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Crystal levels

Production flow of the plant—charging of starting materials (level 4), reaction (level 3), crystallization (level 2), filtration (level 1), and drying and blending (level 0). [Pg.50]

JThe usual contribution of the crystal field potential to the Hamiltonian is much smaller than the Ft s and 4/. It should be recognized that all parameters, A , Ft and 4/ cannot be treated as free variables. The parameters Ft and 4/ are first adjusted to fit the free ion levels and then the crystal field parameters are considered to get a best fit with the crystal levels. The available crystal field parameters of the rare earth ions in LaCk and ethylsulphate hosts are compared in Table 43. [Pg.64]

Measurements of strain using X-ray diffraction can be made on polymers but to derive a modulus from these requires the assumption that the applied stress is known at the crystal level. This for the reasons given above, is not valid in the present state of polymer physics. [Pg.114]

A textbook example of conformational polymorphism is provided by ferrocene [44], for which one room temperature disordered and two low-temperature ordered crystalline forms are known. At the crystal level they differ in the relative orientation of the cyclopentadienyl rings and in small rotations of the molecules,... [Pg.345]

A systematic study of the luminescent characteristics of glasses containing rare earths was done in this laboratory (14—20). There has been considerable spectroscopic investigation involving europium activated phosphors for several reasons. The phosphors are of practical use in color television and more information about crystal levels can be obtained for even-electron systems than those with odd-electron systems. Reisfeld et al. (21—25) and Rice and DeShazer (26) have used the fluorescence of europium as an indicator of site S5nnmetry of rare earth ions in glasses. [Pg.57]

Theoretical calculations using a quantum chemical model, which considers the total molecular wavefunctions for each transition, shows good agreement with the experimental findings for the energy and polarization of the optically allowed crystal levels [142b]. [Pg.324]

Fig, I The relationship between an aggregate at the molecular level — a supermolecule — and an aggregate at the crystal level— a periodic supermolecule. [Pg.350]

Fig. 13.21. Self-organization of the tobacco virus. The virus consists of an RNA helix (shown as a single file ) contaming about 7000 nucleotides, which is sufficient genetic material to code the production of 5 — 10 proteins (first level of supramolecular self-organization). The RNA strand interacts very effectively with a certain protein (shown as a drop, which is the second level). The protein molecules associate with the RNA strand forming a kind of necklace, and then the system folds (third level) into a rodUke shape typical for this virus. The rods are able to form a crystal (level four, not shown here), which melts after heating but is restored when cooled down. Fig. 13.21. Self-organization of the tobacco virus. The virus consists of an RNA helix (shown as a single file ) contaming about 7000 nucleotides, which is sufficient genetic material to code the production of 5 — 10 proteins (first level of supramolecular self-organization). The RNA strand interacts very effectively with a certain protein (shown as a drop, which is the second level). The protein molecules associate with the RNA strand forming a kind of necklace, and then the system folds (third level) into a rodUke shape typical for this virus. The rods are able to form a crystal (level four, not shown here), which melts after heating but is restored when cooled down.
We have shown the analysis of a single zeolite crystal under isothermal conditions and non-isothermal conditions in Sections 10.2 and 10.3, respectively. These analyses are important to understand the rate of adsorption at the crystal level. In practice zeolite solids are available in pellet form, and these pellets are made by compressing zeolite crystals together, usually with a small percentage of binder to join the crystals together. Figure 10.4-1 shows schematically a typical zeolite pellet composed of many small zeolite crystals. These crystals are of the order of 0.1 to 1 micron, and the zeolite pellets are of the order of one millimeter. The void between the microparticles contributes to the mesopores and macropores of the particle. These pores act as conduit to transport molecules from the surrounding into the interior of the particle. Once inside the particle, molecules adsorb at the pore mouth of the micropores and thence the adsorbed species diffuse into the interior of the crystal. Micropores within the crystal provide the adsorption space to accommodate adsorbate molecules. [Pg.634]

Based on the above assumptions, the model equations are shown in Table 4. The mass balance equations at the pellet and crystal level are based in the double linear driving model equations or bidisperse model[30]. The solution of the set of parabolic partial differential equations showed in Table 4 was performed using the method of lines. The spatial coordinate was discretized using the method of orthogonal collocation in finite elements. For each element 2 internal collocation points were used and the basis polynomial were calculated using the shifted Jacobi polynomials with weighting function W x) = (a = Q,p=G) hat has equidistant roots inside each element [31]. The set of discretized ordinary differential equations are then solved with DASPK solver [32] which is based on backward differentiation formulas. [Pg.380]

Load variables are F and z y is the weight fraction of solute in solution at saturation as fbced by temperature, so it is not a variable L and B remain to be manipulated so as to control x and the crystallizer level. [Pg.337]

The stability of f orbitals against changes in the ionic environment results in energy levels of various compounds being closely correlated among themselves as well as with those of the free ion, where known. Ah initio free-ion calculations have therefore proven to be very useful for interpreting the crystal levels, and a parametric model based on these calculations has been developed. This model can be applied in a consistent way to ions of both the actinide and lanthanide series [4], and it is used here to help systematize our overall view of actinide spectra... [Pg.361]

The liquid interface sensors tested included a gamma ray radiation gage, a capacitance gage," two float switches, a vibrating quartz crystal level gage, and a thermistor level switch. These devices were all specified as capable of gaging a quiet level to i 1/16 inch. [Pg.445]

This chapter presents the most recent advances in this domain, divided into two parts. First microscopic models are presented. These use the theory of crystallization kinetics at the crystal level. Second, macroscopic models are detailed. These treat crystallization more globally through its description at the macroscopic scale. [Pg.9]

Fig. 10.2 Plot of percentage change in crystallization level against log t for the crystallization of a long chain branched polyethylene. Temperature of crystallization is indicated for each isotherm. (From Buchdahl et al. (2))... Fig. 10.2 Plot of percentage change in crystallization level against log t for the crystallization of a long chain branched polyethylene. Temperature of crystallization is indicated for each isotherm. (From Buchdahl et al. (2))...

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See also in sourсe #XX -- [ Pg.76 ]

See also in sourсe #XX -- [ Pg.362 ]

See also in sourсe #XX -- [ Pg.76 ]




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Crystal field energy levels

Crystal field level

Crystal field level scheme

Crystal field levels resistivity effects

Crystallizers liquid level control

Energy level diagrams and crystal field spectra of transition metal ions

Energy level diagrams crystal field

Energy levels crystal field theory

Octahedral crystal field energy level diagram

Order of orbital energy levels in crystal field theory

Protein crystallization structure levels

Spin-orbit levels arising from crystal field

Spin-orbit levels arising from crystal field terms

Splitting of -levels in a weak crystal field

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