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440 t/h燃煤锅炉低氮燃烧模式下水冷壁高温腐蚀分析
引用本文:王毅斌,张思聪,谭厚章,林国辉,王萌,卢旭超,杨浩.440 t/h燃煤锅炉低氮燃烧模式下水冷壁高温腐蚀分析[J].中国电力,2021,54(8):118-127.
作者姓名:王毅斌  张思聪  谭厚章  林国辉  王萌  卢旭超  杨浩
作者单位:1. 西安交通大学 热流科学与工程教育部重点实验室,陕西 西安 710049;2. 浙江巨化热电有限公司,浙江 衢州 324004;3. 西安格瑞电力科技有限公司,陕西 西安 710049
基金项目:国家自然科学基金资助项目(51876162, 51906198)
摘    要:分别采用X射线荧光光谱、X射线衍射光谱、电镜扫描和能谱分析等方法,对某440 t/h燃煤锅炉下层燃烧器附近水冷壁区域收集的腐蚀层进行详细表征,分析并讨论腐蚀产物的形成和痕量元素富集特点。结果表明:腐蚀内层主要含有FeS2、Fe2O3、PbS和ZnS,但Pb比Zn富集程度高;腐蚀外层以ZnS、PbS、GaS、Fe1-xS和Zn1.0Al1.04S2.13为主,还含有少量Ga、Se、Bi等元素,但Zn与Ga元素富集程度显著高于内层;腐蚀层中Pb、Zn、Ga、Se、Ge、As、Bi、Th、Sn、Sb等元素主要通过气化-冷凝和黏附的未燃尽碳颗粒释放析出的方式到达管壁,部分元素仍存在二次气化现象并扩散至腐蚀层深处,以进一步增大腐蚀裂纹尺度。基体铁的氧化和硫化反应同时发生并相互竞争,靠近基体侧腐蚀层先发生裂缝后逐渐开始破碎。黄铁矿向外转移中会释放气态硫并生成多种晶型的磁黄铁矿,这说明气态硫在腐蚀过程中扮演重要作用。此外,沉积层中微细颗粒和气态痕量元素可能会向基体侧移动与扩散渗透,增加腐蚀内部应力进而加剧腐蚀。

关 键 词:低氮燃烧  硫化氢  高温腐蚀  硫化锌  硫化铅  痕量元素  
收稿时间:2020-04-25
修稿时间:2020-10-20

Analysis on High Temperature Corrosion of Water-Wall in a 440 t/h Boiler Under Low-NOx Combustion Mode
WANG Yibin,ZHANG Sicong,TAN Houzhang,LIN Guohui,WANG Meng,LU Xuchao,YANG Hao.Analysis on High Temperature Corrosion of Water-Wall in a 440 t/h Boiler Under Low-NOx Combustion Mode[J].Electric Power,2021,54(8):118-127.
Authors:WANG Yibin  ZHANG Sicong  TAN Houzhang  LIN Guohui  WANG Meng  LU Xuchao  YANG Hao
Affiliation:1. MOE Key Laboratory of Thermal Flow Science and Engineering, Xi'an Jiaotong University, Xi'an 710049, China;2. Zhejiang Juhua Cogeneration Co., Ltd., Quzhou 324004, China;3. Xi'an GeRui Power Science and Technology Co., Ltd., Xi'an 710049, China
Abstract:The corrosive products that were collected from water-wall tubes close to burners at the lowest layer in a 440 t/h coal-fired furnace, were characterized by various technology methods including X-Ray Fluorescence spectrum (XRF), X-Ray power Diffraction (XRD), Scanning Electron Microscope and Energy Dispersive System (SEM-EDS), for the analysis and discussion of the formation of corrosive products and enrichments of trace elements. The results showed that inner corroded layer was mainly composed of FeS2, Fe2O3, PbS and ZnS, with higher enrichment of Pb element than Zn. While in the outer corroded layer, ZnS, PbS, GaS, Fe1-xS and Zn1.0Al1.04S2.13 were the major compositions of the mineral phases with minor elements of Ga, Se and Bi, but more significant enrichment of Zn and Ga elements were observed than that in the inner corroded layer. Trace elements including Pb, Zn, Ga, Se, Ge, As, Bi, Th, Sn, Sb were enriched both in inner and outer corroded layer. They were formed mainly via the vaporization-condensation of gaseous species from coal combustion and the release from the unburned carbon particle that adhered to water-wall tube surfaces. Moreover, some of condensed trace elements may re-vaporize and then diffuse into deeper corrosion layer, which would further cause the growth of the crack opening size in corrosion. During the corrosive process, the oxidation and sulfidation reactions of iron matrix occurred simultaneously and competed with each other. The cracks were first formulated at the corroded layer adjacent to iron matrix and then as the cracks developed, it started to break into small patches. Various kinds of pyrrhotite with different crystal sizes would be generated and some gaseous sulfur would be released as the pyrite migrated toward the outer layer, which suggests that gaseous sulfur may play an important role in corrosive process. Additionally, the migration and diffusion of fine particles and gaseous trace elements into iron matrix side may further accelerate the rate of internal stress cracking, to promote the diffusion of corrosive gases and aggravate the corrosion.
Keywords:low-NOx combustion  hydrogen sulfide  high-temperature corrosion  zinc sulfide  lead sulfide  trace elements  
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