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Leonite

Leonite
leonite as white pseudomorphs after sharp freestanding picromerite crystals sizes to 2 cm, perched on a matrix of crystallized halite. 5.5 x 4.7 x 3.4 cm
Leonite
General
Category Sulfate mineral
Formula
(repeating unit)
K2Mg(SO4)2·4H2O
Strunz classification 7.CC.55
Dana classification 29.03.03.01
Crystal system Monoclinic
Crystal class Prismatic (2/m)
(same H-M symbol)
Space group C2/m
Unit cell a = 11.78, b = 9.53
c = 9.88 [Å]; β = 95.4°; Z = 4
Identification
Formula mass 366.69 g/mol
Color White to colorless, yellow
Crystal habit Tabular crystals
Twinning {100}
Cleavage none
Fracture conchoidal
Mohs scale hardness 2.5 - 3
Luster Vitreous or Waxy
Streak White
Diaphaneity Transparent to translucent
Specific gravity 2.201
Optical properties Biaxial (+)
Refractive index nα = 1.479 nβ = 1.482 nγ = 1.487
Birefringence δ = 0.008
2V angle Measured: 90° Calc: 76°
Dispersion none
Fusibility easy
Other characteristics Leonit, 钾镁矾, Leonita, Леонит, Kalium-Astrakanit, Kalium-Blödit
References

Leonite is a hydrated double sulfate of magnesium and potassium. It has the formula K2SO4·MgSO4·4H2O. The mineral was named after Leo Strippelmann, who was director of the salt works at Westeregeln in Germany. The mineral is part of the blodite group of hydrated double sulfate minerals.

Leonite has a bitter taste.

When leonite is analyzed for elements, it is usually contaminated with sodium and chloride ions, as it commonly occurs with sodium chloride.

In the mineral family of leonite, the lattice contains sulfate tetrahedrons, a divalent element in an octahedral position surrounded by oxygen, and water and univalent metal (potassium) linking these other components together. One sulfate group is disordered at room temperature. The disordered sulfate becomes fixed in position as temperature is lowered. The crystal form also changes at lower temperatures, so two other crystalline forms of leonite exist at lower temperatures.

The dicharged metal cation (magnesium) is embedded in oxygen octahedra, four from water around the equator, and two from sulfate ions at the opposite poles. In the crystal there are two different octahedral environments. Each of these octahedra are joined together by potassium ions and hydrogen bonds.

The sulfate occurs in layers parallel to the (001) surface. In the room temperature form, the sequence is ODODODODOD with O=ordered, and D=disordered. In the next form at lower temperatures, the disordered sulfate appears in two different orientations giving the sequence OAOBOAOBOAOBOAOB. At the lowest temperatures, the sequence simplifies to OAOAOAOAOAO.

The first phase transition happens at -4 °C. At 170 K (−103 °C), the crystals have space group I2/a, lattice parameters a = 11.780 Å, b = 9.486 Å, c = 19.730 Å, β = 95.23°, 8 formula per unit cell, and a cell volume of V = 2195.6 Å3. The c dimension and unit cell volume are doubled due to the presence of four sulfate layers rather than two as in the other forms. The next phase change happens at -153 °C. At 100 K (−173 °C), the space group is P21/a, a = 11.778 Å, b = 9.469 Å, c = 9.851 Å, β = 95.26°, 4 formula per unit cell, and a cell volume of V = 1094.01 Å3.


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Wikipedia

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