The chemical components were closely related to the particle sizes of constituent minerals.
A modified sintering process, where the relative particle sizes of constituent phases are controlled to minimize interdiffusion between starting materials, has been proposed to achieve the formation of a composite having tailored physical properties.
In the case of simple shear flow, the value of 〈i〉 is approximated by the following universal function of NDA, the ratio of the representative hydrodynamic drag force and the adhesive force, independently of the number, the size and the size distribution of constituent particles, and the minimum separation distance between particle surfaces.
The permeability of a rock is dependent on the geometric properties of the rock, such as porosity, shape and size distribution of constituent rock grains, and degree of cementation of the rock.
The data suggests that the fraction of M A constituent is not influenced by grain size, but the size of M A constituent is influenced by the prior austenite grain size, which consequently governs toughness.
The US, Australia and many other countries have had to find ways of managing the gross inequalities in the size of their constituent parts.
Conglomerates are usually subdivided according to the average size of their constituent materials into pebble (fine), cobble (medium), and boulder (coarse).
In other studies he showed that the size of the constituent atoms was of prime importance in explaining mineral composition and that crystal hardness is determined by the distance between and the charge of adjacent ions (charged atoms).
In several works published during the 1860s, Graham observed that low diffusivity, the absence of crystallinity, and the lack of ordinary chemical relations were some of the most salient characteristics of colloids and that they resulted from the large size of the constituent particles.
The size of the constituent grains is also an important parameter.
