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Rheological properties of high-temperature melts of coal ashes and other silicates
This paper reviews the 20th century advances within the field of the measurement and the prediction of the rheological properties of high-temperature (T>1000 K) silicate melts at atmospheric pressure with a focus on coal ashes and other melts of compositions relevant to coal ashes. Theoretical co...
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Published in: | Progress in energy and combustion science 2001-03, Vol.27 (3), p.237-429 |
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Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | This paper reviews the 20th century advances within the field of the measurement and the prediction of the rheological properties of high-temperature
(T>1000
K)
silicate melts at atmospheric pressure with a focus on coal ashes and other melts of compositions relevant to coal ashes.
Theoretical considerations are represented firstly by a synopsis of definitions and flow-regimes and secondly by an outline of the ruling network theory and the notations used therein. The influence of different cations on viscosity is discussed thoroughly.
Experimental points include a listing of the most common apparatus for viscosity measurements on high-temperature liquids and a summary of existing experimental data. Viscosity vs temperature is reported in tables as well as graphically for melts composed of major amounts of one or more of the species: SiO
2, Al
2O
3, FeO
x
, CaO, MgO, Na
2O, K
2O, Li
2O, MnO, TiO
2, B
2O
3. For each experimental source, relevant information is listed (apparatus, sensor material, atmosphere).
With a basis in both theory and experimental data, general equations for liquids, are presented, relating viscosity to temperature and/or concentration of dispersed solids, as are more specific mathematical models, relating the viscosity of silica melts and glasses to temperature and composition. |
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ISSN: | 0360-1285 1873-216X |
DOI: | 10.1016/S0360-1285(00)00023-X |