Experimental study of the properties of alkali metals and alloys in the temperature range 1000?1800�K

1980 ◽  
Vol 39 (6) ◽  
pp. 1281-1286
Author(s):  
V. V. Grafova ◽  
N. Ya. Mikhailov ◽  
I. I. Novikov ◽  
M. A. Pokrasin ◽  
V. V. Roshchupkin ◽  
...  
1992 ◽  
Vol 114 (1) ◽  
pp. 13-18 ◽  
Author(s):  
F. Wang ◽  
J. G. Lenard

Ring compression tests were conducted at constant true strain rates in the temperature range of 900–975°C. The constant friction shear factor, m, was determined using a calibration chart. Scaling was permitted during the experiments in which a glass based lubricant was also used. Frictional conditions were affected most by the rate of strain; increasing it led to lower values of m.


2017 ◽  
Vol 21 (5) ◽  
pp. 15-23
Author(s):  
Muhammad Irsyad ◽  
Yuli S. Indartono ◽  
Ari D. Pasek ◽  
Willy Adriansyah

2013 ◽  
Vol 34 (5) ◽  
pp. 425-429 ◽  
Author(s):  
P. Priputen ◽  
T. Y. Liu ◽  
I. Černičková ◽  
D. Janičkovič ◽  
V. Kolesár ◽  
...  

2013 ◽  
Vol 694-697 ◽  
pp. 712-715
Author(s):  
Hai Bin Liang ◽  
Hui Zhong Zhao

The solar adsorption water tube was put forward in this research paper, which producing water from atmosphere with solar energy. When the ambient temperature range is 30.7°C-41.6 °C and the solar transient radiation range is 284 W/m2-1007 W/m2, a solar adsorption water tube could produce 78ml water after adsorbed 10m3 air. The highest temperature of the adsorption bed can reach to 200°Cin the process of desorption.


1968 ◽  
Vol 36 (284) ◽  
pp. 1061-1077 ◽  
Author(s):  
Ian Parsons

SummaryVariations in the value of 2θ131 – 2θ13̄1 of two anorthoclase feldspars of compositions Ab95Or5 and Ab90Or10 were investigated by hydrothermal crystallization of gels for long periods in the temperature range 500–950 °C, at water vapour pressures up to 15 000 lb/in.2. The results are compared to those obtained by MacKenzie (1957) for pure albite. It is shown that the variation in 2θ131 – 2θ13̄1 is largely the result of Al-Si order-disorder and that at 700 °C and above the magnitude of the variation in the anorthoclases suggests that the degree of order is like that in albite, but at lower temperatures, particularly below 600 °C, the variation is less, and the anorthoclases are less ordered than albite at the same temperatures. At 600 °C and above the rate of attainment of equilibrium is the same for all three compositions. Below 600 °C Ab95Or5 behaves differently to albite. At low temperatures the equilibrium degree of Al-Si order in mixed Na-K feldspars is a function of composition as well as of temperature of crystallization.


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