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汪建敏. 高浓度水煤浆反触变性的流变模式[J]. 力学学报, 1990, 22(5): 603-609. DOI: 10.6052/0459-1879-1990-5-1995-989
引用本文: 汪建敏. 高浓度水煤浆反触变性的流变模式[J]. 力学学报, 1990, 22(5): 603-609. DOI: 10.6052/0459-1879-1990-5-1995-989
ANTITHIXOTROPY OF HIGHLY CONCENTRATECD COAL-WATER SLURRLES[J]. Chinese Journal of Theoretical and Applied Mechanics, 1990, 22(5): 603-609. DOI: 10.6052/0459-1879-1990-5-1995-989
Citation: ANTITHIXOTROPY OF HIGHLY CONCENTRATECD COAL-WATER SLURRLES[J]. Chinese Journal of Theoretical and Applied Mechanics, 1990, 22(5): 603-609. DOI: 10.6052/0459-1879-1990-5-1995-989

高浓度水煤浆反触变性的流变模式

ANTITHIXOTROPY OF HIGHLY CONCENTRATECD COAL-WATER SLURRLES

  • 摘要: 本文根据速率型物料的假设和实验的等结构方法,确定了水煤浆反触变性的流变状态方程及速率方程。并对正、反触变性的特征进行了比较。

     

    Abstract: Coal-water slurries (CWS) a boiler fuels represent a new area of research in the coal utilization. They are concentrated suspensions. The knowledge of their rheological behaviour plays an important role in the preparation, storage, pumping and atomization. According to the assumption of a thixotropic fluid as a material of the rate type, and using the experimental method of the equivalent structure, the rheological equation of state and the rate equation of antithixotropic of CWS, are determined in this pap...

     

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