Strontianite

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Strontianite
2V angle
Measured: 7°, Calculated: 12° to 8°
Ultraviolet fluorescenceAlmost always fluorescent
SolubilitySoluble in dilute HCl
Alters toCelestine SrSO4
References[2][3][4][5]

Strontianite (SrCO3) is an important raw material for the extraction of strontium. It is a rare carbonate mineral and one of only a few strontium minerals. It is a member of the aragonite group.

Aragonite group members:[2] aragonite (CaCO3), witherite (BaCO3), strontianite (SrCO3), cerussite (PbCO3)

The ideal formula of strontianite is SrCO3, with molar mass 147.63 g,[4] but calcium (Ca) can substitute for up to 27% of the strontium (Sr) cations, and barium (Ba) up to 3.3%.[2]

The mineral was named in 1791 for the locality, Strontian, Argyllshire, Scotland, where the element strontium had been discovered the previous year.[2] Although good mineral specimens of strontianite are rare, strontium is a fairly common element, with abundance in the Earth's crust of 370 parts per million by weight, 87 parts per million by moles, much more common than copper with only 60 parts per million by weight, 19 by moles.[6] Strontium is never found free in nature. The principal strontium ores are celestine SrSO4 and strontianite SrCO3. The main commercial process for strontium metal production is reduction of strontium oxide with aluminium.[6]

Unit cell

Strontianite is an orthorhombic mineral, belonging to the most symmetrical class in this system, 2/m 2/m 2/m, whose general form is a rhombic dipyramid. The space group is Pmcn. There are four formula units per unit cell (Z = 4) and the unit cell parameters are a = 5.1 Å, b = 8.4 Å, c = 6.0 Å.

Structure

Strontianite is

divalent cations with ionic radii greater than 1.0 Å, the radius ratios generally do not permit stable 6-fold coordination. For small cations the structure is rhombohedral, but for large cations it is orthorhombic. This is the aragonite structure type with space group Pmcn. In this structure the CO3 groups lie perpendicular to the c axis, in two structural planes, with the CO3 triangular groups of one plane pointing in opposite directions to those of the other.[7] These layers are separated by layers of cations.[2]

The CO3 group is slightly non-planar; the carbon atom lies 0.007 Å out of the plane of the oxygen atoms. The groups are tilted such that the angle between a plane drawn through the oxygen atoms and a plane parallel to the a-b unit cell plane is 2°40’.[8]

Crystal form

Strontianite occurs in several different habits. Crystals are short prismatic parallel to the c axis and often acicular.[2][3][5] Calcium-rich varieties often show steep pyramidal forms.[2] Crystals may be pseudo hexagonal[2][3][5] due to equal development of different forms.[3] Prism faces are striated horizontally.[2][3] The mineral also occurs as columnar to fibrous, granular or rounded masses.[2][3][5]

Radial aggregate of strontianite
Acicular strontianite in spherical aggregates
Strontianite in pseudo-hexagonal crystals

Optical properties

Strontianite is colourless, white, gray, light yellow, green or brown, colourless in transmitted light. It may be longitudinally zoned. It is transparent to translucent, with a vitreous (glassy) lustre, resinous on broken surfaces, and a white streak.

It is a biaxial(−) mineral. The direction perpendicular to the plane containing the two optic axes is called the optical direction Y. In strontianite Y is parallel to the b crystal axis. The optical direction Z lies in the plane containing the two optic axes and bisects the acute angle between them. In strontianite Z is parallel to the a crystal axis. The third direction X, perpendicular both to Y and to Z, is parallel to the c crystal axis.[2][5] The refractive indices are close to nα = 1.52, nβ = 1.66, nγ = 1.67, with different sources quoting slightly different values:

  • nα = 1.520, nβ = 1.667, nγ = 1.669[2]
  • nα = 1.516 – 1.520, nβ = 1.664 – 1.667, nγ = 1.666 – 1.668[3][4]
  • nα = 1.517, nβ = 1.663, nγ = 1.667 (synthetic material)[9]

The maximum birefringence δ is 0.15[3] and the measured value of 2V is 7°, calculated 12° to 8°.[3][4]

If the colour of the incident light is changed, then the refractive indices are modified, and the value of 2V changes. This is known as dispersion of the optic axes. For strontianite the effect is weak, with 2V larger for violet light than for red light r < v.[5]

Luminescence

Strontianite is almost always

X-rays and electron beams. All materials will glow red hot if they are heated to a high enough temperature (provided they do not decompose first); some materials become luminescent at much lower temperatures, and this is known as thermoluminescence. Strontianite is sometimes thermoluminescent.[2][3][5]

Physical properties

Cleavage is nearly perfect parallel to one set of prism faces, {110}, and poor on {021}. Traces of cleavage have been observed on {010}.[3][5]

Twinning is very common, with twin plane {110}. The twins are usually contact twins; in a contact twin the two individuals appear to be reflections of each other in the twin plane. Penetration twins of strontainite are rarer; penetration twins are made up of interpenetrating individuals that are related to each other by rotation about a twin axis. Repeated twins are made up of three or more individuals twinned according to the same law. If all the twin planes are parallel then the twin is polysynthetic, otherwise it is cyclic.[7] In strontianite repeated twinning forms cyclic twins with three or four individuals, or polysynthetic twins.[2][3][5]

The mineral is brittle, and breaks with a subconchoidal to uneven

specific gravity of the pure endmember with no calcium substituting for strontium is 3.78,[9] but most samples contain some calcium, which is lighter than strontium, giving a lower specific gravity, in the range 3.74 to 3.78.[3] Substitutions of the heavier ions barium and/or lead increase the specific gravity, although such substitutions are never very abundant.[9] Strontianite is soluble in dilute hydrochloric acid HCl[2][3] and it is not radioactive.[4]

Environment and associations

Strontianite is an uncommon low-temperature

ground water.[9] Under appropriate conditions it alters to celestine SrSO4, and it is itself found as an alteration from celestine.[2] These two minerals are often found in association, together with baryte, calcite, harmotome and sulfur.[5]

Occurrences

Type locality

The

veins in gneiss.[2]

Other UK localities include Brownley Hill Mine (Bloomsberry Horse Level), Nenthead,

Mississippi Valley-type deposits.[11]

Canada

The Francon quarry,

Montréal
, Québec.
Strontianite is very common at the Francon Quarry, in a great variety of habits. It is a late stage mineral, sometimes found as multiple generations. It is found as translucent to opaque, white to pale yellow or beige generally smooth surfaced spheroids, hemispheres and compact spherical and botryoidal aggregates to 10 cm in diameter, and as spheres consisting of numerous radiating acicular crystals, up to 1 cm across. Also as tufts, parallel bundles, and sheaf-like clusters of fibrous to acicular crystals, and as white, finely granular porcelaneous and waxy globular aggregates. Transparent, pale pink, columnar to tabular sixling twins up to 1 cm in diameter have been found, and aggregates of stacked stellate sixling twins consisting of transparent, pale yellow tabular crystals.[10]

Another Canadian occurrence is at Nepean, Ontario, in vein deposits in limestone.[2]

Germany

Commercially important deposits occur in

zeolites at Oberschaffhausen, Bötzingen, Kaiserstuhl, Baden-Württemberg.[2]

India

In

phosphate nodules in clay.[2]

Mexico

It occurs in the Sierra Mojada District, with celestine in a lead-silver deposit.[2]

Russia

It occurs in the Kirovskii

pegmatites, associated with kukharenkoite-(La), microcline, albite, calcite, nenadkevichite, hilairite, catapleiite, donnayite-(Y), synchysite-(Ce), pyrite and others.[12]

It also occurs at

cerite-(Ce), edingtonite, ilmenite and calcite.[14]

United States

In the

salt domes.[2]

At the Minerva Number 1 Mine (Ozark-Mahoning Number 1 Mine) Ozark-Mahoning Group,

Fluorspar District, Hardin County strontanite occurs as white, brown or rarely pink tufts and bowties of acicular crystals with slightly curved terminations.[15]

In the Silurian Lockport Group, Central and Western New York strontianite is observed in cavities in eastern Lockport, where it occurs as small white radiating sprays of acicular crystals.[16]

In

Mifflin County, Pennsylvania, it occurs with aragonite, again in limestone.[2]

  • Strontianite from Strontian, Scotland
    Strontianite from Strontian, Scotland
  • Dresserite and Strontianite from the Francon quarry, Canada
    Dresserite and Strontianite from the Francon quarry, Canada
  • Strontianite from the Dreislar Mine, North Rhine-Westphalia, Germany
    Strontianite from the Dreislar Mine, North Rhine-Westphalia, Germany
  • Strontianite from Texas, US
    Strontianite from Texas, US
  • Strontianite from Illinois, US
    Strontianite from Illinois, US
  • Strontianite from California
    Strontianite from California

See also

References

  1. S2CID 235729616
    .
  2. ^ a b c d e f g h i j k l m n o p q r s t u v w x y Gaines et al (1997) Dana’s New Mineralogy Eighth Edition. Wiley
  3. ^ a b c d e f g h i j k l m n o p Strontianite on Mindat.org retrieved 23/08/11
  4. ^ a b c d e Barthelmy, Dave. "Strontianite Mineral Data". Retrieved 23 August 2011.
  5. ^ a b c d e f g h i j k "Strontianite in the Handbook of Mineralogy" (PDF). Retrieved 24 August 2011.
  6. ^ a b "Strontium". Retrieved 24 August 2011.
  7. ^ a b c Klein and Hurlbut (1993) Manual of Mineralogy 21st Edition. Wiley
  8. ^ De Villiers, Johan P R (1971) Crystal Structures of Aragonite, Strontianite and Witherite. The American Mineralogist 56:758
  9. ^ a b c d Speer, J A and Hensley-Dunn, M L (1976) Strontianite composition and physical properties. American Mineralogist 61:1001–1004
  10. ^ a b The Mineralogical Record (2006) 37-1:44
  11. ^ The Mineralogical Record (2010) 41-1:62 supplement
  12. ^ The Mineralogical Record (2004) 35-4:355
  13. ^ The Mineralogical Record (2004) 35-2:176
  14. ^ The Mineralogical Record 35-4:347 (2004)
  15. ^ Rocks & Minerals (2010) 85-3:212
  16. ^ Rocks & Minerals (2009) 84-4:332

External links

Media related to Strontianite at Wikimedia Commons

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