate the stage - unlike a biaxial mineral, where it splits apart on rotation. That invariance is itself the standard diagnostic test for telling uniaxial and biaxial minerals apart at the microscope.
Chemistry of Heinrichite
Mindat Formula:
Ba(UO2)2(AsO4)2 · 10H2O
Element Weights:
Crystallography of Heinrichite
Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P2/b
Setting:
P2/c
Cell Parameters:
a = 7.1548(11) Å, b = 7.1340(11) Å, c = 21.290(3)(21) Å
β = 104.171(5)°
β = 104.171(5)°
Ratio:
a:b:c = 1.003 : 1 : 2.984
Unit Cell V:
1053.6 ų
Z:
2
Comment:
Data for synthetic material. Pseudotetragonal lattice.
Crystal Structure
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Data courtesy of the American Mineralogist Crystal Structure Database. Click on an AMCSD ID to view structure
| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0006009 | Heinrichite | Locock A J, Burns P C, Flynn T M (2005) Structures of strontium- and barium-dominant compounds that contain the autunite-type sheet The Canadian Mineralogist 43 721-733 | ![]() | 2005 | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 3.57 Å | (100) |
| 8.89 Å | (80) |
| 5.03 Å | (80) |
| 3.38 Å | (70) |
| 2.25 Å | (50) |
| 2.11 Å | (50) |
| 2.53 Å | (20) |
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 7: Great Oxidation Event | <2.4 |
| 47a : [Near-surface hydration of prior minerals] | |
| 47d : [Arsenates, antimonates, selenates, bismuthinates] | |
| 47f : [Uranyl (U⁶⁺) minerals] |
Type Occurrence of Heinrichite
Co-Type Localities:
Synonyms of Heinrichite
Other Language Names for Heinrichite
Relationship of Heinrichite to other Species
Member of:
Other Members of Autunite Group:
| Autunite | Ca(UO2)2(PO4)2 · 10-12H2O | Orth. mmm(2/m2/m2/m) : Pnma |
| Bassetite | Fe2+(UO2)2(PO4)2 · 10H2O | Mon. 2/m |
| Hydronováčekite | Mg(UO2)2(AsO4)2 · 12H2O | Tric. 1 : P1 |
| Kahlerite | Fe2+(UO2)2(AsO4)2 · 12H2O | Tet. 4/m : P42/n |
| Nováčekite | Mg(UO2)2(AsO4)2 · 10H2O | Mon. 2/m |
| Rauchite | Ni(UO2)2(AsO4)2 · 10H2O | Tric. 1 : P1 |
| Sabugalite | HAl(UO2)4(PO4)4 · 16H2O | Mon. 2/m : B2/m |
| Saléeite | Mg(UO2)2(PO4)2 · 10H2O | Mon. 2/m |
| Torbernite | Cu(UO2)2(PO4)2 · 12H2O | Tet. 4/mmm(4/m2/m2/m) : I4/mmm |
| Uranocircite | Ba(UO2)2(PO4)2 · 10H2O | Tet. |
| Uranospinite | Ca(UO2)2(AsO4)2 · 10H2O | Tet. 4/mmm(4/m2/m2/m) : P4/nmm |
| Zeunerite | Cu(UO2)2(AsO4)2 · 12H2O | Tet. 4/mmm(4/m2/m2/m) : I4/mmm |
Common Associates
Associations Based on Photo Data:
| 16 photos of Heinrichite associated with Arseniosiderite | Ca2Fe3+3(AsO4)3O2 · 3H2O |
| 14 photos of Heinrichite associated with Baryte | BaSO4 |
| 13 photos of Heinrichite associated with Abernathyite | K(UO2)(AsO4) · 3H2O |
| 9 photos of Heinrichite associated with Erythrite | Co3(AsO4)2 · 8H2O |
| 6 photos of Heinrichite associated with Hematite | Fe2O3 |
| 6 photos of Heinrichite associated with Quartz | SiO2 |
| 4 photos of Heinrichite associated with Goethite | Fe3+O(OH) |
| 4 photos of Heinrichite associated with Zeunerite | Cu(UO2)2(AsO4)2 · 12H2O |
| 3 photos of Heinrichite associated with Metaheinrichite | Ba(UO2)2(AsO4)2 · 8H2O |
| 1 photo of Heinrichite associated with Emplectite | CuBiS2 |
Related Minerals - Strunz-mindat Grouping
| 8.EB. | Meta-autunite Group | A1-2(UO2)2(TO4)2 · 5-10H2O |
| 8.EB.05 | Rauchite | Ni(UO2)2(AsO4)2 · 10H2O |
| 8.EB.05 | Uranocircite | Ba(UO2)2(PO4)2 · 10H2O |
| 8.EB.05 | Uranospinite | Ca(UO2)2(AsO4)2 · 10H2O |
| 8.EB.05 | Zeunerite | Cu(UO2)2(AsO4)2 · 12H2O |
| 8.EB.05 | Metarauchite | Ni(UO2)2(AsO4)2 · 8H2O |
| 8.EB.05 | Kahlerite | Fe2+(UO2)2(AsO4)2 · 12H2O |
| 8.EB.05 | Hydronováčekite | Mg(UO2)2(AsO4)2 · 12H2O |
| 8.EB.05 | Torbernite | Cu(UO2)2(PO4)2 · 12H2O |
| 8.EB.05 | Nováčekite | Mg(UO2)2(AsO4)2 · 10H2O |
| 8.EB.05 | Autunite | Ca(UO2)2(PO4)2 · 10-12H2O |
| 8.EB.05 | Saléeite | Mg(UO2)2(PO4)2 · 10H2O |
| 8.EB.05 | Xiangjiangite | (Fe3+,Al)(UO2)4(PO4)2(SO4)2(OH) · 22H2O |
| 8.EB.10 | Bassetite | Fe2+(UO2)2(PO4)2 · 10H2O |
| 8.EB.10 | Lehnerite | Mn2+(UO2)2(PO4)2 · 8H2O |
| 8.EB.10 | Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
| 8.EB.10 | Metasaléeite | Mg(UO2)2(PO4)2 · 8H2O |
| 8.EB.10 | Metauranocircite | Ba(UO2)2(PO4)2 · 7H2O |
| 8.EB.10 | Metauranospinite | Ca(UO2)2(AsO4)2 · 8H2O |
| 8.EB.10 | Metaheinrichite | Ba(UO2)2(AsO4)2 · 8H2O |
| 8.EB.10 | Metakahlerite | Fe2+(UO2)2(AsO4)2 · 8H2O |
| 8.EB.10 | Metakirchheimerite | Co(UO2)2(AsO4)2 · 8H2O |
| 8.EB.10 | Metanováčekite | Mg(UO2)2(AsO4)2 · 8H2O |
| 8.EB.10 | Metanatroautunite | Na(UO2)(PO4)(H2O)3 |
| 8.EB.10 | Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
| 8.EB.10 | Metazeunerite | Cu(UO2)2(AsO4)2 · 8H2O |
| 8.EB.10 | Przhevalskite | Pb2(UO2)3(PO4)2(OH)4 · 3H2O |
| 8.EB.10 | 'Pseudo-autunite' | (H3O)4Ca2(UO2)2(PO4)4 · 5H2O |
| 8.EB.15 | Abernathyite | K(UO2)(AsO4) · 3H2O |
| 8.EB.15 | Uramphite | (NH4)2(UO2)2(PO4)2 · 6H2O |
| 8.EB.15 | Meta-ankoleite | K2(UO2)2(PO4)2 · 6H2O |
| 8.EB.15 | Natrouranospinite | Na2(UO2)2(AsO4)2 · 5H2O |
| 8.EB.15 | Trögerite | (H3O)(UO2)(AsO4) · 3H2O |
| 8.EB.15 | Chernikovite | (H3O)2(UO2)2(PO4)2 · 6H2O |
| 8.EB.15 | Uramarsite | (NH4)(UO2)(AsO4) · 3H2O |
| 8.EB.20 | Chistyakovaite | Al(UO2)2(AsO4)2(F,OH) · 6.5H2O |
| 8.EB.20 | Threadgoldite | Al(UO2)2(PO4)2(OH) · 8H2O |
| 8.EB.25 | Uranospathite | (Al,◻)(UO2)2(PO4)2F · 20(H2O,F) |
| 8.EB.25 | Arsenuranospathite | Al(UO2)2(AsO4)2F · 20H2O |
| 8.EB.30 | Vochtenite | (Fe2+,Mg)Fe3+(UO2)4(PO4)4(OH) · 12-13H2O |
| 8.EB.35 | Coconinoite | Fe3+2Al2(UO2)2(PO4)4(SO4)(OH)2 · 20H2O |
| 8.EB.40 | Ranunculite | HAl(UO2)(PO4)(OH)3 · 4H2O |
| 8.EB.45 | Triangulite | Al3(UO2)4(PO4)4(OH)5 · 5H2O |
| 8.EB.50 | Furongite | Al13(UO2)7(PO4)13(OH)14 · 58H2O |
| 8.EB.55 | Arsenosabugalite | H0.5Al0.5(UO2)2(AsO4)2 · 8H2O |
| 8.EB.55 | Sabugalite | HAl(UO2)4(PO4)4 · 16H2O |
| 8.EB.60 | Horákite | (Bi7O7OH)[(UO2)4(PO4)2(AsO4)2(OH)2] · 3.5H2O |
Radioactivity
Other Information
Health Risks:
Radioactive.
Internet Links for Heinrichite
mindat.org URL:
https://www.mindat.org/min-1848.html
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References for Heinrichite
Reference List:
Gross, E. B., Corey, A. S., Mitchell, R. S., Walenta, K. (1958) Heinrichite and metaheinrichite, hydrated barium uranyl arsenate minerals. American Mineralogist, 43 (11-12) 1134-1143
Walenta, Kurt (1965) Beiträge zur Kenntnis seltener Arsenatmineralien unter besonderer Berücksichtigung von Vorkommen des Schwarzwaldes. 2. Folge [Rare arsenate minerals with special consideration of occurrences in the Black Forest. Part II]. Mineralogy and Petrology, 9 (3). 252-282 doi:10.1007/bf01128088
Frost, Ray L., Carmody, Onuma, Erickson, Kristy L., Weier, Matt L. (2005) Near-infrared spectroscopy to uranyl arsenates of the autunite and metaautunite group. Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy, 61 (8) 1923-1927 doi:10.1016/j.saa.2004.07.023
Locock, A. J., Burns, P. C., Flynn, T. M. (2005) Structures of strontium- and barium-dominant compounds that contain the autunite-type sheet. The Canadian Mineralogist, 43 (2) 721-733 doi:10.2113/gscanmin.43.2.721 (synthetic heinrichite)
Localities for Heinrichite
Showing 25 localities.
Locality List
- 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).
All localities listed without proper references should be considered as questionable.
France | |
| Cuchet et al. (2000) |
| - (1998) |
| Queneau (n.d.) |
| |
| - (1998) |
| Caubel (1997) +1 other reference |
Germany | |
| Walenta (1992) |
| Scharrer et al. (2020) +1 other reference |
| Walenta (1992) |
| |
| |
| Walenta (1992) | |
| Steffen Möckel probed 23/10/2005 |
| Walenta (1992) |
| Walenta (1992) |
| Lorenz (1998) +1 other reference |
| Heidtke (2001) |
| Trinkler (2010) |
| Lapis 30 (7/8) | |
Greece | |
| Rieck et al. (1999) |
| Simon et al. (2017) |
Poland | |
| Syczewski et al. (2023) |
Spain | |
| MTI Mineralogía Topográfica Ibérica |
USA (TL) | |
| Nevada Bureau of Mines and Geology NBMG ... +1 other reference |
| Anthony et al. (2000) |
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The
Schmiedestollen dump, Wittichen, Schenkenzell, Rottweil, Freiburg Region, Baden-Württemberg, Germany