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A combination of optical microscopy, confocal Raman microspectroscopy and electron microscopy was used to investigate the spatial distribution, morphology and crystal phase of the calcium phosphate mineral, as well as to study transformation of the mineral phases during the hydrogel mineralization process and upon incubation in a simulated body fluid.
Since MEPE protein has an important role in the regulation of the skeleton mineralization process and since the mineralized tissue is a critical innovation in vertebrate evolution, the evolutionary study of this developmental gene could provide valuable insights on the adaptive diversification of morphological phenotypes in mammals.
Gradients in mineral concentration were observed in this secondary mineralization process, and incremental growth lines reminiscent of other normal and pathological calcifying tissues [ 22- 27, 33] were also visible.
Given their binding affinities for calcium and apatite, certain proteins may interact with the apatite crystals during the mineralization process and as such they are expected to be enriched in mineralized tissues like bones and teeth.
Benitez et al. (1999) have reported that decomposition of organic materials by earthworm accelerates the N mineralization process and subsequently changes the N profile of the substrate.
The earthworms drive the mineralization process and convert a fraction of calcium from binding form to free forms, resulting in its enrichment in worm casts.
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Protozoan grazing on rhizobacteria stimulates microbial mineralization processes and thereby indirectly nutrient cycling.
Bacterivores, such as protozoans, contribute significantly to mineralization processes and key ecosystem functions in soil.
Direction of microbiological processes in rhizosphere soil of chickpea plants was determined using the coefficient of mineralization, which allows to characterize the processes and intensiveness of mineralization processes and oligotrophic index that characterizes the oligotrophic degree of microbial communities.
The focus of microbiological processes was determined using the mineralization coefficient, which permits to characterize the intensity of mineralization processes and oligotrophic index of microbial communities.It was noted that the intensity of mineralization processes was higher in variants with colloidal solution of nanoparticles of molybdenum.
More specifically, hydrochemical composition and ionic ratios were used to identify the origin of groundwater mineralization processes and saltwater intrusion in coastal areas (Bear et al. 1999; Djabri et al. 2008; Reddy et al. 2010; Agoubi et al. 2012).
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