Exact(8)
Qualitative and quantitative compositions (Table 1) of insulin-loaded microspheres were used for designing the formulation.
Suitability of water for irrigation is a function of its mineral compositions (Table 2).
Three starting compositions (Table 1) were prepared as gel mixtures, following the procedure of Hamilton and Henderson ([1968]).
Starting materials in this study were Pb-, Sr-, and Rb-bearing glasses (0.7 wt.% for each element) of haplogranite (HGR) and approximately jadeite (Jd) compositions (Table 1).
Before analysis, samples were assigned to visual colour groups distinguished as clearly as possible by eye to record the variability of colours produced from much less varied chemical compositions (Table 1).
Because of the differences in bulk compositions (Table 1), and pressure and temperature conditions, H2O is expected to play a fundamental role in modifying the liquids surface of these carbonatitic liquids, as observed in silicate systems.
Their chemical compositions (Table 1) were characterized by lower concentrations of Na and K and a higher concentration of Al than the starting materials, thus resulting in a higher norm corundum and higher ASI than the starting materials.
Table 3 Saturation indices of Fe(OH 3, goethite, and hematite Date Fe(OH 3 Goethite Hematite 25 August 2012 −4.57 0.84 3.62 30 September 2012 −4.69 0.72 31 October 2012 2012 −4.62 0.79 3.52 Values calculated from groundwater compositions (Table 2) using PHREEQC (Parkhurst and Appelo 2013) and the phreeqc.dat thermodynamic database.
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