A photoelectric pyrometer for measuring the true temperature of tungsten

1968 ◽  
Vol 8 (3) ◽  
pp. 259-261
Author(s):  
V. D. Dmitriev ◽  
G. V. Kholopov
1968 ◽  
Vol 8 (2) ◽  
pp. 135-138
Author(s):  
V. D. Dmitriev ◽  
G. K. Kholopov

Minerals ◽  
2021 ◽  
Vol 11 (7) ◽  
pp. 725
Author(s):  
Ludmila B. Damdinova ◽  
Bulat B. Damdinov

This article discusses the peculiarities of mineral composition and a fluid inclusions (FIs further in the text) study of the Kholtoson W and Inkur W deposits located within the Dzhida W-Mo ore field (Southwestern Transbaikalia, Russia). The Mo mineralization spatially coincides with the apical part of the Pervomaisky stock (Pervomaisky deposit), and the W mineralization forms numerous quartz veins in the western part of the ore field (Kholtoson vein deposit) and the stockwork in the central part (Inkur stockwork deposit). The ore mineral composition is similar at both deposits. Quartz is the main gangue mineral; there are also present muscovite, K-feldspar, and carbonates. The main ore mineral of both deposits is hubnerite. In addition to hubnerite, at both deposits, more than 20 mineral species were identified; they include sulfides (pyrite, chalcopyrite, galena, sphalerite, bornite, etc.), sulfosalts (tetrahedrite, aikinite, stannite, etc.), oxides (scheelite, cassiterite), and tellurides (hessite). The results of mineralogical and fluid inclusions studies allowed us to conclude that the Inkur W and the Kholtoson W deposits were formed by the same hydrothermal fluids, related to the same ore-forming system. For both deposits, the fluid inclusion homogenization temperatures varied within the range ~195–344 °C. The presence of cogenetic liquid- and vapor-dominated inclusions in the quartz from the ores of the Kholtoson deposit allowed us to estimate the true temperature range of mineral formation as 413–350 °C. Ore deposition occurred under similar physical-chemical conditions, differing only in pressures of mineral formation. The main factors of hubnerite deposition from hydrothermal fluids were decreases in temperature.


1970 ◽  
Vol 92 (3) ◽  
pp. 639-652 ◽  
Author(s):  
C. E. Smeltzer ◽  
M. E. Gulden ◽  
W. A. Compton

This is a two-part paper, which stresses the materials science approach to understanding dust erosion mechanisms. The first part is an experimental phase, studying the effects upon solid-particle erosion, of such material and environmental variables as target alloy composition and heat-treat condition; dust particle velocity, size, concentration, velocity, and kinetic energy; carrier-gas true temperature and impingement angle. All test variables and their limits were chosen to simulate the range of engineering conditions and erosive environments encountered in helicopter turbine service. Actual erosion data are compared with erosion levels predicted by existing theories on particulate erosion. The second part is a diagnostic phase, programmed to detect and study visible phenomena associated with the erosion processes, using high-magnification electron microscopy. Phenomenological evidence obtained from the erosion surfaces and erosion products are used to define probable physical models of the erosion mechanisms.


1967 ◽  
Vol 54 (1_2) ◽  
pp. 1-12 ◽  
Author(s):  
Giulio Milazzo ◽  
Micheline Sotto ◽  
Claude Devillez

2007 ◽  
Vol 298 ◽  
pp. 202-206 ◽  
Author(s):  
F. Brunner ◽  
V. Hoffmann ◽  
A. Knauer ◽  
E. Steimetz ◽  
T. Schenk ◽  
...  

2010 ◽  
Vol 30 (8) ◽  
pp. 2412-2416 ◽  
Author(s):  
董伟 Dong Wei ◽  
原遵东 Yuan Zundong ◽  
卢小丰 Lu Xiaofeng

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