Sentence examples for modes of grain from inspiring English sources

Exact(2)

From left to right, X-ray image, photo, sedimentary units and the 1st and 2nd modes of grain size, and the sedimentological parameters d10 and d90 are presented.

Five basic modes of grain coarsening were deduced from the measurements, which include: anisotropic (I) and isotropic (II) growth (or shrinkage); movement of grain boundaries resulting in no change in volume but a change in shape (III); movement of grain boundaries resulting in no change in volume and mosaicity, but a change in crystallographic orientation (IV); no movement of grain boundaries (V).

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The gray scale indicates the mode of grain diameter.

(B) The first mode of grain size versus water depth based on samples from seafloor types B, C and D show no correlation.

For sampling positions see Figs. 2 and 3. (A) The first mode of grain size versus water depth, based on samples retrieved from seafloor type A, showing a decreasing first mode with increasing water depth.

The mode of the grain size of samples retrieved from seafloor type E is independent of the water depth.

The analyses revealed only subtle differences between the life-limiting and the long-lifetime failure in terms of deformation modes of the faceted grain(s) and their first nearest neighbors on a given section.

The subtlety of differences indicates that the facet plane and the deformation modes of the faceting grain and its neighbors as determined from a 2D section may not be the most discriminating crack-initiation factors between the two lifetime regimes in this alloy.

Multiple agriculture zones, multiple transportation modes for the transport of grain and biofuel, multiple biofuel plants, and multiple market centers were considered in this model, and the price of the resources, the yield of grain and the market demands were regarded as interval numbers instead of constants.

The acoustic velocities and calculated Young's and shear moduli decreased by a large percentage with an increase in the number of cycles in all cycle modes due to growth of grain boundary voids.

The modes of contact between grains contain mostly lineal contact, then lineal-concave and convex contact.

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