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Montmorillonite information


Montmorillonite
A sample of montmorillonite
General
CategoryPhyllosilicates
Smectite group
Formula
(repeating unit)
(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2·nH2O
IMA symbolMnt[1]
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
(same H-M symbol)
Space groupC2/m
Unit cella = 5.19 Å, b = 9.02 Å,
c = 12.4 Å; β = 94°; Z = 2
Identification
ColorWhite, pale pink, blue, yellow, red, green
Crystal habitCompact masses of lamellar or globular microcrystalline aggregates
Cleavage{001} Perfect
FractureUneven
Mohs scale hardness1–2
LusterDull, earthy
DiaphaneityTranslucent
Specific gravity2–3
Optical propertiesBiaxial (−)
Refractive indexnα = 1.485–1.535 nβ = 1.504–1.550 nγ = 1.505–1.550
Birefringenceδ = 0.020
2V angleMeasured: 5° to 30°
References[2][3][4][5]

Montmorillonite is a very soft phyllosilicate group of minerals that form when they precipitate from water solution as microscopic crystals, known as clay. It is named after Montmorillon in France. Montmorillonite, a member of the smectite group, is a 2:1 clay, meaning that it has two tetrahedral sheets of silica sandwiching a central octahedral sheet of alumina. The particles are plate-shaped with an average diameter around 1 μm and a thickness of 0.96 nm; magnification of about 25,000 times, using an electron microscope, is required to resolve individual clay particles. Members of this group include saponite, nontronite, beidellite, and hectorite.

Montmorillonite is a subclass of smectite, a 2:1 phyllosilicate mineral characterized as having greater than 50% octahedral charge; its cation exchange capacity is due to isomorphous substitution of Mg for Al in the central alumina plane. The substitution of lower valence cations in such instances leaves the nearby oxygen atoms with a net negative charge that can attract cations. In contrast, beidellite is smectite with greater than 50% tetrahedral charge originating from isomorphous substitution of Al for Si in the silica sheet.

The individual crystals of montmorillonite clay are not tightly bound hence water can intervene, causing the clay to swell, hence montmorillonite is a characteristic component of swelling soil. The water content of montmorillonite is variable and it increases greatly in volume when it absorbs water. Chemically, it is hydrated sodium calcium aluminium magnesium silicate hydroxide (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2·nH2O. Potassium, iron, and other cations are common substitutes, and the exact ratio of cations varies with source. It often occurs intermixed with chlorite, muscovite, illite, cookeite, and kaolinite.

  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. ^ "Mineralienatlas – Fossilienatlas". mineralienatlas.de. Archived from the original on 23 April 2018. Retrieved 23 April 2018.
  3. ^ Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W.; Nichols, Monte C., eds. (1995). "Montmorillonite" (PDF). Handbook of Mineralogy. Vol. II (Silica, Silicates). Chantilly, VA, USA: Mineralogical Society of America. ISBN 0962209716. OCLC 895497384. Archived (PDF) from the original on 2012-02-05. Retrieved 2017-06-22.
  4. ^ Montmorillonite Archived 2012-05-24 at the Wayback Machine. Mindat.org
  5. ^ Montmorillonite Archived 2011-06-07 at the Wayback Machine. Webmineral

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warm water. In the field of geology, it is more commonly known as montmorillonite. Diosmectite is a contraction of "dioctahedral smectite". Its effectiveness...

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James Ferris

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ion-exchange resins (functionalized porous or gel polymer), zeolites, montmorillonite, clay, and soil humus. Ion exchangers are either cation exchangers...

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lakes and marine basins. The main groups of clays include kaolinite, montmorillonite-smectite, and illite. Chlorite, vermiculite, talc, and pyrophyllite...

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halloysite (from the proper name), saponite (soapstone),: 187  bentonite or montmorillonite (from the French: Montmorillon, toponym). The last mineral is a large...

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other mudrocks. The clay minerals represented are largely kaolinite, montmorillonite and illite. Clay minerals of Late Tertiary mudstones are expandable...

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commonly used are kaolin and the smectite clays such as bentonite, montmorillonite, and Fuller's earth. However, their use is declining, and modern evidence-based...

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MMT

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astronomical observatory in Arizona, USA MMt, one million metric tons Montmorillonite, a clay Magical Mystery Tour, a record by the English rock band the...

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Rhodium

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benzene to cyclohexane catalyzed by rhodium(I) complex supported on montmorillonite clay". Reaction Kinetics and Catalysis Letters. 48 (2): 547. Bibcode:1992RKCL...

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within the liposomes than they would have outside. Some clays, notably montmorillonite, have properties that make them plausible accelerators for the emergence...

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Soil

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Clays — over 30 Sesquioxides — 0–3 Kaolinite — 3–15 Illite — 25–40 Montmorillonite — 60–100 Vermiculite (similar to illite) — 80–150 Humus — 100–300...

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History of life

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can be produced non-biologically in the wild. Some clays, notably montmorillonite, have properties that make them plausible accelerators for the emergence...

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Red Sea

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siliceous fossils Volcanogenic constituents: Tuffites, volcanic ash, montmorillonite, cristobalite, zeolites Terrigenous constituents: Quartz, feldspars...

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aluminium phyllosilicate generally impure clay consisting mostly of montmorillonite. There are a few types of bentonites and their names depend on the...

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Tosudite Smectites and vermiculite family Beidellite Ferrosaponite Montmorillonite Nontronite Saponite Sauconite Swinefordite Vermiculite Volkonskoite...

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Atterberg limits

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Atterberg Limit Values for the Clay Minerals Mineral LL, % PL, % SL, % Montmorillonite 100-900 50-100 8.5-15 Nontronite 37-72 19-27 Illite 60-120 35-60 15-17...

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Glossary of chemical formulae

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Mg(NO3)2·6H2O magnesium nitrate hexahydrate 13446-18-9 MgNaAl5(Si4O10)3(OH)6 montmorillonite (clay) 1318-93-0 MgO magnesium oxide magnesia periclase 1309-48-4 Mg(OH)2...

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