Anhydrite

























































Anhydrite

Anhydrite HMNH1.jpg
Anhydrite, Chihuahua, Mexico

General
CategorySulfate mineral

Formula
.mw-parser-output .noboldfont-weight:normal
(repeating unit)
Anhydrous calcium sulfate:CaSO4
Strunz classification7.AD.30
Dana classification28.3.2.1
Crystal systemOrthorhombic
Crystal classDipyramidal (mmm)
H–M symbol: (2/m 2/m 2/m)
Space groupAmma
Unit cell
a = 6.245(1) Å, b = 6.995(2) Å
c = 6.993(2) Å; Z = 4
Identification
ColorColorless to pale blue or violet if transparent; white, mauve, rose, pale brown or gray from included impurities
Crystal habitRare tabular and prismatic crystals. Usually occurs as fibrous, parallel veins that break off into cleavage fragments. Also occurs as grainy, massive, or nodular masses
TwinningSimple or repeatedly on 011 common; contact twins rare on 120
Cleavage[010] perfect
[100] perfect
[001] good, resulting in pseudocubic fragments
FractureConchoidal
TenacityBrittle

Mohs scale
hardness
3.5
LusterPearly on 010
vitreous to greasy on 001
vitreous on 100
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity2.97
Optical propertiesBiaxial (+)
Refractive index
nα = 1.567–1.574
nβ = 1.574–1.579
nγ = 1.609–1.618
Birefringence
δ = 0.042–0.044
PleochroismFor violet varieties
X = colorless to pale yellow or rose
Y = pale violet or rose
Z = violet.
2V angle56–84°
Fusibility2
Other characteristicsSome specimens fluoresce; many more fluoresce after heating
References
[1][2][3][4]

Anhydrite, or anhydrous calcium sulfate, is a mineral with the chemical formula CaSO4. It is in the orthorhombic crystal system, with three directions of perfect cleavage parallel to the three planes of symmetry. It is not isomorphous with the orthorhombic barium (baryte) and strontium (celestine) sulfates, as might be expected from the chemical formulas. Distinctly developed crystals are somewhat rare, the mineral usually presenting the form of cleavage masses. The Mohs hardness is 3.5, and the specific gravity is 2.9. The color is white, sometimes greyish, bluish, or purple. On the best developed of the three cleavages, the lustre is pearly; on other surfaces it is glassy. When exposed to water, anhydrite readily transforms to the more commonly occurring gypsum, (CaSO4·2H2O) by the absorption of water. This transformation is reversible, with gypsum or calcium sulfate hemihydrate forming anhydrite by heating to around 200 °C (400 °F) under normal atmospheric conditions.[5] Anhydrite is commonly associated with calcite, halite, and sulfides such as galena, chalcopyrite, molybdenite, and pyrite in vein deposits.




Contents





  • 1 Occurrence

    • 1.1 Tidal flat nodules


    • 1.2 Salt dome cap rocks


    • 1.3 Igneous rocks



  • 2 Naming history


  • 3 Other uses


  • 4 References


  • 5 Further reading




Occurrence




Crystal structure of anhydrite


Anhydrite is most frequently found in evaporite deposits with gypsum; it was, for instance, first discovered in 1794 in a salt mine near Hall in Tirol. In this occurrence, depth is critical since nearer the surface anhydrite has been altered to gypsum by absorption of circulating ground water.


From an aqueous solution, calcium sulfate is deposited as crystals of gypsum, but when the solution contains an excess of sodium or potassium chloride, anhydrite is deposited if the temperature is above 40 °C (104 °F). This is one of the several methods by which the mineral has been prepared artificially and is identical with its mode of origin in nature. The mineral is common in salt basins.



Tidal flat nodules


Anhydrite occurs in a tidal flat environment in the Persian Gulf sabkhas as massive diagenetic replacement nodules. Cross sections of these nodular masses have a netted appearance and have been referred to as chicken-wire anhydrite. Nodular anhydrite occurs as replacement of gypsum in a variety of sedimentary depositional environments.[6]



Salt dome cap rocks


Massive amounts of anhydrite occur when salt domes form a caprock. Anhydrite is 1–3% of the minerals in salt domes and is generally left as a cap at the top of the salt when the halite is removed by pore waters. The typical cap rock is a salt, topped by a layer of anhydrite, topped by patches of gypsum, topped by a layer of calcite.[7] Interaction with oil can reduce SO4 creating calcite, water, and hydrogen sulfide (H2S).[8]



Igneous rocks


Anhydrite has been found in some igneous rocks, for example in the intrusive dioritic pluton of El Teniente, Chile and in trachyandesite pumice erupted by El Chichón volcano, Mexico.[9]



Naming history


The name anhydrite was given by A. G. Werner in 1804, because of the absence of water of crystallization, as contrasted with the presence of water in gypsum. Some obsolete names for the species are muriacite and karstenite; the former, an earlier name, being given under the impression that the substance was a chloride (muriate). A peculiar variety occurring as contorted concretionary masses is known as tripe-stone, and a scaly granular variety, from Volpino, near Bergamo, in Lombardy, as vulpinite; the latter is cut and polished for ornamental purposes.


A semi-transparent light blue-grey variety from Peru is referred to by the trade name angelite.[10]



Other uses




Relief carving of an anhydrite kiln, made from a piece of anhydrite, by Ophelia Gordon Bell


The Catalyst Science Discovery Centre in Widnes, England, has a relief carving of an anhydrite kiln, made from a piece of anhydrite, for the United Sulphuric Acid Corporation.




References




  1. ^ Klein, Cornelis; Hurlbut, Cornelius S. (1985). Manual of Mineralogy (20th ed.). New York: John Wiley and Sons. ISBN 0-471-80580-7..mw-parser-output cite.citationfont-style:inherit.mw-parser-output .citation qquotes:"""""""'""'".mw-parser-output .citation .cs1-lock-free abackground:url("//upload.wikimedia.org/wikipedia/commons/thumb/6/65/Lock-green.svg/9px-Lock-green.svg.png")no-repeat;background-position:right .1em center.mw-parser-output .citation .cs1-lock-limited a,.mw-parser-output .citation .cs1-lock-registration abackground:url("//upload.wikimedia.org/wikipedia/commons/thumb/d/d6/Lock-gray-alt-2.svg/9px-Lock-gray-alt-2.svg.png")no-repeat;background-position:right .1em center.mw-parser-output .citation .cs1-lock-subscription abackground:url("//upload.wikimedia.org/wikipedia/commons/thumb/a/aa/Lock-red-alt-2.svg/9px-Lock-red-alt-2.svg.png")no-repeat;background-position:right .1em center.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registrationcolor:#555.mw-parser-output .cs1-subscription span,.mw-parser-output .cs1-registration spanborder-bottom:1px dotted;cursor:help.mw-parser-output .cs1-ws-icon abackground:url("//upload.wikimedia.org/wikipedia/commons/thumb/4/4c/Wikisource-logo.svg/12px-Wikisource-logo.svg.png")no-repeat;background-position:right .1em center.mw-parser-output code.cs1-codecolor:inherit;background:inherit;border:inherit;padding:inherit.mw-parser-output .cs1-hidden-errordisplay:none;font-size:100%.mw-parser-output .cs1-visible-errorfont-size:100%.mw-parser-output .cs1-maintdisplay:none;color:#33aa33;margin-left:0.3em.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration,.mw-parser-output .cs1-formatfont-size:95%.mw-parser-output .cs1-kern-left,.mw-parser-output .cs1-kern-wl-leftpadding-left:0.2em.mw-parser-output .cs1-kern-right,.mw-parser-output .cs1-kern-wl-rightpadding-right:0.2em


  2. ^ "Anhydrite". Webmineral.


  3. ^ "Anhydrite". Mindat.org.


  4. ^ "Anhydrite" (PDF). Handbook of Mineralogy.


  5. ^ Deer; Howie; Zussman (1992). An Introduction to the Rock=Forming Minerals (2nd ed.). England: Pearson Education. p. 614. ISBN 0-582-30094-0.


  6. ^ Michael A., Church (2003). Encyclopedia of Sediments & Sedimentary Rocks. Springer. p. 17–18. ISBN 978-1-4020-0872-6.


  7. ^ Walker, C. W. (Dec 1976). "Origin of Gulf Coast salt-dome cap rock". AAPG Bulletin. 60 (12): 2162–2166. doi:10.1306/c1ea3aa0-16c9-11d7-8645000102c1865d.


  8. ^ Saunders, James A.; Thomas, Robert C. (September 1996). "Origin of 'exotic' minerals in Mississippi salt dome cap rocks: results of reaction-path modeling". Applied Geochemistry. 11 (5): 667–676. doi:10.1016/S0883-2927(96)00032-7.


  9. ^ Luhr, James F. (2008). "Primary igneous anhydrite: Progress since its recognition in the 1982 El Chichón trachyandesite". Journal of Volcanology and Geothermal Research. 175: 394–407. doi:10.1016/j.jvolgeores.2008.02.016.


  10. ^ "Angelite". Mindat.org.




Further reading


  • Spencer, Leonard James. Anhydrite. 1911 Encyclopædia Britannica

  • Mineralgalleries.com

  • Minerals.net


Popular posts from this blog

How to check contact read email or not when send email to Individual?

Displaying single band from multi-band raster using QGIS

How many registers does an x86_64 CPU actually have?