Crystals rhombohedral

The remaining trifluorides of the transition elements known so far apparently crystallize rhombohedrally like VFa. Prior to this structure type the cubic ReOs-type will be discussed briefly, though only oxide-fluorides rather than trifluorides seem to adapt this structure. Yet it is te simple basic type of which the others may be derived. 

Boln. containing Bodium chloride or nitrate in addition to the Bodium carbonate. H. Lowel also emphasized the importance of preventing access of air to the soln. from which the heptahvdrated carbonate is to be obtained—possibly because atm. dust contains some sodium decahydrated carbonate dust, which inoculates the solution with the wrong nuclei. H. Lowel also noted that there are dimorphic forms of the crystals—rhombohedral and rhombic—with different solubilities in water. 

Black crystals. Rhombohedral and hexagonal crystal structure, if 7,70 (also reported as 6.82). mp 710°, Heat of fcoration —13.9 kcal/mol. Heat of combustion 296.4... 

Ko, T. R, Kuznetsov, Y. G., MaUdn, A. J., Day, J., and McPherson, A. 2001. X-ray diffraction and atomic force microscopy analysis of twinned crystals Rhombohedral canavalin, Acta Crystallogr D Biol Crystallogr 57, 829-839. 

Graphite exists in two forms alpha and beta. These have identical physical properties, except for their crystal structure. Naturally occurring graphites are reported to contain as much as 30% of the rhombohedral (beta) form, whereas synthetic materials contain only the alpha form. The hexagonal alpha type can be converted to the beta by mechanical treatment, and the beta form reverts to the alpha on heating it above lOOOoC. 

Texture. All limestones are crystalline, but there is tremendous variance in the size, uniformity, and arrangement of their crystal lattices. The crystals of the minerals calcite, magnesite, and dolomite are rhombohedral those of aragonite are orthorhombic. The crystals of chalk and of most quick and hydrated limes are so minute that these products appear amorphous, but high powered microscopy proves them to be cryptocrystalline. Hydrated lime is invariably a white, fluffy powder of micrometer and submicrometer particle size. Commercial quicklime is used in lump, pebble, ground, and pulverized forms. 

Silver nitrate forms colorless, rhombic crystals. It is dimorphic and changes to the hexagonal rhombohedral form at 159.8°C. It melts at 212°C to a yellowish Hquid which solidifies to a white, crystalline mass on cooling. An alchemical name, lunar caustic, is stiU appHed to this fused salt. In the presence of a trace of nitric acid, silver nitrate is stable to 350°C. It decomposes at 440°C to metallic silver, nitrogen, and nitrogen oxides. Solutions of silver nitrate are usually acidic, having a pH of 3.6—4.6. Silver nitrate is soluble in ethanol and acetone. 

Antimony(III) iodide [7790-44-5] Sbl, forms red rhombohedral crystals, intermediate in stmcture between a molecular and an ionic crystal. In Sbl vapor there is no indication of association. 

The physical properties of elemental boron are significantly affected by purity and crystal form. In addition to being an amorphous powder, boron has four crystalline forms a-rhombohedral, P-rhombohedral, a-tetragonal, and -tetragonal. The a-rhombohedral form has mp 2180°C, sublimes at approximately 3650°C, and has a density of 2.45 g/mL. Amorphous boron, by comparison, has mp 2300°C, sublimes at approximately 2550°C, and has a density of 2.35 g/mL. 

The a-rhombohedral form of boron has the simplest crystal stmcture with slightly deformed cubic close packing. At 1200°C a-rhombohedral boron degrades, and at 1500°C converts to P-rhombohedral boron, which is the most thermodynamically stable form. The unit cell has 104 boron atoms, a central B 2 icosahedron, and 12 pentagonal pyramids of boron atom directed outward. Twenty additional boron atoms complete a complex coordination (2). 

Crystal Structure. Sihcon carbide may crystalline in the cubic, hexagonal, or rhombohedral stmcture. There is a broad temperature range where these stmctures may form. The hexagonal and rhombohedral stmcture designated as the a-form (noncubic) may crystalline in a large number of polytypes. 

There are three possible arrangements of atoms in a layer of SiC crystal, and each type has the same layers but a different stacking sequence (29). Designation (30) is by the number of layers in the sequence, followed by H, R, or C to indicate whether the type belongs to the hexagonal, rhombohedral, or cubic class. 

Fig. 5 shows data from a simulation of TIP4P water that is confined on both sides by a rhombohedral mercury crystal with (111) surface structure. Bosio et al. [135] deduce from their X-ray studies that a solid o-mercury lattice with a larger lattice constant in the z direction may be used as a good structural model for liquid mercury. Thus, the mercury phase was modeled as a rigid crystal in order to simplify the simulations. The surface of such a crystal shows rather low corrugation. 

Polonium is unique in being the only element known to crystallize in the simple cubic form (6 nearest neighbours at 335 pm). This a-form distorts at about 36° to a simple rhombohedral modification in which each Po also has 6 nearest neighbours at 335 pm. The precise temperature of the phase change is difficult to determine because of the self-heating of crystalline Po (p. 751) and it appears that both modifications can coexist from about 18° to 54°. Both are silvery-white metallic crystals with substantially higher electrical conductivity than Te. 

Trivalent Oxides.—It is probable that the rhombohedral crystal corundum, AI2O3, consists of ions that is, the bonds are probably electrostatic. The oxygen ions are arranged in layers parallel to the base (111) within each layer the distances between adjacent ions are 2.50 and 2.89 A., the values being somewhat uncertain because of the difficulty in the accurate determination of the parameter. These values are probably compatible with the oxygen radius 1.40 A., calculated for crystals with bivalent cations. The aluminum-oxygen distances are 1.85 and 1.99 A., in satisfactory agreement with the calculated radius sum 1.90 A. 

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