Effect of feed melting, temperature history, and minor component addition on spinel crystallization in high-level waste glass

Spinet crystallization affects the anticipated cost and risk of high-level waste (HLW) vitrification. Spinet, (Fe, Ni) (Fe, Cr)(2)O-4, is the primary crystalline phase that precipitates from melts containing oxides of Fe, Ni, and Cr in sufficient concentrations. This study was undertaken to help des ign and verify mathematical models for a HLW glass melter in which spinet c rystals precipitate and partially settle. To study melting reactions, we us ed a simulated HLW feed, prepared with co-precipitated Fe, Ni, Cr, and Mn h ydroxides. Feed samples were heated up at a temperature-increase rate presu med to be close to that which the feed experiences in the HLW glass melter. The decomposition, melting, and dissolution of feed components (such as ni trates, carbonates, and quartz) and the formation of intermediate crystalli ne phases (spinet, sodalite, and Zr-containing minerals) were characterized using evolved gas analysis, vol-arne-expansion measurement, optical micros copy, scanning electron microscopy (SEM), thermogravimetric analysis (TGA), differential scanning calorimetry (DSC), and X-ray diffraction (XRD). Nitr ates and quartz, the major feed components, converted to a glass-forming me lt by 880 degreesC. A nearly chron-dum-free primary spinet formed in the ni trate melt starting from 520 degreesC and eventually dissolved in the boros ilicate melt by 1060 degreesC. Sodalite, a transient product of corundum di ssolution, appeared above 600 degreesC and eventually dissolved in glass. T o investigate the effects of temperature history and minor components (Ru, Ag, and Cu) on the dissolution and growth of spinet crystals, samples were heated up to temperatures below or above liquidus temperature (TL) and then subjected to different (constant or cyclic) temperature histories and anal yzed. The results show that the mass fraction of spinet as well as the comp osition and size of crystals depend on the chemical and physical makeup of the feed and the temperature history. Small crystals result from either pre venting the primary spinet from dissolving in the glass-forming melt or fro m the presence of nucleation agents, such as RuO2 (additions of 0.06 mass% Ag2O and 0.06 mass% CuO did not help nucleate spinet). Cyclic temperature h istories with the maximum temperature above TL and minimum temperature belo w TL kept spinet concentration far below the equilibrium concentration, esp ecially when a nucleation agent was absent. (C) 2001 Elsevier Science B.V. All rights reserved.