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The estimated resistivity changes are approximately ±5%, and the polarity differs between depths of 100 and 400 m (Fig. 9).
However, the thermal efficiency, since both useful power and heat transfer rate are decreased and the slope of their changes are approximately equal, undergoes little changes.
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At 1973 K, the corresponding changes were approximately 16% during 220 h.
Subtle strain variations were also seen at 21 15 22 20 on 26 January and 15:05–16:00 on 27 January, prior to the second and third sub-Plinian eruptions (Fig. 5(b and c)), and the amplitudes of these precursory strain changes were approximately 2 × 10−9, somewhat smaller than those associated with the first eruption.
For all other individuals the corresponding changes were approximately 1 percentage point or lower.
However, fetal weight was reduced slightly, and the incidence of minor skeletal changes was approximately three to four times that among fetuses of control dams that were not pair-fed.
Reported thresholds for F-FDG-PET for determining metabolic changes being approximately −34% to +52% for individual centres and −27% to +37% after centralised QA (Velasquez et al, 2009).
Demineralization of exposed dentin occurs already at pH 6.2 6.4 compared to pH 5.5 5.7 for enamel and acid attacks in the plaque/biofilms cause destructive hard tooth changes being approximately twice as rapid compared to similar processes in enamel [ 51– 51].
For I C 2 on average both oxy- and deoxy-hemoglobin changes were approximately equal by magnitude and, on average, opposite by sign. Figure 4 shows examples of the time courses of I C 1 and I C 2 for three subjects during the repetitive BH exercises.
The magnitude of change is approximately ± 5 m.
Because the slope is relatively linear, the rate of change is approximately the same each year.
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