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Influence of Melt Carbon and Sulfur on the Wetting of Solid Graphite by Fe-C-S Melts

机译:熔融碳和硫对Fe-C-S熔体润湿固体石墨的影响

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摘要

The interfacial phenomena between carbonaceousmaterials such as graphite, coke ,and char and Fe一C一S meltsare important due to the extensive use of these materials in ironprocessing furnaces. However, the understanding of theinterfacial phenomena between these kinds of carbomaceorsmaterials and molten iron alloys is far from complete. In thisstudy ,graphite was selected as the solid carbonaceous materialbecause its atomic structure has been well established. Thesesslie drop method was adopted in this investigation to measurethe contact angle between solid graphite and molten iron and tostudy the interfacial phenomena. The influence of carbon andsulfur content in Fe一C一S melts on the wettability of solidgraphite has been investigated at 1600℃.The melt carboncontent was in the range of 0.13 to 2.24 wt pct, andthe melt sulfur content was in the range of 0.05 to 0.37wt pct .X-ray energy-dispersive spectrometer(EDS)analysis was conducted on an HITACHIS-4500scanning electron microscope to detect compositiondistribution at the interfacial region. It was foundthat contact of solid graphite with Fe一C一S melts willresult in a nonequilibrium reactive wetting. It involved xarbontransfer from the solid to the liquid and iron transfer from theliquid to the solid. The Fe一C一S melts exhibited relativelypoor wetting when the reactions were absent. The mass transferbetween solid graphite and Fe一C一S melts was observed tostrongly enhance the wetting phenomena. It is proposed that thedecrease of system free energy corresponding to the masstransfer reactions strongly influences the formation of theinterface region and results in the progressive spreading of thewetting line. The composition and thickness of the graphite/ironinterfacial layer was dependent on the intensity of mass transferacross the interface. The resulting change in the interfacialenergyγls is a strong function of mass transfer, and it varies inaccordance with time of contact. The influence of carboncontent on the wetting phenomena could only be seen at in theinitial stages, whereas the influence of sulfur on the wettabilitywas found when the system approached equilibrium.Therefore ,the interfacial tension in its equilibrium condition atthe graphite/ Fe一C一S melt interface was determined only bythe extent of sulfur adsorption at this interface.
机译:碳质材料(例如石墨,焦炭,焦炭和Fe一C一S熔体)之间的界面现象很重要,因为这些材料在炼铁炉中得到了广泛使用。然而,对这类卡波马斯材料与铁水合金之间的界面现象的理解还远远不够。本研究选择石墨作为固体含碳材料,因为它的原子结构已经很好地建立了。本研究采用滴滴法测量了固体石墨与铁水的接触角,研究了界面现象。研究了在1600℃下Fe一C一S熔体中碳和硫含量对固态石墨润湿性的影响。熔体中碳含量在0.13至2.24 wt%范围内,熔体硫含量在0.05至5%之间。在HITACHIS-4500扫描电子显微镜上进行0.37wt%的X射线能量色散谱仪(EDS)分析,以检测界面区域的成分分布。发现固态石墨与Fe一C一S熔体的接触将导致非平衡反应性润湿。它涉及从固体到液体的碳氢键转移和从液体到固体的铁转移。当不存在反应时,Fe一C一S熔体的润湿性相对较差。观察到固体石墨与Fe一C一S熔体之间的传质可显着增强润湿现象。提出与传质反应相对应的体系自由能的减少强烈影响界面区域的形成,并导致润湿线的逐渐扩散。石墨/铁界面层的组成和厚度取决于穿过界面的传质强度。界面能的变化是传质的重要函数,并且它随着接触时间的变化而变化。碳含量对润湿现象的影响只有在初始阶段才能看到,而当体系达到平衡时才发现硫对润湿性的影响。因此,石墨/ Fe一C一S熔体在平衡状态下的界面张力界面仅由该界面上硫的吸附程度决定。

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