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FRACTURE TOUGHNESS OF SAMARIUM COBALT MAGNETS

机译:MAR钴磁铁的断裂韧性

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Samarium Cobalt (SmCo) magnets have been the magnet of choice for a variety of industries for many years due to their favorable magnetic properties. Their high coercivity, combined with a low temperature coefficient, make them the ideal permanent magnet for demanding high temperature applications. One of the biggest concerns with rare earth magnets is their brittleness. Samarium Cobalt magnets in particular are prone to fracturing during machining and assembly. In manufacturing, great care must be taken to avoid chipping or fracturing these magnets due to their brittle nature. There are two main grades of Samarium Cobalt magnets, 1:5 and 2:17. These ratios define the nominal ratio of rare earth to transition metal content. In this paper, an investigation is performed on the fracture toughness of permanent magnets based on the Samarium Cobalt 2:17 composition. Various techniques are used to characterize the microstructure of the material, and quantify the material properties. Optical microscopy is used to characterize the grain structure of the material and quantify the porosity of the material after sintering. By comparing the average grain size and fracture toughness of several samples, grain size was shown to not affect fracture toughness in standard material. Latent cracks in defective material showed no preference to follow grain boundaries, oxides inclusions or voids. River marks in fracture surfaces are seen through scanning electron microscopy, confirming the transgranular cracking pattern seen by Li et al This suggests that the toughness of the material is an inherent property of the main phase, not of grain boundaries or contaminants. Samarium Cobalt magnets exhibit both mechanical and magnetic anisotropy due to the alignment of their crystal structure in the manufacturing process. Using Palmqvist indentation crack techniques, the magnetic orientation of the grains was seen to greatly influence the direction of crack propagation from the tip of the indenter. Measurements of fracture toughness using this technique produce highly scattered data due to this anisotropic nature of the material. Specimens loaded with the indenter axis parallel to the direction of orientation show normal Palmqvist cracks, while specimens loaded perpendicular to the direction of magnetization exhibit crack propagation initiating from the faces of the indenter. To better quantify the material's brittleness, fracture testing is performed on specially prepared samples to obtain an absolute measure of fracture toughness (K1c). Results show that SmCo is measurably weaker than other magnetic materials such as neodymium iron boron magnets. Furthermore, neither relative concentration of Samarium nor source of raw material show notable effect on the fracture toughness of the material.
机译:mar钴(SmCo)磁体由于具有良好的磁性,多年来一直是各种行业的首选磁体。它们的高矫顽力加上较低的温度系数,使其成为苛刻高温应用的理想永磁体。稀土磁体的最大问题之一是其脆性。 machining钴磁铁特别容易在机加工和组装过程中破裂。在制造过程中,由于其易碎性,必须格外小心,以免使这些磁体碎裂或破裂。 mar钴磁铁有两个主要等级,即1:5和2:17。这些比率定义了稀土与过渡金属含量的标称比率。在本文中,对基于2:钴2:17成分的永磁体的断裂韧性进行了研究。使用各种技术来表征材料的微观结构,并量化材料的性能。光学显微镜用于表征材料的晶粒结构并量化烧结后材料的孔隙率。通过比较几个样品的平均晶粒尺寸和断裂韧性,表明晶粒尺寸不影响标准材料的断裂韧性。缺陷材料中的潜在裂纹显示不倾向于遵循晶界,氧化物夹杂物或空隙。通过扫描电子显微镜可以看到断裂表面的河痕,证实了Li等人所见的跨晶裂纹模式。这表明材料的韧性是主相的固有特性,而不是晶界或污染物的固有特性。 the钴磁体由于在制造过程中晶体结构的对准而表现出机械各向异性和磁各向异性。使用Palmqvist压痕裂纹技术,可以看到晶粒的磁取向极大地影响了从压头尖端传播裂纹的方向。由于这种材料的各向异性,使用这种技术测量断裂韧性会产生高度分散的数据。压头轴平行于取向方向加载的试样显示出正常的Palmqvist裂纹,而垂直于磁化方向加载的试样则显示出从压头表面开始的裂纹扩展。为了更好地量化材料的脆性,对专门准备的样品进行了断裂测试,以得到断裂韧性(K1c)的绝对量度。结果表明,SmCo比其他磁性材料(如钕铁硼磁体)弱得多。此外,relative的相对浓度或原料来源均未显示出对材料的断裂韧性的显着影响。

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