高挥发分煤煤焦燃烧过程中矿物与煤焦的相互作用

Melissa M. Lunden , Nancy Y.C. Yang , Thomas J. Headley , Christopher R. Shaddix
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引用次数: 24

摘要

我们报道了最近关于无机矿物质在碳燃尽过程中对焦炭结构演变的作用的研究。在一个精心控制的层流火焰支持的夹带流反应器中收集的焦炭样品已经使用许多显微镜工具进行了表征。对在各种燃烧条件下产生的煤焦的无机结构的观察与煤焦颗粒群的原位粒度高温计测量相结合,目的是确定矿物相互作用的机制及其对煤粉-煤焦燃烧过程中碳燃尽动力学的影响。在煤焦上没有发现宏观灰膜的证据,该灰膜被假设为延缓煤焦氧化动力学。然而,高分辨率电子显微镜显示,碳质基质内的固溶体中有数量惊人的无机矿物。有机和无机成分的这种紧密混合可以通过阻断氧气进入活性碳位点和影响燃烧过程中形成的微观碳结构来影响反应性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mineral-char interactions during char combustion of a high-volatile coal

We report on recent investigations of the role of inorganic mineral matter on the evolution of char structure during carbon burnout. Char samples collected in a carefully controlled, laminar flame-supported entrained flow reactor have been characterized using a number of microscopy tools. Observations of the inorganic structure of chars produced at a variety of combustion conditions are coupled with in situ particlesizing pyrometry measurements of the char particle population with an eye toward identifying the mechanism of mineral interaction and its effects on carbon burnout kinetics during pulverized coal char combustion. No evidence of a macroscopic ash film which has been hypothesized to retard char oxidation kinetics, was found on the chars. High-resolution electron microscopy, however, shows a surprising amount of inorganic mineral in solid solution within the carbonaceous matrix. This intimate mixing of organic and inorganic constituents may affect reactivity by both blocking oxygen access to active carbon sites and influencing the microscopic carbon structure that evolves during combustion.

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