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Cl isotope compositions are homogeneous within individual grains.
Some individual grains are twinned in two or more ways.
The sound of the flute is broken into individual grains that gradually loose cohesion.
Low-resolution scanning electron microscopy magnifies the shapes of individual grains.
Individual grains were characterized by ESEM-EDAX, X-ray diffraction, and Raman spectrometry.
This is a consequence of different drying histories for individual grains.
The surface roughness is determined by the micro roughness on the individual grains.
In most cases, individual grains thus retain characteristics imparted to them in the area where they formed.
The lack of cohesion meant that at the surface of the sand individual grains could be moved laterally with ease.
We find, within individual grains, spatially correlated heterogeneity in short-circuit current and open-circuit voltage up to 0.6 V.
In addition, grain boundaries promote the lattice rotation of individual grains in shear bands but suppress that of individual grains within non-shear bands.
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