On the other hand, BBB disruption has been observed at several hours after ischemia/reperfusion [26, 27].
These fluttering oscillations have been observed at several dams and artificial waterfalls and, depending on their scale, have been considered to be either attractive or objectionable.
Although similar phenomena have been observed at several volcanoes, the sequence was for the first time correlated with the growth and shrinkage of the lava in the crater and compared with the entire sequence of the eruption activity.
Already grouting failures related to slippage of the transition piece relative to the monopile due to weakening of the adhesion between the grout and the steel have been observed at several windfarms during the construction phase.
Presently, multiple cycles of eruption and intrusion have only been observed at a handful of volcanoes (e.g., Sigmundsson et al., 2010; Lu et al., 2010; Biggs et al., 2010a, b; Bagnardi et al., 2013), although cycles of activity within long-lasting eruption have been observed at several more (e.g., Poland et al., 2008; Peltier et al., 2010).
Populations had been observed at several other sites throughout the bay by the end of the 1980s, and by the mid 1990s Carcinus was common throughout Tokyo Bay and had spread as far south as Dokai Bay [35].
Microstructural analysis of the samples revealed the poor corrosion resistance of high density and low density graphite and severe attack was observed at several places on the surface.
Strong fluorescence was observed at several sites of the cecal mucosa, irrespective of cancer cell type.
Quadratic effects of the grinding level on rumen fermentation parameters were observed at several sampling times for RAW.
These previous and our findings suggest that ROS generation might be observed at several hours after ischemia/reperfusion.
Evidence of soil nonlinearity can be observed at several other stations, such as 51CXQ, although not evident.
