Weddellite
| Weddellite | |
|---|---|
| General | |
| Category | Organic compounds |
| Formula (repeating unit) |
Oxalate(Oxalic acid) (Calcium oxalate dihydrate CaC2O4·2H2O ) |
| Strunz classification | 10.AB.40 |
| Identification | |
| Color | Yellowish brown |
| Crystal habit | eight-face bi-pyramid (typical) |
| Crystal system | Tetragonal |
| Twinning | yes |
| Cleavage | OUI |
| Fracture | Conchoidal |
| Mohs scale hardness | 4 |
| Luster | Vitreous (Glassy) |
| Streak | White |
| Refractive index | 1.52-1.54 - DR +0.009 (B-G interval) |
Weddellite (CaC2O4·2H2O) is a mineral form of calcium oxalate named for occurrences of millimeter-sized crystals found in bottom sediments of the Weddell Sea, off Antarctica. Occasionally, weddellite partially dehydrates to whewellite, forming excellent pseudomorphs of grainy whewellite after weddellite's short tetragonal dipyramids.
Contents |
Structural properties [edit]
The weddellite or calcium oxalate di-hydrate crystallizes in the tetragonal system. The classic crystal shape is the eight-face bi-pyramid. In bright field microscopy, the weddellite crystals are recognized easily by their shape that reminds a mail envelope. More complex shapes of weddellite are possible. The dumbbell shape is not rare. The former has no precise angles or sides. This form is, in reality, a microcrystalline agglomerate that takes the shape of a biconcave disc. Weddellite crystals are poorly birefringent and do not show any interference pattern under polarized light.
Biological role [edit]
Weddellite crystals are usually of little clinical value. Many specimens develop weddellite crystals on standing. Together, whewellite and weddellite are the most common renal calculi.
[edit]
Natroxalate, Whewellite, Caoxite, Novgorodovaite, Oxammite, Glushinskite, Humboldtine, Minguzzite, Zhemchuzhnikovite, Stepanovite, Moolooite, Wheatleyite, Coskrenite
References [edit]
- "Weddellite". Weddellite: Weddellite mineral data. Retrieved June 23, 2005.
- "Weddellite". MINERALOGY OF KIDNEY STONES. Retrieved June 21, 2005.