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C spacing

The electronic structure of an infinite crystal is defined by a band structure plot, which gives the energies of electron orbitals for each point in /c-space, called the Brillouin zone. This corresponds to the result of an angle-resolved photo electron spectroscopy experiment. [Pg.266]

The Fermi energy is the energy of the highest-energy filled orbital, analogous to a HOMO energy. If the orbital is half-filled, its energy will be found at a collection of points in /c-space, called the Fermi surface. [Pg.270]

Kelvin, or a point in /c-space a constant Boltzmann constant kilograms... [Pg.401]

FIGURE 1 6 Molecular models of methane (CH4) (a) Framework (tube) models show the bonds connecting the atoms but not the atoms themselves (b) Ball and stick (ball and spoke) models show the atoms as balls and the bonds as rods (c) Space filling models portray overall molecular size the radius of each sphere approximates the van der Waals radius of the atom (d) An electrostatic potential map of methane... [Pg.28]

The stmcture of tridymite is more open than that of quart2 and is similar to that of cristobaUte. The high temperature form, probably S-IV, has a hexagonal unit cell containing four Si02 units, where ttg = 503 pm and Cg = 822 pm > 200° C, space group Pb./mmc. The Si—O distance is 152 pm. [Pg.475]

Reforming Conditions. The main process variables are pressure, 450—3550 kPa (50—500 psig), temperature (470—530°C), space velocity, and the catalyst employed. An excess of hydrogen (2—8 moles per mole of feed) is usually employed. Depending on feed and processing conditions, net hydrogen production is usually in the range of 140—210 m /m feed (800—1200 SCF/bbl). The C —products are recovered and normally used as fuels. [Pg.308]

The unit layers stack together face-to-face and are held in place by weak attractive forces. The distance between corresponding planes in adjacent unit layers is called the c-spacing. A clay crystal structure with a unit layer consisting of three sheets typically has a c-spacing of about 9.5 X 10 mm. [Pg.59]

Two types of swelling may occur. Surface hydration is one type of swelling in which water molecules are adsorbed on crystal surfaces. Hydrogen bonding holds a layer of water molecules to the oxygen atoms exposed on the crystal surfaces. Subsequent layers of water molecules align to form a quasi-crystalline structure between unit layers which results in an increased c-spacing. All types of clays swell in this manner. [Pg.60]

Osmotic swelling is a second type of swelling. Where the concentration of cations between unit layers in a clay mineral is higher than the cation concentration in the surrounding water, water is osmotically drawn between the unit layers and the c-spacing is increased. Osmotic swelling results in larger overall volume increases than surface hydration. However, only certain clays, like sodium montmorillonite, swell in this manner. [Pg.60]

Pillinger, C. Space is a Funny Place. Barnstorm Productions, Venice (2007)... [Pg.475]

Fig. 3.4.2 Schematic description of the three-dimensional SPRITE imaging technique. Gz, Gx and Gy are the phase encode magnetic field gradients and are amplitude cycled. A single data point is acquired at a fixed encoding time tp after the rf excitation pulse from the free induction decay (FID). TR is the time between rf pulses. Notice that Gx is ramped (+GZ max to -GXt max) and one /c-space point is acquired for each value of the magnetic field gradient. Gy and Gz are on during the Gx magnetic field gradient ramp and turned off at the end. Fig. 3.4.2 Schematic description of the three-dimensional SPRITE imaging technique. Gz, Gx and Gy are the phase encode magnetic field gradients and are amplitude cycled. A single data point is acquired at a fixed encoding time tp after the rf excitation pulse from the free induction decay (FID). TR is the time between rf pulses. Notice that Gx is ramped (+GZ max to -GXt max) and one /c-space point is acquired for each value of the magnetic field gradient. Gy and Gz are on during the Gx magnetic field gradient ramp and turned off at the end.
Temperature, T (°C) Space time (sec) Fraction propane converted... [Pg.309]

Fig. 4 Cationic structure of 4. a Stereo view of the structure of the octahedron with only two of the vertices, b Ellipsoid and c space-tilling representations of 4. d Huge LngCui2 octahedral core Emcapsulates a CIO anion, e f Coordination environment of Tb3+ and the outer Cu2+ ions in the two vertices. The symmetry codes of a and b are z, x — 1, y+ 1 and y + 1, z — 1, x, respectively. The dashed line represents the weak coordination bonding... Fig. 4 Cationic structure of 4. a Stereo view of the structure of the octahedron with only two of the vertices, b Ellipsoid and c space-tilling representations of 4. d Huge LngCui2 octahedral core Emcapsulates a CIO anion, e f Coordination environment of Tb3+ and the outer Cu2+ ions in the two vertices. The symmetry codes of a and b are z, x — 1, y+ 1 and y + 1, z — 1, x, respectively. The dashed line represents the weak coordination bonding...
James and Williams have determined that triprolidine hydrochloride monohydrate crystals belong to the P2j/c space group.8 There are 4 molecules per unit cell. The... [Pg.516]

The Adsorption of Cs+on Clays - an ion with a simple solution chemistry (no hydrolysis, no complex formation) - can be remarkably complex. Grutter et al. (1990) have studied adsorption and desorption of Cs+ on glaciofluvial deposits and have shown that the isotherms for sorption and exchange on these materials are nonlinear. Part of this non-linearity can be accounted for by the collaps of the c-spacing of certain clays (vermiculite, chlorite). As illustrated in Fig. 4.23 the Cs+ sorption on illite and chlorite is characterized by non-linearity. [Pg.141]

Na-montmorillonite (89) (Clay Spur) and Na-vermiculite (90) (Palabora) and the C-spacings... [Pg.275]

Cation Anion Montmorillonite AH (kJ Eq ) C-spacing Vermiculite AH (kJ Eq 0 C- spacing... [Pg.275]

Vermiculites have a 2 1 layer structure similar to smectites, but expand less freely in water, presumably because of the higher layer charge in the former minerals. Most of this structural charge resides in the tetrahedral layers of the vermiculite platelets. Even when fully wetted, vermiculites do not expand beyond the two water-layer stage ( " 1.5 nm c-spacing). [Pg.364]


See other pages where C spacing is mentioned: [Pg.1527]    [Pg.1527]    [Pg.1527]    [Pg.62]    [Pg.266]    [Pg.266]    [Pg.269]    [Pg.400]    [Pg.400]    [Pg.401]    [Pg.401]    [Pg.340]    [Pg.358]    [Pg.71]    [Pg.457]    [Pg.189]    [Pg.214]    [Pg.236]    [Pg.237]    [Pg.218]    [Pg.60]    [Pg.36]    [Pg.46]    [Pg.278]    [Pg.71]    [Pg.71]    [Pg.255]    [Pg.133]    [Pg.174]    [Pg.373]    [Pg.225]    [Pg.231]   
See also in sourсe #XX -- [ Pg.243 ]




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