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Exact(6)
Shear and tensile moduli of oriented samples were determined over the temperature range −100°C to 190°C.
The thermal properties and fine structures of the isotropic and oriented samples were investigated using thermal analysis and X-ray diffraction methods.
Fifty-four oriented samples were taken from six sites by in situ drilling.
The oriented samples were scanned over an interval of 5° 60° (2θ) at a scanning speed of 1.375°/min for every 0.03° (2θ) step.
Hence, we were unable to retrieve reliable paleomagnetic results from A2. Forty-four oriented samples were collected at five sites (sites 12, 13, 14, 15, and 16) from the IWT.
Forty-six oriented samples were collected at six sites from the first eruptive cycle: two (sites 11 and 18) in A1 and four (sites 1, 2, 3, and 4) in A3 (Figures 1 and 2).
Similar(54)
The mechanical properties of these oriented samples are comparable with commercially available PET and PA-6,6 melt spun fibres.
The mechanical properties of the oriented samples are compared together with relevant structural data, and their differences discussed.
For fiber-textured samples, it is quantitatively shown that highly oriented samples are equivalent to polycrystals with a high density of low-angle misorientations, while completely random (untextured) materials are equivalent to microstructures with a high probability of large-angle misorientations.
The highest Schmid factors for <1−10>{111} slip in the (100) and (234) oriented samples are 0.408 and 0.422, respectively.
The true stress versus true strain data for in situ TEM tensile tests for multiple slip and single slip oriented samples is shown in Figure 1.
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