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The origins of the measured lattice strains and peak intensity changes are examined in the following discussion.
In this paper, the dynamics of the changes are examined on a specific Greek island.
Changes of 27% in cohesion and 8% in the friction angle were found due to the attack of the interface and consequences of the changes are examined.
The changes in key indicators for 1997 2007 are tracked and the effects of water-saving policies on these changes are examined.
These changes are examined in a comprehensive fashion, the drive and transfer admittances and the acoustic far field being calculated for excitation at prescribed force amplitude, at prescribed velocity amplitude, and for prescribed input power.
Also, when fractional rather than absolute biodiversity changes are examined, a second peak at about 32 Myr emerges at the 0.1 confidence level.
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The phase formations and microstructural changes were examined by SEM and X-ray diffractometry (XRD).
Phonetogram contour changes were examined, with the primary focus on expansion of frequency range and/or intensity control.
Cell morphology changes were examined by FESEM.
Morphological changes were examined immediately using phase-contrast inverted fluorescence microscope (40×) under UV lamp.
Time-course changes were examined by serial sacrifices on post-exposure days 1, 7, 14, and 28 (phosgene only).
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