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    煤直接液化加氢反应器内固体沉积物性质及形成机理研究

    Study on properties and sedimentation mechanism of solid deposits

    • 摘要: 针对神华煤直接液化工艺中固体沉积问题,开展了煤直接液化加氢反应器内沉积物性质及形成机理研究。结果表明:神华煤直接液化一代和二代技术沉积物的体积平均粒径分别为913μm和581μm,均远大于原煤,这说明一代和二代技术加氢反应器内均发生了明显的矿物质生长聚并过程。两种沉积物均以无机质为主,灰含量分别为91.34%和83.19%,而碳含量则分别为6.98%和11.61%。两种沉积物中晶相物质主要是催化剂Fe1-xS、方解石CaCO3以及少量石英SiO2。与负载催化剂的原煤相比,两种沉积物中Fe元素均出现明显富集,而Ca、Si和Na元素则有所稀释。神华煤直接液化一代及二代技术固体沉积物形成机理相仿,沉积物主要成分为Fe1-xS和CaCO3,次要成分为NaCl、SiO2以及含Mg、Al或K等元素的煤中伴生矿物和有机质,沉积物多以径向元素组成分布相对均匀的颗粒、核-壳结构甚至径向元素组成呈三层分布的形态存在。

       

      Abstract: Aiming at the problem of solid deposition in Shenhua direct coal liquefaction process, a study on the properties of deposits in hydrogenation reactors was carried out, and the formation mechanism of the deposits was inferred. The results show that the volume-average particle sizes of deposits from both the first-generation and second-generation technologies of Shenhua direct coal liquefaction are 913μm? and ?581μm? respectively, both of which are larger than that of raw coal, which indicates that obvious growth and agglomeration processes have occurred for the deposits in the hydrogenation reactors. Both types of deposits are dominated by inorganic matter, with ash contents of 91.34% and 83.19% respectively, while the carbon contents are 6.98% and 11.61% respectively. The crystalline phases in the two deposits are mainly the catalyst Fe1-xS, calcite CaCO?, and a small amount of quartz SiO?. Compared with raw coal loaded with catalyst, the Fe element in both deposits shows obvious enrichment, while the elements of Ca, Si and Na are diluted to some extent, especially Ca and Si. The formation mechanisms of solid deposits from the first-generation and second-generation technologies of Shenhua direct coal liquefaction are similar. The main components of the deposits are Fe1-xS and CaCO?, while the secondary components include NaCl, SiO?, as well as associated minerals in coal containing elements such as Mg, Al or K, and organic matter. The deposits mostly exist in forms of particles with relatively uniform radial elemental composition distribution, core-shell structure, or even three-layer radial elemental composition distribution.

       

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