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Sodium silicate solutions, commonly known as "water-glass", are water-based solutions containing dissolved glass.
These markedly different results are due to transport considerations, the most significant of which are the spatial variability in aqueous concentrations, and advection and diffusion of dissolved glass constituents into the backfill materials.
These conditions provide measurable concentrations of dissolved glass in the effluent while maintaining their concentrations below the point at which they significantly affect the dissolution process.
The authors reported that the dissolution values ranged from a few nanograms of silicon dissolved per cm (chrysotile and crocidolite) to several thousands of ng/cm silicon dissolved (glass wools) and that aramide and carbon fibers proved to be practically insoluble.
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The possible connection between the composition of the dissolving glass and its long-term behavior is discussed.
XPS and energy dispersive X-ray (EDX) analysis indicate the formation of a veneer of calcium phosphate for the most rapidly dissolving glass.
A traditional use for dissolved water glass is as a preservative for eggs.
Small quantities of dissolved water glass are used in the treatment of municipal water supplies as well as wastewater, where it adsorbs metallic ions and aids in the formation of loose agglomerations of particles called flocs, which filter the water of undesirable suspended materials.
Sodalite, a transient product of corundum dissolution, appeared above 600°C and eventually dissolved in glass.
It seems that anorthite phase was melted and dissolved in glass phase by increasing temperature from 1250 to 1340 °C.
Glass fiber dissolution was determined in AM and RNEC cultured for 3 weeks with fast dissolving glass fibers (GF-A) or slow dissolving ones (GF-B).
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