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Effect of Pressure on Graphite Morphology and Mechanical Properties of Squeeze Cast Hyper-Eutectic Grey Cast Iron

机译:压力对挤压超共晶灰铸铁石墨形态和力学性能的影响

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摘要

Squeeze casting is a process in which a high external pressure is applied and maintained on the molten metal during the whole solidification process resulting in the lower porosity, higher solidification rate and improved mechanical properties. In this research, the effects of applied pressure on the morphology of graphite flakes in a squeeze cast hyper-eutectic grey cast iron were investigated. The molten grey cast irons were solidified under atmospheric pressure as well as 25, 50 and 75 MPa externally applied pressures. The results indicated that the pressure increase during solidification decreased the amount of free graphite flakes, reduced the size of pro-eutectic Kish graphite flakes and increased the density of the castings. D-type graphite enclosing austenite dendrites, resembling that expected in hypo-eutectic grey cast iron, was observed near the surfaces of the castings solidified under externally applied pressures. Moreover, some compacted and spheroidal graphite particles were observed in the castings solidified under 50 and 75 MPa pressures. Furthermore, by increasing the squeeze casting pressure from atmospheric pressure to 75 MPa, the hardness, ultimate tensile strength and elongation increased by about 13, 68 and 128%, respectively. The results have been discussed in terms of increased cooling rate, expected change in the phase diagram of the alloy, different atomic structure of the interfaces of graphite and austenite as well as some proposed theories for formation of eutectic cells and spheroidal graphite.
机译:挤压铸造是一种在整个凝固过程中对熔融金属施加并保持较高外部压力的工艺,可降低孔隙率、提高凝固速度并改善机械性能。本文研究了压力对挤压铸造过共晶灰铸铁中石墨片形貌的影响。在大气压力以及25、50和75mpa外加压力下,熔融灰铸铁凝固。结果表明,凝固过程中压力的增加减少了自由石墨片的数量,减小了先共晶Kish石墨片的尺寸,增加了铸件的密度。在外部施加压力下凝固的铸件表面附近,观察到包围奥氏体枝晶的D型石墨,类似于亚共晶灰铸铁中的预期。此外,在50和75mpa压力下凝固的铸件中观察到一些致密和球状石墨颗粒。此外,通过将挤压铸造压力从大气压增加到75mpa,硬度、极限拉伸强度和延伸率分别提高了约13%、68%和128%。从冷却速度的增加、合金相图的预期变化、石墨和奥氏体界面的不同原子结构以及形成共晶胞和球状石墨的一些理论方面对结果进行了讨论。

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