simple eutectic system
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2011 ◽  
Vol 15 ◽  
pp. 01020 ◽  
Author(s):  
V. S. Savvin ◽  
Ye. Yu. Pomytkina ◽  
N. N. Anokhina

2008 ◽  
Vol 63 (5-6) ◽  
pp. 364-370 ◽  
Author(s):  
Monika Szymanska-Kolodziej ◽  
Pavel Kolodziej ◽  
Leszek Rycerz ◽  
Marcelle Gaune-Escard

Differential scanning calorimetry (DSC) was used to investigate the phase equilibrium in the AgCl- NdCl3 system. This binary mixture represents a typical example of simple eutectic system, with eutectic composition x(AgCl)=0.796 and temperature Teut = 668 K, respectively. The electrical conductivity of AgCl-NdCl3 liquid mixtures, together with that of pure components was measured down to temperatures below solidification. Results obtained are discussed in terms of possible complex formation.


2007 ◽  
Vol 45 (3) ◽  
pp. 327-333 ◽  
Author(s):  
V. S. Savvin ◽  
A. K. Azavi ◽  
A. A. Povzner

1975 ◽  
Vol 12 (4) ◽  
pp. 527-530 ◽  
Author(s):  
B. D. Alkire ◽  
W. M. Haas ◽  
T. J. Kaderabek

The dry density of a silty sand compacted at temperatures below 0 °C can be improved by using calcium chloride as an additive. Compaction tests at −7 °C were used to determine the effect of low amounts of calcium chloride on the moisture–density relationship of the test soil. Tests at 20 °C were conducted to provide a frame of reference for comparing the results obtained at the below freezing temperature. The results from the experimental work are analyzed by modeling the pore fluid as a simple eutectic system using the concepts of phase equilibria. The amount of ice in the pore fluid is shown to have a significant effect on the dry density of a soil compacted at temperatures below 0 °C.


Author(s):  
E. Christiaan De Wys ◽  
Wilfrid R. Foster

SummaryThe high-temperature phase equilibrium relationships in the system diopside-anorthite—åkermanite have been investigated by the quenching method. This system may be regarded as essentially a simple eutectic system. The eutectic is located at the composition 9 diopside:44 anorthite:47 åkermanite (by weight) and at a temperature of 1226° C. Åkermanite is a stable phase at least as low as this temperature. Triclinic anorthite is the only form of CaAl2Si2O8 encountered in the liquidus range of temperatures.


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