[1] Synchrotron X-ray computed microtomography (mCT) was applied for the first time to clasts of pumice and scoria generated by active, explosive volcanoes characterized by a range of eruptive styles (mild Strombolian to Plinian) and magmatic composition (basaltic to trachytic). The obtained two-dimensional (2D) tomographic images, corresponding to sample views at different rotation angles, were processed to reconstruct three-dimensional (3D) volumes and then used to make 3D measurements of vesicularity, vesicle number density, volume and connectivity for quantitative characterization of the investigated tephras. The results indicate a positive correlation between vesicle number density and eruption intensity that is used to investigate modes of magma degassing in explosive eruptions. In addition, the vesicle geometry affecting the connected gas flow pathways in pyroclasts from Strombolian eruptions is determined and related to the known permeabilities. Implications on the dynamics of explosive eruptions is discussed and, ultimately, used to quantitatively discriminate between different eruptive styles.

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Dentinal damage may occur following rotary and reciprocating instrumentation.

The evaluation of bread quality can be carried out by performing a nondestructive investigation of its microstructure, which in turn can be performed by adapting image analysis techniques that enables one to obtain rapid, objective, and quantitative information. A suitable and reliable experimental methodology to investigate the porous structure of bread by means of the numerical image processing, and without any sample preparation, has been presented in this work. Different types of breads having varying degrees of porosity were studied by X-ray computerized phase-sensitive microtomography for the acquisition of digital high-resolution images. After acquisition, suitable numeric algorithms were applied to slice reconstruction. Finally, 3D images were rendered and analyzed.

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