Jennite | |
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Crystal structure of jennite: elementary unit cell viewed in 3D |
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General | |
Category | Silicate mineral, Calcium silicate hydrate (CSH) |
Chemical formula | Ca9Si6O18(OH)6·8H2O |
Identification | |
Molar mass | 1062 |
Color | White |
Crystal habit | Blade shaped crystals, fibrous aggregates, platy - sheet forms |
Crystal system | Triclinic, Space Group: P1 |
Cleavage | [001] Distinct |
Mohs scale hardness | 3.5 |
Luster | Vitreous (glassy) |
Streak | White |
Density | 2.32 – 2.33 |
Ultraviolet fluorescence | Weak white |
Other characteristics | Late stage mineral in metamorphosed limestone |
References | [1][2][3] |
Jennite is a calcium silicate hydrate (CSH) of general chemical formula: Ca9Si6O18(OH)6·8(H2O).
Jennite occurs in hydrated cement paste and can be found in nature in particular conditions, e.g., as alteration mineral in metamorphosed limestone and skarn.
A first specimen of jennite found in 1966 at the Crestmore quarries (Crestmore, Riverside County, California, USA) was analysed and identified as a new mineral by Carpenter in 1966 (Carpenter, 1966). They named it in honour of its discoverer: Clarence Marvin Jenni (1896–1973) director of the Geological Museum at the University of Missouri.
In contrast to the first analysis made by Carpenter, jennite does not contain appreciable amount of sodium when the Crestmore specimen was reexamined (Gard, 1977).
The structure of jennite determined by is made of three distinct modules: ribbons of edge-sharing calcium octahedra, silicate chains of wollastonite-type running along the b axis, and additional calcium octahedra on inversion centers. The hydroxyl groups are bonded to three calcium cations while no SiOH groups are observed (Bonaccorsi 2004).
Jennite transforms to metajennite at 70 – 90 °C by losing four water molecules.