Phase diagram versus diagram of solubility: What is the difference for nanosystems?

2005 ◽  
Vol 53 (19) ◽  
pp. 5025-5032 ◽  
Author(s):  
A.S. Shirinyan ◽  
A.M. Gusak ◽  
M. Wautelet
1986 ◽  
Vol 74 ◽  
Author(s):  
Y. Goto ◽  
K. Utsumi ◽  
A. Ushioda ◽  
I. Tsugawa ◽  
N. Koshino

AbstractWritten and erased bits of the In-Sb phase change type optical disk medium were studied using transmission electron microscopy (TEN) and electron probe microanalysis (EPMA). Both the bits were separated into inner and outer areas and were composed of only rhombohedral Sb crystals and zinc blende In50Sb50 crystals. The difference between the two bits were in crystal size and atomic distribution of the inner area. Models of the writing and erasing processes were derived from these observations and the In-Sb phase diagram. With these models, the thicknesses, grain sizes and optical contrasts of the both bits were consistently explained.


1991 ◽  
Vol 253 ◽  
Author(s):  
C. Amador ◽  
W. R. L. Lambrecht ◽  
B. Segall

ABSTRACTProgress in the calculation of the phase diagram of the Ni-Pt compounds from "first-principles" is reported. Our procedure consists of: (1) calculating total energies for ordered structures as a function of volume and including internal relaxations by means of the linear muffin-tin orbitals method within the atomic sphere approximation; (2) mapping these results onto an Ising model with effective interaction parameters; and (3) calculating the phase diagram by means of the cluster variation method. We identify the elastic energy related to the difference in the Ni and Pt lattice constant as one of the major problems in this system and discuss the convergence of the cluster expansion of the energy.


1983 ◽  
Vol 48 (7) ◽  
pp. 1936-1943 ◽  
Author(s):  
Ivan Horsák ◽  
Ivo Sláma

Liquidus curves of the phase diagram for the system water-dimethyl sulphoxide (DMSO) have been calculated in such a way as to give a good fit to experimental data for the phase diagram. The calculation is based on the assumption of an equilibrium chemical reaction yielding DMSO.3 H2O, and on the relation for the excess Gibbs energy in a ternary system composed of the two starting components and their compound. The data for the temperature dependence of the difference in the heat capacities of the liquid and solid phases of the pure components in the supercooling region have been obtained by extrapolation of experimental data in the case of DMSO, and for water by adopting published data measured down to -40 °C and by estimating their further trend.


1982 ◽  
Vol 19 ◽  
Author(s):  
BO Sundman ◽  
John Ågren

ABSTRACTA thermodynamic model, based on the regular solution approximation is presented and a formalism, suitable for phases with an arbitrary number of elements and sublattices is described. A new concept, the component array, is introduced in order to simplify the analytical expressions for the Gibbs energy. The mathematical complexity of the model has been solved by the implementation of the model as a part of a general software system for thermochemical and phase diagram calculations by computer.The sublattice model is suitable for describing phases where the difference in size, charge or electronegativity causes a deviation from random mixing of the atoms in a manner which can be described as long range order. This is the case for interstitial solutions and many intermetallic phases, but also for ionic liquids and slag systems. The application of the model to several alloy system will be described.


2010 ◽  
Vol 654-656 ◽  
pp. 2426-2429 ◽  
Author(s):  
Yuko Aono ◽  
Junpei Sakurai ◽  
Akira Shimokohbe ◽  
Seiichi Hata

In this paper, a new high-throughput evaluation method for crystallization temperature (Tx) of thin film amorphous alloy is introduced. For measurement of Tx on integrated thin film samples, thermography is used. The order of one hundred Pd-Cu-Si thin film amorphous samples with different composition are integrated on one chip and measured their Tx at once. The validity of measured Tx are examined by comparing with results of differential scanning calorimeter that is a conventional method for Tx measurement, and equilibrium phase diagram of Pd-Si. As results, the difference of two methods is within 10 K and the trend of Tx map has strong correlation with the phase diagram, respectively.


The electric conductivity ( k ), and its variation with temperature, of many molten salts of predominantly ionic character can be represented by a simple exponential equation k = const. x e -C/RT . Deviations from this relation are sometimes found for partially covalent compounds (e. g. ZnCl 2 , PbCl 2 ) where constitutional changes may be expected with change of temperature. The activation energy of ionic migration ( C ) is always smaller than the activation energy of viscous flow. This fact is attributed to the difference in the configurational changes that occur in the two processes. For alkali chloride, C decreases with increasing ratio of anion to cation radius. For electrolytes involving multivalent ions, C is greater than for uni-univalent ones. Increasing amount of covalency of the bonds involved tends to lower C . The conductivities of a number of mixtures of electrolytes (CdCl 2 -CdBr 2 , CdCl 2 PbCl 2 , CdCl 2 -NaCl, CdCl 2 -KCl, PbCl 2 -KCl) were measured over a range of compositions and temperatures. The activation energies of ionic migration and, where possible, the equivalent conductivities were calculated, and the results discussed together with those obtained in other systems by various investigators. In no system so far investigated is the conductivity a linear function of the composition expressed as mole fraction. In systems which give no evidence of complex ion formation in the mixture, the conductivity usually shows moderate negative deviations from additivity (e. g. CdCl 2 -CdBr 2 ). Only one system so far shows a positive deviation from additivity (CdCl 2 -PbCl 2 . Strong negative deviations from additivity are found in systems in which complex ions are likely to exist in the mixtures (PbCl 2 -KCl, CdCl 2 -KCl, CdCl 2 -NaCl). In the systems CdCl 2 -KCl and PbCl 2 -KCl, the conductivity isotherms have minima at all temperatures investigated; in these systems, the phase diagram indicates a congruently melting compound. Additional minima in the conductivity isotherms are found near compositions at which the phase diagram indicates incongruently melting compounds, but only at low temperatures; at higher temperatures, these minima disappear. The activation energies (C ) have maximum values near compositions that correspond to unstable compounds; in this case, C contains part of the energy change involved in the transition from the complex to the simple ions. In some cases, the activation energy ( C ) of the molten systems rises to very high values as the crystallization temperature is approached. This is interpreted as being due to the existence of a high degree of order in the melt just above the melting-point. Further relations between conductivity, and its temperature coefficient, the activation energy of ionic migration and the constitution of the molten salt mixtures are discussed.


1962 ◽  
Vol 14 ◽  
pp. 149-155 ◽  
Author(s):  
E. L. Ruskol

The difference between average densities of the Moon and Earth was interpreted in the preceding report by Professor H. Urey as indicating a difference in their chemical composition. Therefore, Urey assumes the Moon's formation to have taken place far away from the Earth, under conditions differing substantially from the conditions of Earth's formation. In such a case, the Earth should have captured the Moon. As is admitted by Professor Urey himself, such a capture is a very improbable event. In addition, an assumption that the “lunar” dimensions were representative of protoplanetary bodies in the entire solar system encounters great difficulties.


1997 ◽  
Vol 161 ◽  
pp. 491-504 ◽  
Author(s):  
Frances Westall

AbstractThe oldest cell-like structures on Earth are preserved in silicified lagoonal, shallow sea or hydrothermal sediments, such as some Archean formations in Western Australia and South Africa. Previous studies concentrated on the search for organic fossils in Archean rocks. Observations of silicified bacteria (as silica minerals) are scarce for both the Precambrian and the Phanerozoic, but reports of mineral bacteria finds, in general, are increasing. The problems associated with the identification of authentic fossil bacteria and, if possible, closer identification of bacteria type can, in part, be overcome by experimental fossilisation studies. These have shown that not all bacteria fossilise in the same way and, indeed, some seem to be very resistent to fossilisation. This paper deals with a transmission electron microscope investigation of the silicification of four species of bacteria commonly found in the environment. The Gram positiveBacillus laterosporusand its spore produced a robust, durable crust upon silicification, whereas the Gram negativePseudomonas fluorescens, Ps. vesicularis, andPs. acidovoranspresented delicately preserved walls. The greater amount of peptidoglycan, containing abundant metal cation binding sites, in the cell wall of the Gram positive bacterium, probably accounts for the difference in the mode of fossilisation. The Gram positive bacteria are, therefore, probably most likely to be preserved in the terrestrial and extraterrestrial rock record.


1994 ◽  
Vol 144 ◽  
pp. 421-426
Author(s):  
N. F. Tyagun

AbstractThe interrelationship of half-widths and intensities for the red, green and yellow lines is considered. This is a direct relationship for the green and yellow line and an inverse one for the red line. The difference in the relationships of half-widths and intensities for different lines appears to be due to substantially dissimilar structuring and to a set of line-of-sight motions in ”hot“ and ”cold“ corona regions.When diagnosing the coronal plasma, one cannot neglect the filling factor - each line has such a factor of its own.


Author(s):  
Jules S. Jaffe ◽  
Robert M. Glaeser

Although difference Fourier techniques are standard in X-ray crystallography it has only been very recently that electron crystallographers have been able to take advantage of this method. We have combined a high resolution data set for frozen glucose embedded Purple Membrane (PM) with a data set collected from PM prepared in the frozen hydrated state in order to visualize any differences in structure due to the different methods of preparation. The increased contrast between protein-ice versus protein-glucose may prove to be an advantage of the frozen hydrated technique for visualizing those parts of bacteriorhodopsin that are embedded in glucose. In addition, surface groups of the protein may be disordered in glucose and ordered in the frozen state. The sensitivity of the difference Fourier technique to small changes in structure provides an ideal method for testing this hypothesis.


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