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Further, change in orientation from lying-down to standing-up state was supported by contact angle analysis.
During the first round of debriefing interviews, it was found that the change in orientation from one item to another was confusing for many respondents and led to erroneous scoring.
One of the most important conclusions from these comparisons is that the smaller Ala215 signature residue in ROCK1, analogous to Thr183 in PKA, allows inhibitors to bind deeper in the ROCK1 active site cleft, resulting in a ∼7° change in orientation from the PKA-bound structure.
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A similar example of this behavior is shown by the fiber given in Supporting Information Figure S5, where the zone axis changes in orientation from close to [0 1 0] to [−2 8 −1] over a length of 300 nm, before switching to the original orientation again.
The mean change in orientation decreased from the unburnt to burnt side of the flame brush and appears to be influenced by the overall flame shape.
Petraeus, too, is a loyal Army man, but he has distinctive views about military doctrine; he has long advocated a change in orientation by the Army, away from preparations for formal warfare between governments and toward the challenges of counter-insurgency and nation building.
With continuous conformational variability, it can thus be mathematically impossible to unambiguously distinguish changes in particle orientation from changes in particle conformation with only a single 2D image for each particle.
From restlessness, to a change in orientation and breathing, the dogs seem to adapt to the needs of the patient.
In VN we observed a change in preferred orientation from (111) to (200) at 300°C growth temperature with normal incident ion-beam energy of higher than 350 V.
For the period around 0.5 Ma, as inferred from the reconstructed flow directions of MTDs and bathymetric analyses (Kanamatsu et al. 2014), seamount subduction could have affected the study area (Fig. 1; Kimura et al. 2011) and resulted in a change in slope orientation from NE SW to NW SE (the present slope).
It consists of aligned volcanoes over a width of ∼50 150 km, presenting a marked change in the orientation from NNW-SSE to NNE-SSW around ∼23° N. Similarly, the aseismic West Mariana Ridge is a remnant arc that separated from the Mariana active volcanic arc ∼7 Ma ago (Karig and Glassley 1970; Gardner 2010).
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