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Experimental data is presented for in-plane loadings of longitudinal tension, transverse tension, and in-plane shear for three different temperatures consisting of 24, 66, and 93 °C (75, 150, and 200 °F).
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The arc vacuum system, which operates at cryogenic temperatures, consists of a 1.9 K cold bore which houses a 5 20 K beam screen.
The scale formed at higher temperatures consisted of a continuous Al2O3 inner layer and outer layer, changed from rutile TiO2 at temperatures below 1200 °C to a mixture of Al2TiO5 and TiO2 at 1300 °C [6].
Researchers (Wang et al. 2013) speculated that coal asphaltene liquefied at different temperatures consisted of similar aromatic structure, mainly 2 3 rings condensed nucleuses, by UV Vis absorption spectra of coal asphaltene in THF solvent.
In contrast to the behavior of sputter-deposited elemental metals and disordered alloys, the films deposited at the two higher temperatures consisted of refined microstructures and exhibited a low degree of texturing.
The genes that played a role in the response to elevated temperatures consisted of both highly conserved and coral-specific genes.
The three root-zone temperatures consisted of ambient, 5 °C below or 5 °C above ambient levels to encompass the natural variation that can occur across a vineyard site in spring.
The first and largest pre-defined group of genes (average over a total of 660 genes) up regulated at elevated temperatures consists of the genes under control of the house-keeping sigma factor σA.
The review focused primarily on quantitative studies of ambient temperature, consisting of studies using the time-series and/or case-crossover methods.
Thus, a sample with composition B consists of liquid C (43 percent CaSiTiO5 and 57 percent CaAl2Si2O8) and solid anorthite D. A sample at point E at a lower temperature consists of the solids titanite (F) and anorthite (G).
The thin film deposited at room temperature consisted of a mixture of Zn and Se.
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