Migration and speciation transformation of K and Cl caused by interaction of KCl with organics during devolatilization of KCl-loaded model biomass compounds

Migration and speciation transformation of K and Cl caused by interaction of KCl with organics during devolatilization of KCl-loaded model biomass compounds
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负载 KCl 的模型生物质化合物脱挥发分过程中 KCl 与有机物相互作用引起的 K 和 Cl 的迁移和形态转化

DOI:
10.1016/j.fuel.2020.118205
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发表时间:
2020-10
期刊:
影响因子:
7.4
通讯作者:
Chuangzhi Wu
Chuangzhi Wu
中科院分区:
工程技术1区
文献类型:
--
作者:
Yanqin Huang;Huacai Liu;Hongyou Yuan;Xianchao Lv;Bin Xu;Weizhen Li;Jenjira Uttaruean;Xiuli Yin;Chuangzhi Wu

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为了更好地理解由KCl与有机物的相互作用引起的K和Cl的迁移,使用固定床装置在300-800 °C内热解负载KCl的模型化合物(纤维素、木聚糖、木质素和果胶)。采用连续化学形态分析结合ICP-OES和IC对煤焦中K和Cl的不同化学形态进行了定量分析。通过XPS和SEM-EDS进一步研究了Cl和K的形态和存在方式。4个样品中K和Cl的迁移存在较大差异,这种差异与有机官能团的类型密切相关。在低于500 °C的温度下,从四个样品中释放出低比例的K,而大量的水溶性K通过不同的离子交换反应机制转化为有机结合形式,从而促进Cl释放。木质素和果胶焦中有机钾含量分别为46.93-53.31%和32.47-41.75%,明显高于木聚糖和纤维素焦。同时,掺杂果胶中Cl的释放量(71.98-81.83%)依次为木质素(35.12-52.34%)、纤维素(18.56-35.68%)和木聚糖(10.67-18.65%)。释放出的部分Cl被活性炭吸附,形成有机氯,C-Cl生成量顺序为木质素>木聚糖>纤维素>果胶。随着热解的进行,纤维素表现出最高的钾释放由于有机钾的分解,而相当一部分具有较高的热稳定性的焦炭钾仍然保留在其他样品。提出了KCl与有机物反应导致K、Cl迁移的机理。
To better understand migration of K and Cl caused by interaction of KCl with organics, KCl-loaded model compounds (cellulose, xylan, lignin and pectin) were pyrolyzed within 300–800 °C using a fixed-bed apparatus. The amounts of different chemical occurrences of K and Cl in chars were quantitatively determined by sequential chemical fraction analysis combined with ICP-OES and IC. Morphologies and occurrence modes of Cl and K were further examined via XPS and SEM-EDS. Big differences in K and Cl migration were observed among four samples, and the distinction was closely related to types of organic functional groups. At temperature of below 500 °C, a low proportion of K was released from four samples, while amounts of water-soluble K was transformed into organically-bounded form via different ion-exchange reaction mechanisms, thereby promoting Cl release. About 46.93–53.31% and 32.47–41.75% of organic-K, presumably formed by reaction of KCl and methoxyls, were detected in lignin and pectin chars, apparently higher than that in xylan and cellulose chars. At the same time, amounts (71.98–81.83%) of Cl was released from doped pectin, followed sequentially by lignin (35.12–52.34%), cellulose (18.56–35.68%), and xylan (10.67–18.65%). Part of released Cl was recaptured by active carbon sites, thereby forming organochlorine, and C-Cl generation followed a sequence of lignin > xylan > cellulose > pectin. As pyrolysis proceeded, cellulose exhibited highest K release due to decomposition of organic-K, while a considerable of char-K with high thermal stability still retained in other samples. Mechanism on migration of K and Cl caused by reaction of KCl with organics was proposed.
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