张燕, 乐恺, 张欣茹, 毛炜, 王广, 张礼, 张欣欣. 煤气化RSC中灰渣沉积层结构、组成及传热分析[J]. 煤炭学报, 2021, 46(12): 4045-4053.
引用本文: 张燕, 乐恺, 张欣茹, 毛炜, 王广, 张礼, 张欣欣. 煤气化RSC中灰渣沉积层结构、组成及传热分析[J]. 煤炭学报, 2021, 46(12): 4045-4053.
ZHANG Yan, YUE Kai, ZHANG Xinru, MAO Wei, WANG Guang, ZHANG Li, ZHANG Xinxin. Deposit layer of the radiation syngas cooler in coal gasification process:Structure,composition,and heat transfer characteristics[J]. Journal of China Coal Society, 2021, 46(12): 4045-4053.
Citation: ZHANG Yan, YUE Kai, ZHANG Xinru, MAO Wei, WANG Guang, ZHANG Li, ZHANG Xinxin. Deposit layer of the radiation syngas cooler in coal gasification process:Structure,composition,and heat transfer characteristics[J]. Journal of China Coal Society, 2021, 46(12): 4045-4053.

煤气化RSC中灰渣沉积层结构、组成及传热分析

Deposit layer of the radiation syngas cooler in coal gasification process:Structure,composition,and heat transfer characteristics

  • 摘要: 随着热量回收技术在现代煤气化领域的应用,辐射式合成气冷却器(RSC)换热表面的灰渣沉积问题已成为该技术发展的瓶颈。以RSC底部换热面灰渣沉积层为研究对象,通过表征沉积层的形貌、结构及成分,探析灰渣沉积机制及其对水冷壁传热的影响规律。沉积层沿径向方向,分为3个主层:内层是由微米级颗粒构成的薄层;中层为烧结层,整体呈多孔状,微观呈连续块状;内层与中层之间由块状含铁大颗粒连接,连接强度低、易脱落;外层为熔融层,呈致密块状;各主层又分为形貌特点不同的2个子层。各元素含量在沉积层中的分布规律不同:Fe元素呈内高外低的分布特点;S元素从内2层开始大幅降低,与铁的硫化物在还原性气氛下分解有关;Na,K元素在内层富集,中层降低,外层再次增加。外层存在NaCl,KCl晶体颗粒,推测其沉积位置的温度高于其熔点温度、低于其冷凝温度。构建了沉积状态与传热特性关联的计算模型,计算结果表明,内层形成时热流密度下降25%,3层沉积均形成时热流密度下降40%,内层形成时主要热阻是表面辐射换热热阻。研究表明,RSC灰渣沉积防治策略应以抑制内层的形成与增长为主,阻止或延缓中外层的生成;中外层已形成时,可通过诱发层间剪切运动,促使沉积层从连接薄弱处断裂、脱落。

     

    Abstract: In recent years, heat recovery technology has been applied in the field of modern coal gasification. Ash deposition on the radiant syngas cooler’s (RSC) heat exchange surface has become the bottleneck problem. Herein, this work aims to understand the deposit layer on the heat exchange surface at the RSC’s bottom. By characterizing the morphology, structure, and composition of the deposit layer, the ash deposition mechanism and its influence on the heat transfer process has been analyzed. The results reveal that the deposit layer can be divided into three main layers along the radial direction. The inner layer is a thin layer mainly composed of micro-particles. The middle layer is the sintered layer, being porous on the whole and dense at the micro-level. The large massive Fe-rich particles are supposed to be the connection points between the inner and middle layers. The outer layer is a molten layer with significantly fewer holes and dense lumps. According to the morphological characteristics, each main layer can be divided into two sub-layers. The content of Fe is higher on the inner side than on the outer side. The S content at the interface between the first inner layer and the second inner layer suddenly drops, which is related to the decomposition of iron sulfide. The contents of Na and K are enriched in the inner layer, decreased in the middle layer, and increased again in the outer layer. The NaCl and KCl crystal particles appear in the outer layer, so it is speculated that the temperature of the deposition location is higher than the melting temperature and lower than the condensation temperature of the alkali chlorides. Based on the deposit layer’s morphology and composition, the surface temperatures of three deposition states are estimated, and the heat transfer flux is calculated. The results show that the heat flux decreases by 25% when the inner layer is formed, and 40% when the three layers are all formed. The inner layer has the greatest thermal barrier effect, mainly related to its low radiation characteristics. This study indicates that the prevention of inner layer formation has important implications for developing efficient technology to control the RSC ash deposition. If the middle and the outer layers have already formed, the interlayer shear movement could cause the sedimentary layer to fracture and fall off from the weak point of connection.

     

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