Sentence examples for grains of material from inspiring English sources

Because most of the grains of material have nearly identical orbits, collisions between them are relatively mild, which allows the particles to stick and remain together.

The meteoritic remains may even contain ancient grains of material cooked up in stars that predate the sun.

The substrate obtained by spin-coating process generates a homogeneous layer across the surface, with very low roughness [21] and small grains of material, so the current applied to the surface is distributed homogenously.

In many cases, the eye is then able to interpolate from the luminescence of even a few remaining grains of material or pigment and partially reconstruct the lost fragments, giving clues towards the original appearance of the object.

The sediments seen by Mars Express are typically low-density grains of material that have been eroded away by water and carried off to their current location.

Researchers have known for decades that, when shaken or stirred, a mixture of two grainy materials will spontaneously separate if the grains of one material are much larger or denser than the grains of the other.

This most likely indicates that no natural orpiment was used as a starting material for the synthesis of the pigment, since otherwise grains of this material would have been found in the thin section [21].

HR TEM showed high crystallinity of some grains of this material (Fig. 3) with the interplanar distances of 0.34 0.37 nm.

This is particularly important for the automotive and naval industry, and those applications that involve abrasive phenomena, such as presence of dust, sand or grains of hard material.

If water clings more tightly to the grains of one material than to those of the other, the grains may separate even if they are otherwise identical and would ordinarily mix, the researchers report in a paper to be published in Physical Review Letters.

All three stable elements occur in heavy mineral sands ore deposits, which are placer deposits formed, most usually in beach environments, by concentration due to the specific gravity of the mineral grains of erosion material from mafic and ultramafic rock.