Sentence examples for material to be characterized from inspiring English sources

The material to be characterized is placed between two layers of materials with known thermophysical properties.

However, projected two-dimensional (2D) images acquired from three-dimensional (3D) nanostructured materials can provide limited information, and sometimes, information is missing; the development of nanotechnology requires the relationship between the 3D structure and properties of the material to be characterized on the nanometer scale (Ercius et al. 2015).

Therefore, each analyzed sample may have its own identifier while its (source) material sample to be characterized has a different identifier (the Material Source Name). Figure 5 and Figure 6 show an example of how to use the Study and Assay files, respectively, to represent the assay data (metadata, summary data) of each sample analyzed in a size characterization assay using DLS technique.

We show the CH3NH3PbI3– x Cl x material evolution to be characterized by three distinct structures: a crystalline precursor structure not described previously, a 3D perovskite structure, and a mixture of compounds resulting from degradation.

The wettability of such materials has to be characterized experimentally under the operating process conditions.

For how are material objects now to be characterized?

The EPR signal of these materials is shown to be characterized by the following parameters: g = 2.0022 ÷ 2.0023, ΔH pp ≅ 2 G.

UV-visible spectroscopy provides an extremely powerful methodology to investigate molecular structures of high molecular weight aromatic materials, not amenable to be characterized by analytical techniques as gas-chromatography, mass spectrometry, etc.

Thus, as shown in Figure 5, the first column of the Study file (Material Source Name REF) represents the identifier of the material sample that is to be characterized.

The material behavior of this elastomer needs to be characterized for the purpose of performing LS-DYNA simulations.

Comparison with piezometric data showed that the estimated hydraulic conductivities of most materials were too high; the low piezometric levels especially indicate that the materials composing the upstream face as well as the alluvium and blast-fill material must be characterized by low to very low permeability.