4.7 Article

Sub-particle scale study on the melting behavior of Zhundong coal ash based on the heterogeneous distribution of elements

期刊

COMBUSTION AND FLAME
卷 216, 期 -, 页码 223-231

出版社

ELSEVIER SCIENCE INC
DOI: 10.1016/j.combustflame.2020.03.006

关键词

Sub-particle scale; Zhundong coal; Element heterogeneous distribution; In-situ combustion; Residual ash particle; Melting behavior

资金

  1. National Key R&D Program of China [2018YFC0808500]
  2. Shanghai Engineering Research Center of Coal Gasification [18DZ2283900]
  3. China Postdoctoral Science Foundation [2018M632041]
  4. Fundamental Research Funds for the Central Universities [222201817004, 222201814052]

向作者/读者索取更多资源

The current research work focused on the effect of the heterogeneous distribution of elements on the ash melting behavior of Zhundong coal at the sub-particle scale by using a high temperature stage microscope (HTSM) and scanning electron microscope (SEM) equipped with energy dispersive spectrometry (EDS). Experimental results showed that both molten and unmolten areas existed in the residual ash sample after combustion below 1200 degrees C. Below this temperature, the partial ash melting behavior was significantly found during the ash melting process. Comparing the element composition of local molten and unmolten areas, Na, Si and Mg played predominant roles in the partial melting behavior. The enrichment of Na and Si promoted the formation of low temperature eutectic mixture and further molten areas, while the unmolten areas were rich in Mg. Combined with the micro-Raman analysis, minerals like spinel and forsterite that containing Mg were the main refractory components in the unmolten areas. Thermodynamic calculation results from FactSage software showed that the mass fraction of the liquid phase started to form rapidly at about 1100 degrees C in molten areas mainly with the fast melting of olivine and nepheline. However, the unmolten areas started to melt swiftly at about 1200 degrees C mainly with the fast melting of merwinite. Spinel was the main refractory component in both molten and unmolten areas. (C) 2020 The Combustion Institute. Published by Elsevier Inc. All rights reserved.

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