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Model binary phase diagram showing the composition and sintering temperature associated with liquid-phase sintering in the L S2 phase field. The favorable characteristics for liquid-phase sintering include a suppression of the melting temperature, high solid solubility in the liquid, and low liquid solubility in the solid. Reproduced with permission from . Copyright 2009, Springer

Model boundary interphase exchange currents involving lattice vacancy injection at the compound-electrolyte interface and vacancy exchange into the metal releasing an electron and transferring a metal ion into the compound layer

Model boundary interphase exchange currents involving the injection of a lattice vacancy with trapped hole at compound lectrolyte interface and vacancy release into the metal with a hole and metal ion in the compound

Model building by Modeller , First, spatial restraints in the form of atomic distances and dihedral angles are extracted from the template stmcture. The alignment is used to determine equivalent residues between the target and the template. The restraints are combined into an objective function. Finally, the model for the target is optimized until a model that best satisfies the spatial restraints is obtained. This procedure is technically similar to the one used in structure determination by NMR.

Model building could not determine the position of the uronic acid side chain - there was no possibility of forming a hydrogen bond across the glycosidic linkage that defines its orientation. However refinement of the model against the observed X-ray data indicated a high sensitivity to the orientation of the uronic acid side chain and favoured the side chain being folded down along the backbone as shown in

Model building of the pentacoordinate transition state of the reaction into the crystallographic structure of tyrosyl-tRNA synthetase. Reprinted with permission from Ref.

Model building using Bayesian estimation and model discrimination selection.

Model Calculated Liquid Velocity and CARPT Data uq-1.99 cm s b Ug 14.08 cm s .

Model Calculated Liquid Velocity and Data of Hills Ug 16.9 cm s .

Model calculated, diurnally and seasonally averaged OH concentrations as a function of altitude and latitude. The globally averaged OH concentration is predicted to be TxlO molecular cm-.

Model calculation

Model calculation according to Ref. 37 of the photocatalytic rate as a function of parameters F 02 and Z 03 0.001 and ai 0.01. Note that the rate shows a maximum which position depends on the photon flux. At low Z, the rate shape is comparable to those observed in

Model calculation according to Scheme III .

Model calculation for specular reflection and off-specular scattering for only conformal roughness at the interfaces of the polymer multilayer for the system in

Model calculation for specular reflection and off-specular scattering reflecting the Island structure on top of the polymer multilayer for the system In

Model calculation for spin diffusion to a sink. If Region 2 is a sink 60 of the intensity associated with Region I is in the component with the

Model calculation for the CO decomposition. Model parameters Mean residence time, state of mixedness and temperature, Oj concentration 2 Vol and H2O concentration 15 Vol , Kinetic data see Table I

Model calculation for the isomerisation of methyl isocyanide using a two-component generalised weak collision matrix as shown in

Model calculation method for skip-counterbaiance hoist

Model calculation of atmospheric O2 concentration during the Phanerozoic.

Model calculation of boundary motion .

Model calculation of heat flow rates into unilaterally heated layers of 1 mm thick indium and paraffin during the melting process.

Model calculation of major ionic species for MHD combustion of Montana rosebud coal under iuel-rich conditions, equivalence ratio 1.09, O enriched.

Model calculation of neutral phosphorus species for MHD combustion of Montana rosebud coal under fuel-rich conditions equivalence ratio 1.09, O

Model calculation of sulfate in pore water, alkalinity and methane in an explicit numeric solution of Pick s Second Law, accounting for the reaction between sulfate and methane and the alkalinty which is affected thereby. The adjustment to the measured profiles depends on the time passed since the slide occurrence and thus permits the reconstruction of the time of its occurrence which took place about 300 years ago.



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