scholarly journals Electromagnetic Transport Properties of La0.7Sr0.3MnO3/xZn0.95Co0.05OComposite

2016 ◽  
Vol 06 (04) ◽  
pp. 77-82
Author(s):  
彬 庄
2008 ◽  
Vol 181 (9) ◽  
pp. 2123-2126 ◽  
Author(s):  
C.S. Xiong ◽  
Y.F. Cui ◽  
Y.H. Xiong ◽  
H.L. Pi ◽  
X.C. Bao ◽  
...  

2015 ◽  
Vol 462 ◽  
pp. 108-113 ◽  
Author(s):  
A.A. Gapud ◽  
N.T. Greenwood ◽  
J.A. Alexander ◽  
A. Khan ◽  
K.J. Leonard ◽  
...  

2011 ◽  
Vol 60 (10) ◽  
pp. 107306
Author(s):  
Yu Hong-Fei ◽  
Zhang Lu-Shan ◽  
Wu Xiao-Hui ◽  
Guo Yong-Quan

2001 ◽  
Vol 33 ◽  
pp. 28-36 ◽  
Author(s):  
K. M. Golden

AbstractSea ice is distinguished from many other porous composites, such as sandstones or bone, in that its microstructure and bulk material properties can vary dramatically over a small temperature range. For brine-volume fractions below a critical value of about 5%, which corresponds to a critical temperature of about −5°C for salinity of 5 ppt, columnar sea ice is effectively impermeable to fluid transport. For higher brine volumes, the brine phase becomes connected and the sea ice is permeable, allowing transport of brine, sea water, nutrients, biomass and heat through the ice. Over the past several years it has been found that brine transport is fundamental to such processes as sea-ice production through freezing of flooded ice surfaces, the enhancement of thermal and salt fluxes through sea ice, nutrient replenishment for sea-ice algal communities, and to sea-ice remote sensing. Motivated by these observations, recently we have shown how percolation theory can be used to understand the critical behavior of fluid transport in sea ice. We applied a percolation model developed for compressed powders of large polymer particles with much smaller metal particles, which explains the observed behavior of the fluid permeability in the critical temperature regime, as well as Antarctic data on surface flooding and algal growth rates. Moreover, the connectedness properties of the brine phase play a significant role in the microwave signature of sea ice through its effective complex permittivity and surface flooding. Here we review our recent results on brine percolation and its role in understanding the fluid and electromagnetic transport properties of sea ice. We also briefly report on measurements of percolation we made on first-year sea ice during the winter 1999 Mertz Glacier Polynya Experiment.


1988 ◽  
Vol 102 ◽  
pp. 165-174
Author(s):  
C. de Michelis

AbstractImpurities being an important concern in tokamaks, spectroscopy plays a key role in their understanding. Techniques for the evaluation of concentrations, power losses and transport properties are surveyed, and a few developments are outlined.


Author(s):  
Alain Claverie ◽  
Zuzanna Liliental-Weber

GaAs layers grown by MBE at low temperatures (in the 200°C range, LT-GaAs) have been reported to have very interesting electronic and transport properties. Previous studies have shown that, before annealing, the crystalline quality of the layers is related to the growth temperature. Lowering the temperature or increasing the layer thickness generally results in some columnar polycrystalline growth. For the best “temperature-thickness” combinations, the layers may be very As rich (up to 1.25%) resulting in an up to 0.15% increase of the lattice parameter, consistent with the excess As. Only after annealing are the technologically important semi-insulating properties of these layers observed. When annealed in As atmosphere at about 600°C a decrease of the lattice parameter to the substrate value is observed. TEM studies show formation of precipitates which are supposed to be As related since the average As concentration remains almost unchanged upon annealing.


1993 ◽  
Vol 3 (12) ◽  
pp. 2173-2188
Author(s):  
N. G. Chechenin ◽  
A. V. Chernysh ◽  
V. V. Korneev ◽  
E. V. Monakhov ◽  
B. V. Seleznev

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