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Investigation of the intermediate layers formed by austenitic nitrocarburizing

机译:奥氏体氮碳共渗形成的中间层的研究

摘要

By nitriding the Fe-N system above the eutectoid temperature (592°C), an intermediate layer called (nitro)austenite is formed under the compound layer that can transform into braunite during low-rate cooling at eutectoid temperature. The two-phase complement of structure forming such a way - namely the braunite - is an eutectoid consisting of body-centred cubic α-iron and Fe4N iron-nitride compound (α + γ´). This poorly investigated texture and its formation was investigated. During our experiments, 100Cr6 and C105U steels were nitrocarburised above the eutectoid temperature (592°C). The conditions and properties of the formation of the developed intermediate layers, the microstructure and the distribution of the nitrogen and carbon in the specimens were investigated by using light optical microscopy (LOM), microhardness measurements, X-ray diffraction (XRD) method, scanning (SEM) and transmission (TEM) electronmicroscopy and glow discharge optical emission spectrometry (GD-OES).
机译:通过在共析温度(592°C)之上氮化Fe-N系统,在化合物层下形成了一个称为(硝基)奥氏体的中间层,该中间层在共析温度下低速冷却时可转变成褐铁矿。形成这种方式的结构的两相互补物,即褐铁矿,是一种共析物,由体心立方α-铁和Fe4N氮化铁化合物(α+ γ´)组成。研究不充分的质地及其形成过程。在我们的实验中,100Cr6和C105U钢在共析温度(592°C)以上进行了氮碳共渗。利用光学显微镜(LOM),显微硬度测量,X射线衍射(XRD)法,扫描法研究了形成的中间层的形成条件和性质,试样中氮和碳的微观结构和分布。 (SEM)和透射(TEM)电镜和辉光放电光发射光谱(GD-OES)。

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