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CARBON ORDERING IN Fe-1.83C MARTENSITE Ⅰ. Crystal Structure of a Conventional Ordered Phase |
REN Xiaobing; WANG Xiaotian (Xi'an Jiaotong University); SHIMIZU Ken'ichi (Kanazawa institute of Technology; Japan); TADAKI Tsugio (Osaka University;Japan)(Manuscript received 27 October; 1993; in revised form 4 January; 1994) |
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Cite this article:
REN Xiaobing; WANG Xiaotian (Xi'an Jiaotong University); SHIMIZU Ken'ichi (Kanazawa institute of Technology; Japan); TADAKI Tsugio (Osaka University;Japan)(Manuscript received 27 October; 1993; in revised form 4 January; 1994). CARBON ORDERING IN Fe-1.83C MARTENSITE Ⅰ. Crystal Structure of a Conventional Ordered Phase. Acta Metall Sin, 1994, 30(7): 296-301.
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Abstract Electron diffraction technique is applied to determine the crystal structure of a conventional ordered phase found in an aged high carbon(1.83%) martensite. Experimental data of good quality are obtained to ensure the reliability of the structure determination. The ordered phase is found to be an off-stoichiometric compound isomorphic with γ'-Fe_4N, it is thus called γ'-Fe_xC (I)(x= 4-11). Its cell dimension is (a_M and c_M are the length of a and c axis of martensite unit cell, respectively). The ordered phase is coherent with martensite, their orientation relationship is (001)Ⅰ∥(001)M,[100]Ⅰ∥[110]M. Diffraction patterns calculated based on γ'-Fe_xC (I) are in agreement with experimental observations.Correspondent: REN Hiaobing, Presently with Department of physics, Nanjing University, Nanjing 210008
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Received: 18 July 1994
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