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Larderellite

A valid IMA mineral species - grandfathered
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About LarderelliteHide

07823770017271924639673.jpg
François (Francesco) de Larderel
Formula:
(NH4)B5O7(OH)2 · H2O
Colour:
White, yellowish due to impurities; colourless in transmitted light
Specific Gravity:
1.905
Crystal System:
Monoclinic
Name:
Named in 1853 by E. Bechi in honor of François Jacques (Francesco Giacomo) de Larderel (5 August 1790, Vienne, Isère, France - 15 June 1858, Florence, Italy), an engineer and entrepreneur who promoted the industrial exploitation of geothermal vents in Tuscany, producing boric acid. He became the principal operator of the Tuscan borax works.
Dimorph of:
This page provides mineralogical data about Larderellite.


Unique IdentifiersHide

Mindat ID:
2332
Long-form identifier:
mindat:1:1:2332:6

IMA Classification of LarderelliteHide

Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
N3-H4B5O7(OH)2·H2O

Classification of LarderelliteHide

6.EB.05

6 : BORATES
E : Pentaborates
B : Ino-pentaborates
26.5.4.1

26 : HYDRATED BORATES CONTAINING HYDROXYL OR HALOGEN
5 : Pentaborates
9.1.14

9 : Borates
1 : Borates of the alkalis and boric acid

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

Physical Properties of LarderelliteHide

Transparency:
Translucent
Colour:
White, yellowish due to impurities; colourless in transmitted light
Streak:
White
Cleavage:
Perfect
On {001} (?) and {010} (?).
Density:
1.905(4) g/cm3 (Measured)    1.887 g/cm3 (Calculated)

Optical Data of LarderelliteHide

Type:
Biaxial (+)
RI values:
nα = 1.493(1) nβ = 1.509(1) nγ = 1.561(1)
2V:
Measured: 58° , Calculated: 56°
Max. Birefringence:
δ = 0.068
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:
Low (negative)
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:
none

Chemistry of LarderelliteHide

Mindat Formula:
(NH4)B5O7(OH)2 · H2O
Element Weights:
Element% weight
O67.760 %
B22.893 %
N5.932 %
H3.415 %

Calculated from ideal end-member formula.
O
B
N
H

Crystallography of LarderelliteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/b
Setting:
P21/a
Cell Parameters:
a = 11.64(1) Å, b = 7.62(1) Å, c = 9.45(1) Å
β = 96.75°
Ratio:
a:b:c = 1.528 : 1 : 1.24
Unit Cell V:
832.37 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Microscopic rhomboidal tablets flattened {100}. The acute plane angle of the rhombs is ~ 68°.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0009364LarderelliteMerlino S, Sartori F (1969) The crystal structure of lardellite, NH4B5O7(OH)2*H2O Acta Crystallographica B25 2264-22701969synthetic0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
9.45 Å(50)
5.44 Å(71)
5.12 Å(50)
4.70 Å(100)
2.960 Å(71)
2.921 Å(100)
2.887 Å(100)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
45b : [Other oxidized fumarolic minerals]
Stage 10b: Anthropogenic minerals<10 Ka
55 : Anthropogenic mine minerals
57 : Other minerals formed by human processes

Type Occurrence of LarderelliteHide

Place of Conservation of Type Material:
Natural History Museum, Paris, France, 100.1384, 100.1386, 100.1388.
Geological Setting of Type Material:
Boric acid fumaroles in a volcanic region.
Associated Minerals at Type Locality:

Synonyms of LarderelliteHide

Other Language Names for LarderelliteHide

Related Minerals - Strunz-mindat GroupingHide

6.EB.05YarzhemskiiteK[B5O7(OH)2] · H2OMon. 2/m : P21/b
6.EB.10EzcurriteNa4B10O17 · 7H2OTric. 1 : P1
6.EB.15ProbertiteNaCa[B5O7(OH)4] · 3H2OMon. 2/m : P21/b
6.EB.20TertschiteCa4B10O19 · 20H2OMon.
6.EB.25PriceiteCa2B5O7(OH)5 · H2OMon. 2/m : P21/b

Other InformationHide

Notes:
Decomposed by hot water.
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 LarderelliteHide

References for LarderelliteHide

Reference List:

Localities for LarderelliteHide

Showing 2 localities.

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.
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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.
Italy
 
  • Sicily
    • Metropolitan City of Messina
      • Eolie Islands (Aeolian Islands)
        • Lipari
          • Vulcano Island
Campostrini et al. (2011)
  • Tuscany
    • Pisa Province
      • Pomarance
D'Achiardi (1930) +4 other references
 
and/or  
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