中碳合金鋼高溫相變的晶體學(xué)分析
[Abstract]:In this paper, the crystallographic characteristics of 50Si2Mn3 steel during high temperature isothermal transformation and the mechanism of magnetic induction of diffusion-type transformation under the action of different magnetic fields are studied.The crystal orientation characteristics of medium carbon silicon manganese cast steel under different magnetic fields are analyzed from the viewpoints of nucleation, growth and crystallography. For the starting point of magnetic induced pearlite (MIP) phase transition and the highest temperature at which pearlite can be induced, the relationship between the starting point of phase transition and magnetic field intensity, phase transition temperature and phase transition time is established. At the beginning of transformation, the pearlite ferrite phase (PF), one of the constituent phases, grows mainly along the direction of 110 / / ND, the proportion of 111 / / ND and 100 / / / ND is relatively low, showing a certain preferred nucleation and growth; with the increase of the amount of transformation, PF maintains its preferred crystal growth at the beginning of nucleation, and the crystallographic degree of the new phase is subjected to the interface energy. Besides the influence of volume free energy and magnetic free energy, the spatial orientation tends to be multi-directional due to the gradually accumulated elastic strain energy in the parent phase. The preferential growth trend of MIP formed in the middle and late stages is weakened, and the relative proportion of MIP with other orientations is also reduced, thus losing the preference of 110//ND. The magnetic treatment time of the samples was prolonged and the samples were characterized by non-microtexture. The research focus of higher magnetic field was to investigate whether the ferromagnetic PF could show the preferred magnetization direction of BCC Fe 001 or continue the growth rule of 12T. The field strength of 20T was the comprehensive sample size, the size of the furnace, and the magnet had the same magnetism. The crystal orientation of MIP under the magnetic field of 19.8 T.19.8 T shows that there are crystal orientation changes closely related to the isothermal temperature and magnetic time during the formation of MIP. At a relatively low isothermal temperature (983 K), a specific orientation (100) of MIP crystals tends to increase with the extension of the magnetization time in the range of transformation, while at a relatively high isothermal temperature (995 K), the fraction of 100 orientations decreases with the extension of the magnetization time. Therefore, the preferred orientation 100 of MIP is related to the growth rate of PF, and is mainly stronger in the early stage of MIP formation. When the MIP reaches a certain amount of transformation, other crystal orientations (such as 110) turn to show growth advantage, even in the direction of difficult magnetization, the growth rate of MIP also appears. The starting point of phase transition (producing 1% MIP) and the highest temperature of induced pearlite structure (in the range of isothermal time, which means that no pearlite structure can be observed above this temperature) are studied according to the transformation amount of MIP under different magnetic treatment conditions. The starting point of phase transition and the magnetic field intensity-phase transition temperature are established. The results show that the effect of magnetic field on the maximum temperature of pearlite transformation is not linear. In addition, the results of MIP incremental change and electron backscatter diffraction (EBSD) orientation analysis show that magnetic field promotes the nucleation and growth of easily magnetized 100-direction grains at the initial stage of pearlite transformation, and cementite exists. In the latter stage, the increase of pearlite transformation is mainly due to the growth of the primary pearlite rather than the increase of nucleation.
【學(xué)位授予單位】:昆明理工大學(xué)
【學(xué)位級(jí)別】:碩士
【學(xué)位授予年份】:2015
【分類號(hào)】:TG142.1
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