2012
DOI: 10.1016/j.jnoncrysol.2012.02.014
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Dissolution rate and mechanism of solid MgO particles in synthetic ladle slags

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Cited by 23 publications
(8 citation statements)
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“…Binary and ternary phases, such as C 3 S and merwinite (C 3 MS 2 ), were identified between zones I and II, which suggested the presence of 'inner slag', as has been reported by Wang et al 38 The ion Si 4+ was also generated by the dissolution of magnesia particles; binary (C 2 S and C 3 S) and ternary (C 2 AS) phases containing this component were therefore detected in zone III.…”
Section: Corrosion Testsupporting
confidence: 70%
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“…Binary and ternary phases, such as C 3 S and merwinite (C 3 MS 2 ), were identified between zones I and II, which suggested the presence of 'inner slag', as has been reported by Wang et al 38 The ion Si 4+ was also generated by the dissolution of magnesia particles; binary (C 2 S and C 3 S) and ternary (C 2 AS) phases containing this component were therefore detected in zone III.…”
Section: Corrosion Testsupporting
confidence: 70%
“…Finally, the region III was defined, where phases formed with the ions incorporated into the melt by the complete dissolution of the outer layers of the particle, mainly Mg +2 , and Ca +2 and Si +4 in lower proportions, were identified. The aspect of the spinel detected in this last region suggested that it was formed by precipitation from the liquid, 38 which was saturated in MgO, contrary to that of zone II.…”
Section: Corrosion Testmentioning
confidence: 81%
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“…During the dissolution process, a mass change in a shrinking/dissolving particle was equal to the mass flux across the boundary layer, which is as follows4πρnormalPR2dRdt=4πR2kΔCPe=2RUD;Re=2RρnormalsUμwhere ρ P and ρ s are the densities of the dissolving particle and slag, respectively; U is the fluid flow speed around particle, μ is the viscosity of the liquid slag; and the mass transfer coefficient k is approximately equal to D / R when the Peclet number Pe < 10 and the Reynolds number Re << 1 . The dissolution was expressed in the following equation describing the classical shrinking‐core model as limited by mass transfer through the boundary layertτ=1(RR0)2;τ=ρnormalPR022DnormalsΔC…”
Section: Resultsmentioning
confidence: 99%
“…[1][2][3][4][5][6] The dissolution rate of MgO refractory into oxide slags strongly depends on the slag composition and temperature. 7) Both dissolution and penetration are considerably affected by wettability. [8][9][10][11] Wettability, also called dynamic wetting, is divided into two categories: non-reactive wetting and reactive wetting.…”
Section: Introductionmentioning
confidence: 99%