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To explore the possible effect of the Black Death on genetic diversity, it would be intriguing to analyse remains from medieval burials sites with well characterised layers from various time periods before and after AD 1350.
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Pore diameters are about 50 μm in the low-porosity layers, but can be up to a few hundred microns in the layers characterised by coarser grains and a higher porosity (Fig. 8d).
The first three habitat types were generally characterised by field layers kept permanently shorter than 5 cm, whereas the latter three habitat types were characterised by field layers growing dense and tall (≥15 cm) during late incubation and nestling care (field layer height estimated by eye at four occasions during the breeding season [35], [37]).
Hybrid structures are idealized as structures with homogeneous layers characterised by different thermal conductivities.
The layers, characterised by Scanning Electron Microscopy, Fourier-Transform Infrared Spectroscopy and X-ray Photoelectron Spectroscopy, have been successfully functionalised with diene groups.
Well adherent coating layers characterised by loadings between 1.1 2.2 mg/cm2 and thickness of 10 20 μm have been obtained upon dip-coating deposition.
A heat transfer problem in strongly heterogeneous materials, and a groundwater flow problem in presence of geological layers characterised by different hydraulic conductivity, are taken as engineering applications to test the capabilities of the CV-HRBF method to handle multi-zone problems.
The remaining medieval walls, characterised by alternative layers of limestone and flat brick, were covered with stucco.
Conversely, backward-type terminations in agranular cortex can be characterised by avoiding layer 3, and/or being concentrated in layer 1 (see Fig. 6).
A new test rig for thermal fatigue testing was used to investigate and characterise surface layer degradation of indefinite chill double pour (ICDP) cast iron hot work roller.
However, the most notable application of Os isotopes in geology has been in conjunction with the abundance of iridium, to characterise the layer of shocked quartz along the Cretaceous Paleogene boundary that marks the extinction of the dinosaurs 66 million years ago.
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