scholarly journals The system beryllia-alumina-titania: phase relations and general physical properties of three-component porcelains

1952 ◽  
Vol 48 (4) ◽  
pp. 298 ◽  
Author(s):  
S.M. Lang ◽  
C.L. Fillmore ◽  
L.H. Maxwell
Keyword(s):  
Physical Properties ◽  
Phase Relations ◽  
General Physical

Phase Relations along the Cu2S(Sb2S3, PbSb2S4, Pb5Sb4S11)–PbCuSbS3 Joins in the Pseudoternary System Cu2S–PbS–Sb2S3 and Physical Properties of (Sb2S3)1 –x(PbCuSbS3)x Solid Solutions

2018 ◽  
Vol 54 (12) ◽  
pp. 1199-1204
Author(s):  
O. M. Aliyev ◽  
D. S. Ajdarova ◽  
R. M. Agayeva ◽  
T. F. Maksudova ◽  
Sh. H. Mamedov
Keyword(s):  
Physical Properties ◽  
Solid Solutions ◽  
Phase Relations

The general physical properties of manganese metal

1968 ◽  
Vol 13 (1) ◽  
pp. 97-114 ◽  
Author(s):  
George Terence Meaden
Keyword(s):  
Physical Properties ◽  
General Physical

Observations on the Physical Properties of Sea-Ice at Hopedale, Labrador

ARCTIC ◽  
1958 ◽  
Vol 11 (3) ◽  
pp. 134 ◽  
Author(s):  
Wilford F. Weeks ◽  
Owen S. Lee
Keyword(s):  
Sea Ice ◽  
Physical Properties ◽  
Air Force ◽  
Sea Water ◽  
Field Studies ◽  
Water Levels ◽  
Cambridge Research ◽  
Freezing Period ◽  
Before And After ◽  
General Physical

Preliminary results are reported of field studies 1955-56 by the U.S. Air Force Cambridge Research Center, the Hydrographic Office and SIPRE on the general physical properties of sea ice; methods of measurement are described. Characteristics of sea water during the freezing period are outlined: formation, structure, and salinity of the initial ice cover, formation and characteristics of infiltrated snow-ice, growth of the ice and influencing factors, density of the ice at various periods, and crack formation are discussed. Data on the salinity of sea ice formed during during wave action and that of sheet-ice, hourly averages of air and ice temperatures at various levels, snow and slush density and thickness, observed slush levels and theoretical water levels are shown. Salinity of ice before and after the slush layer froze, and that of deteriorating ice , salinity of ice vs. ice thickness, thickness of ice versus degree-days, the density of the ice, and measured ice densities vs. theoretical density of air-free sea ice at -15 C are figured and discussed. The orientation of sea ice c-axes and of infiltrated snow-ice c-axes are diagrammed.--From SIPRE.

scholarly journals Phase relations, crystal chemistry, and physical properties of MgZn2-type Laves phases in the Mn-Cu-Si and Mn-Ni-Si systems

2013 ◽  
Vol 88 (17) ◽  
Author(s):  
X. Yan ◽  
M. W. Pieper ◽  
H. Michor ◽  
G. Hilscher ◽  
M. Reissner ◽  
...  
Keyword(s):  
Physical Properties ◽  
Crystal Chemistry ◽  
Phase Relations ◽  
Laves Phases

GENERAL PHYSICAL PROPERTIES OF SOILS IN THE CHIRCHIK BASIN

2021 ◽  
Author(s):  
R Kurvantaev ◽  
Z Khalilova
Keyword(s):  
Physical Properties ◽  
General Physical

Изучение современное состояние обшие физичкские свойства почв Чирчикского бассена является актуальным вопросам. Во всех изученных геоморфологических районах удельная масса почвы колеблется от 2,52 до 2,71 г/см3. Оптимальная плотность сложения (1,13-1,38 г/см3) было отмечено на целинных горнокоричневых, орошаемых типичных сероземах, серозёмно-луговых и луговых почвах. Общая порозность горнокоричневых почвах очень высокая (53-61%), богарных тёмных сероземах, орошаемых типичных серозёмах, серозёмно-луговых и луговых почвах составляет 50 - 56%.

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