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In the impregnation technique, silica particles were added, then removed by dissolution in alkaline medium.
The detachment of hydrogen bond between the chains in polymer complexes was investigated during the dissolution in alkaline solution, ionic liquid and tertiary amine N-oxide.
Formation and dissolution of oxide on copper under transpassive conditions, i.e. during OER and transpassive dissolution, in alkaline electrolyte was investigated by a combination of electrochemical techniques and in situ and operando Raman and photoluminescence (PL) spectroscopy, as well as spectropscopic ellipsometry.
Under conditions of electrochemical diagnostic experiments (performed in 0.1 mol dm−3 KOH): (i) the phosphomolybdate adsorbates are removed from the interface as they undergo dissolution in alkaline medium; and (ii) the Au nanoparticles (Au loading, 30 μg cm−2) remain well-dispersed on the carbon as evident from transmission electron microscopy.
Dissolution in alkaline concentrated urea enhanced the dissociation of acid-soluble constituents.
The acid-soluble constituents can be dissociated by acidification after dissolution in alkaline medium [13].
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It was also observed that complete sample re-dissolution in alkaline solutions may form suspended particles, which may reduce spectral quality and undermine TP and OP detectability.
This paper reports that addition of reduced graphene oxide (rGO) in MgCo2O4 improves the binding of Mg with Co thereby minimizing magnesium dissolution in aqueous alkaline electrolytes and the resulting MgCo2O4/rGO electrodes offered impressive improvements in charge storage properties.
In contrast, mineral dissolution in an alkaline environment (pH 13) resulted in a rapid (< 10 h) increase in carbonate, followed by a slow (10 s to 100 s of hours) increase in silica concentration, likely from montmorillonite, muscovite, and kaolinite dissolution.
It was also likely that the hydrolysis of extractive components such as suberin and long chain fatty acids, and their subsequent dissolution in the alkaline solution, was representative of the efficiency of removal of the majority of the extractive compounds [ 42].
Dissolution of hardness causing Ca and Mg from bed rock and anthropogenic sources, fluoride dissolution from bedrock in alkaline environment and salinity from natural and anthropogenic sources were identified to be the main factors influencing the ground water quality in both the clusters.
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