The effect of cooling rate on the microstructures formed during solidification of ferritic steel

Citation
Nh. Pryds et X. Huang, The effect of cooling rate on the microstructures formed during solidification of ferritic steel, MET MAT T A, 31(12), 2000, pp. 3155-3166
Citations number
29
Categorie Soggetti
Apllied Physucs/Condensed Matter/Materiales Science",Metallurgy
Journal title
METALLURGICAL AND MATERIALS TRANSACTIONS A-PHYSICAL METALLURGY AND MATERIALS SCIENCE
ISSN journal
10735623 → ACNP
Volume
31
Issue
12
Year of publication
2000
Pages
3155 - 3166
Database
ISI
SICI code
1073-5623(200012)31:12<3155:TEOCRO>2.0.ZU;2-Q
Abstract
This article describes in detail the effect of cooling rate on the microstr ucture of a low-carbon Fe-12 pet Cr alloy. The alloy was prepared using a r elatively simple technique, i.e., rapid cooling of the melt in a copper wed ge mold. The dependence of microstructure on the cooling rate (similar to 4 0 to 10(5) W S) has been determined by X-ray diffraction (XRD), microhardne ss measurement, optical microscopy (OM), and transmission electron microsco py (TEM). It has been found that the matrix structure over a large cooling rate range is composed of columnar ferrite grains, the size of which decrea ses with increasing cooling rate. Precipitation of second phases has been o bserved at either the ferrite grain boundaries or within the ferrite grains . The former takes place along the entire wedge sample, whereas the latter characterizes a region 12 mm away from the tip of the wedge sample. The ess ential structure of the grain boundary precipitates was identified as marte nsite, which is a transformation product of austenite precipitated at high temperatures. Retained austenite was identified at the tip region as isolat ed particles (<4 <mu>m). The precipitates within the ferrite grains appeare d as planar colonies consisting of two sets of needles. The density of thes e precipitates increases with increasing the cooling rate while their size decreases. Characteristic precipitate-free zones (PFZs) at the ferrite grai n boundaries were observed and are discussed.