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These major differences in mineralization can be found in the lower second premolar buds [28 32].
By controlling all the parameters, complete dye mineralization can be achieved within an equilibration time frame of 40 min, using a mere 100 mg of the photocatalyst material.
This study shows that through further optimization a very high degree of mineralization can be achieved, with compositions matching that of bone.
This suggests that petroleum hydrocarbon mineralization can be underestimated if it is determined based on concentrations of dissolved oxidants and reduced species.
Indeed, 'epitaxial' relationships have been calculated; but in practice, it has not been demonstrated that intrafibrillar mineralization can be accomplished via this route.
We hypothesized that hydroxyapatite crystal nucleation and matrix mineralization can be significantly increased by mineralization-inducing (MIP) and integrin binding motif (RGD) peptides presented on biomimetic nanoparticles.
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The mineral precipitation orientation change, and the growth of later marcasite minerals, can be explained by the absence of the worms at this stage of tube mineralization.
Although a globular mineralization pattern can be found in normal teeth, where interglobular areas eventually mineralize, extensive areas of globular dentin are often associated with biomineralization abnormalities such as vitamin D deficient X-linked hypophosphatemia, vitamin D deficiency [ 29– 31], and DGI-I.
To create a silica nanotube forest, the aforementioned flagella mineralization method can be used.
Carbon mineralization rate can be used to quantify the impact of different organic and inorganic materials on soil functions.
Gross organic P mineralization rates can be quantified by an isotopic dilution method using 33P labeling of soil.
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