The rejection of entrained particles, in this case, inorganic ash forming minerals, depends on froth depth.
The proportion of healing minerals depends on exposure condition and the type of cementitious materials used.
The speed of reaction and dissolution of minerals depends on their reaction rate with acid and the exposed surface areas.
These results reveal that the frictional strength of montmorillonite is sensitive to hydration state and interlayer cation species, suggesting that the strength of faults containing these clay minerals depends on the physical and chemical environment.
The specific gravity of a mineral depends on the atomic weights of all its constituent elements and the manner in which the atoms (and ions) are packed together.
Thus, the cation exchange capacity (CEC) of clay mineral depends on the net elemental composition that varies with the geographical availability in the environment (Stucki 2006).
It should be noted that the bulk density is less than the grain density of the constituent mineral (or mineral assemblage), depending on the porosity.
In particular, during firing specific new minerals grow, depending on temperature and composition of clay (i.e., Ca-rich or Ca-poor clays).
After discharge from OWTS, some ammonium and organic nitrogen may be lost through assimilation into bacteria, sorption to clay minerals, or depending on pH, nitrogen in the form of ammonium may be lost through volatilization.
The combination of gravimetric measurements and 3H2O tracer studies furnished estimates of precipitated mineral mass; depending on the assumed identity of the predominant mineral phase(s), the porosity decrease associated with solute precipitation amounted to 6 24% of the initial porosity.
