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Texturing of Magnetite Forming During Long-Term Operation of a Pipeline of 10CrMo9-10 Steel

机译:10CrMo9-10钢管道长期运行期间磁铁矿形成的组织

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The paper presents results of X-ray measurements of the texture of a magnetite (Fe_3O_4) layer formed on 10CrMo9-10 steel during 100,000 hours operation at the temperature of 575°C (in a flowing medium environment). The formed oxide layer was ~140μm thick. Measurements of texturing were performed on the oxide surface and also at the depth of ~50μm from the surface (1st polishing) and ~100μm (2nd polishing). X-ray studies were carried out using the radiation of a cobalt anode tube, λ_(Co)=0.17902nm, for (311) and (400) Fe_3O_4 reflections, using a radiation beam collimated to Φ=2mm. The study was aimed at determination of correlation between the texturing and the structure on the magnetite layer cross-section. A clear texturing of {111}<112> and {111}<110> type for the magnetite in the initial state and after the second polishing was found. Instead, after the first polishing there was a substantial texturing of {034}<100> and {015}<051> type. A different nature of the texture may result from a diversified morphology of magnetite at various depths (caused inter alia by a differentiated temperature on the tube wall cross-section during the material operation), which is related among other things to the crystallites size. The magnetite structure and texture changes can affect the magnetite porosity and cleavage.
机译:本文介绍了在575°C(在流动介质环境中)运行10万小时的过程中,在10CrMo9-10钢上形成的磁铁矿(Fe_3O_4)层的织构的X射线测量结果。所形成的氧化物层为〜140μm厚。在氧化物表面以及距表面约50μm的深度(第一次抛光)和约100μm的深度(第二次抛光)进行纹理化测量。 X射线研究是使用钴阳极管的辐射λ_(Co)= 0.17902nm,针对(311)和(400)Fe_3O_4反射,使用准直为Φ= 2mm的辐射束进行的。该研究旨在确定纹理与磁铁矿层横截面上的结构之间的相关性。对于初始状态和第二次抛光之后的磁铁矿,发现了{111} <112>和{111} <110>型的清晰纹理。取而代之的是,在第一次抛光之后,出现了{034} <100>和{015} <051>类型的大量纹理。质地的不同性质可能是由于在不同深度(尤其是由于在材料操作过程中管壁横截面的不同温度所致)的磁铁矿的形态不同所致,这尤其与微晶的尺寸有关。磁铁矿的结构和质地变化会影响磁铁矿的孔隙率和解理作用。

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