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Exact(6)
No {123}<111> slip system traces were observed.
At large strains where significant γ′-particle shearing occurs, the classical straight and thin slip bands along the {1 1 1} traces were observed.
Similar mitochondrial respiration traces were observed in cortex.
However, similar irregular dynamics in the FRET time traces were observed at 100 nM Pif1 and 20 µM ATP as seen for DD31 (bottom right).
Quantitatively similar [O2] traces were observed with all the other tested QH2 as well as with α-tocopherol and its synthetic analog 6-hydroxy-2,2,5,7,8-pentamethylchromane (HPMC).
In both experiments, no cellobionic acid was detected in a quantifiable amount during the hydrolysis, although traces were observed at high values of cellulose conversion or at long hydrolysis times using Cellic CTec2.
Similar(54)
The upper gray traces are observed, and the lower black traces are synthetic waveforms.
Red traces are observed at stations on the deep trench of the Kanto Basin, as shown in Fig. 2.
An example of waveform fit is displayed in Fig. 2, where red traces are synthetic seismograms and black traces are observed ones.
For the local deformation structure, pronounced and graded deformation traces are observed which often pass over the neutral fiber of the twisted wire and which are obviously reflecting domains of high geometrically necessary dislocations content.
The HD shows large absolute values not only along the Kushigata Range fault zone (KRFZ) and the Tsukioka fault zone (TFZ), which constitute the EBFZNP, but also along the area between the two fault zones where no surface fault traces are observed.
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