Sentence examples for mineral stability from inspiring English sources

hMSC cultured under osteogenic conditions, after 10 days exhibited robust von Kossa staining, suggesting calcification and mineralization, and VDR staining which is responsible for mineral stability [ 28– 30].

Here the effects of aS0 on trace element speciation and sulfide mineral stability are briefly discussed.

A mineral stability diagram is consistent with observations from the field.

Our results corroborate previous studies that have demonstrated a direct relationship between intrinsic mineral composition and mineral stability.

In addition, we further demonstrate that ion composition and pH of the surrounding solution environment can significantly influence mineral stability.

Since then they have been used to understand, predict and describe physico-chemical phenomena such as osmosis [2], mineral stability [3] and cholesterol biosynthesis [4, 5].

Such disequilibrium features provide a wealth of information on the reaction history of the sample and, by comparison with experimental studies of mineral stabilities, can also constrain the quantitative pressure-temperature history of the rock during metamorphism.

In diagrams of pressure-temperature fields of stability of silica minerals, stability fields are not shown for keatite, melanophlogite, opal, or the low forms of tridymite and cristobalite because they have not been demonstrated.

Nanostructures, which frequently occur in geologic materials, may directly control mineral phase stability, mineral water interface chemistry, geochemical reaction kinetics, geo-fluid migration and transport, and even global biogeochemical cycles as a whole.

DNA Lipoplex presence in mineral, DNA Lipoplex stability (vs. coprecipitation time), and transfection efficiency (determined with C3H10T1/2 cells) as a function of coprecipitation time, DNA Lipoplex concentration, and DNA incorporation method were studied.

These results suggest variation in organo-mineral complex stability is associated with degree of crystallinity of the mineral phase.