Atomic and nano scale chemical and structural changes in quenched and tempered 4340 steel

被引:114
|
作者
Clarke, A. J. [1 ]
Miller, M. K. [2 ]
Field, R. D. [1 ,3 ]
Coughlin, D. R. [1 ]
Gibbs, P. J. [1 ]
Clarke, K. D. [1 ]
Alexander, D. J. [1 ]
Powers, K. A. [2 ]
Papin, P. A. [1 ]
Krauss, G. [3 ]
机构
[1] Los Alamos Natl Lab, Div Mat Sci & Technol, Los Alamos, NM 87545 USA
[2] Oak Ridge Natl Lab, Ctr Nanophase Mat Sci, Oak Ridge, TN 37831 USA
[3] Colorado Sch Mines, Golden, CO 80401 USA
关键词
Steel; Tempering; Martensite; Atom probe tomography (APT); Transmission electron microscopy (TEM); NI-C MARTENSITES; PROBE TOMOGRAPHY; CARBON-STEEL; MECHANICAL-PROPERTIES; ELECTRON-MICROSCOPY; RETAINED AUSTENITE; ALLOY-STEEL; TEMPERATURE; CARBIDE; IRON;
D O I
10.1016/j.actamat.2014.05.032
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Atom probe tomography and transmission electron microscopy (TEM) have been used to determine the location and distribution of carbon and alloying elements associated with the complex structural changes that occur at the atomic and nanoscale in 4340 steel after quenching to martensite and tempering at 325, 450 or 575 degrees C. Tempering at 325 degrees C resulted in carbide formation without partitioning of chromium, manganese, molybdenum, aluminum, nickel or phosphorus, but with early-stage silicon rejection from the carbide. TEM verified the presence of cementite and the Bagaryatsky orientation relationship with the tempered martensite matrix and detected complex precipitate structures. Tempering at 450 or 575 degrees C developed concentrations of all alloying elements at ferrite-cementite interfaces: chromium, manganese and molybdenum partitioned into the cementite, and silicon, aluminum, nickel and phosphorus were clearly rejected from the cementite. These results provide direct evidence for staged cementite growth, where early-stage growth likely occurs under paraequilibrium conditions, followed by initial silicon redistribution and subsequent alloying element redistribution during late-stage growth. Tempering at 575 degrees C induced spheroidization of the cementite, loss of the Bagaryatsky orientation relationship, and phosphorus concentrations at Cottrell atmospheres within the cementite and at ferrite-cementite interfaces, correlating with early observations of the retardation of spheroidization by phosphorus. (C) 2014 Acta Materialia Inc. Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码:17 / 27
页数:11
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