CIESC Journal

• 能源和环境工程 • 上一篇    下一篇

黄陵煤灰自身固硫的微观特性分析

程军;周俊虎;刘建忠;徐小琼;曹欣玉;岑可法   

  1. 浙江大学能源洁净利用与环境工程教育部重点实验室,浙江 杭州 310027;浙江省电力试验研究所,浙江 杭州 310014

  • 出版日期:2004-11-25 发布日期:2004-11-25

MICROSTRUCTURE OF SELF-DESULFURIZATION RESIDUE OF HUANGLING COAL ASH IN COMBUSTION

CHENG Jun;ZHOU Junhu;LIU Jianzhong;XU Xiaoqiong;CAO Xinyu;CEN Kefa   

  • Online:2004-11-25 Published:2004-11-25

摘要: 利用XRD、氮吸附仪和SEM分析了黄陵煤灰自身固硫渣样的微观结构.发现800℃下渣样中CaSO4和BaSO4含量达到8.5%、CaCO3和CaO含量达到4.9%,渣样表面由许多7.5~15μm的块状颗粒组成,其表面又含有一些0.7~1.5μm的纽扣状层片结构和孔隙.但1200℃下因热力分解和高温熔融,渣样中不再存在CaCO3、CaO、CaSO4或BaSO4晶相,渣样表面由少量30μm左右的大块颗粒组成,其表面又含有一些3~5μm的小块颗粒,带有明显烧结胀大和高温熔融的痕迹.1200℃下渣样的孔隙参数比800℃时急剧减少.

Abstract: The crystal phases, porosity and surface morphology of self-desulfurization residue of Huangling coal ash were studied by XRD, N2 absorption and SEM.It was found that the total content of sulfation product CaSO4 and BaSO4 was 8.5% in the self-desulfurization residue obtained at 800 ℃, while that of active CaCO3 and CaO was 4.9%.The residue surface was composed of many 7.5—15 μm particles that containd some 0.7—1.5 μm button-like particles and pores.However neither CaCO3,CaO,CaSO4 nor BaSO4 were found in the residue obtained at 1200℃,due to thermal decomposition and intense melting.The residue surface was composed of some 30μm particles that containd 3—5 μm nonporous particles with smooth surface.There was a distinct decrease in porosity parameters of the residue when the furnace temperature increased from 800 ℃ to 1200 ℃.