Sentence examples for small-grained from inspiring English sources

A weak LPO and lower dislocation density of olivine and the presence of four-grain junctions in the small-grained area are clear evidence that grain-boundary sliding influenced the deformation of olivine (Hirth and Kohlstedt 1995).

(H) Garnet grains found in the small-grained area (sample 379).

It is also found that the dislocation density in the mylonite zone is much lower than that of the large-grained area (Figure 8G,H), and there are four-grain junctions preserved in the small-grained area (Figure 8H).

(H) Four-grain junctions (yellow arrows) found in the small-grained area in mylonite (sample 379).

Four-grain junctions were also found frequently in the small-grained area (Figure 8H).

This is a weathered layer that contains an accumulation of humus (decomposed, dark-coloured, carbon-rich matter) and microbial biomass that is mixed with small-grained minerals to form aggregate structures.

The grain size of the aluminium used in the cathode was varied and small grained devices were found to have degraded faster.

On the basis of grain size, the peridotite sample can be divided into three different areas: large, medium, and small grained.

In hopes of toughening such small grained metals, researchers in the United States and Switzerland led by physicist Eduardo Bringa at Lawrence Livermore National Laboratory in California carried out both supercomputer simulations and experiments on nanocrystalline copper that was exposed to an intense shock wave from a high powered laser.

In fact, it is possible to classify the deposited films as large grained (~ 15 nm) with a reduced lattice constant (~ 4.15 Å) and low compressive residual stresses for lower applied substrate biases, and as small grained (~ 4 nm) with an increased lattice constant (~ 4.25 Å) and high compressive residual stresses for applied biases of − 100 V or more.

We performed column experiments using a synthetic porous medium, in which a substantial part of the sorption sites was concentrated in regions within small grained aggregates that were accessible only by diffusion, a feature often found in natural soils and sediments.