Materials Science and Engineering A 507 (2009) 58–60
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Materials Science and Engineering A
journal homepage: www.elsevier.com/locate/msea
Part I: Anisotropy of cracking from oxygen-induced dynamic embrittlement in
bicrystals of IN718
William M. Kane
a,b
, U. Krupp
a,c
, C.J. McMahon Jr.
a,∗
a
Department of Materials Science and Engineering, University of Pennsylvania, Philadelphia, PA 19104, United States
b
Exponent Failure Analysis Associates, 3401 Market Street, Philadelphia, PA 19104, United States
c
Fachhochschule Osnabrück, P.O. Box 19 40, D-49009 Osnabrück, Germany
article info
Article history:
Received 20 June 2008
Received in revised form
24 November 2008
Accepted 2 December 2008
Keywords:
Dynamic embrittlement
IN718
Bicrystals
Intergranular fracture
High-temperature brittle fracture
Superalloys
abstract
It is shown that cracking from oxygen-induced dynamic embrittlement in bicrystals of the nickel-base
superalloy IN718 having symmetrical ˙ =5 (013) tilt boundaries is considerably more rapid in the fast-
diffusion direction parallel to the tilt axis than in the direction perpendicular to this axis. This lends
support to the model that envisions the process as caused by diffusive penetration of grain boundaries
ahead of a sharp crack by a surface-adsorbed embrittling element.
© 2008 Elsevier B.V. All rights reserved.
1. Introduction
Dynamic embrittlement is the diffusion-controlled intergran-
ular cracking that can occur in a high-strength alloy that has a
cohesion-lowering element adsorbed on a free surface. It was first
characterized in studies of oxygen-induced cracking of a Ni-Al inter-
metallic [1] and of sulfur-induced cracking of a pressure-vessel
steel [2]. One characteristic that is generally noted in polycrystals is
the disparity in the susceptibility to cracking among various grain
boundaries. This was noted particularly in a study involving the
nickel-base alloy IN718 [3].
This behavior was also noted in the highly susceptible Cu–8%Sn
alloy [4]. A later study of cracking of bicrystals of this alloy having
symmetrical ˙ =5 (013) tilt boundaries showed that it occurred
much more rapidly along the tilt axis (i.e., the fast-diffusion direc-
tion) than perpendicular to the tilt axis [5]. This supported the
proposition that the phenomenon involves diffusive penetration
by the surface element into the core of a sharp crack and that
the atomic configuration along the grain boundary would play a
decisive role.
∗
Corresponding author.
E-mail addresses: wkane@exponent.com (W.M. Kane),
cmcmahon@lrsm.upenn.edu (C.J. McMahon Jr.).
The Cu–Sn alloy study involved the matrix element, tin, which
is known to be surface active [4] and is an embrittling element
in steels [6], for example. It has also been shown to segregate to
grain boundaries in the Cu–Sn alloy during elevated-temperature
aging [7]. In contrast, the oxygen-induced cracking of nickel-base
alloys involves an element from the vapor phase extraneous to
the alloy that is not to be found ab initio in the grain boundaries.
The present study was carried out to determine what kind of
cracking anisotropy would be found in the commonly used alloy
IN718 in experiments similar to the previous ones on the Cu–Sn
alloy.
This first part of a two-part paper serves as the introduction
to both and as the basis for understanding the anisotropy of the
cracking process in polycrystalline material, which is the subject of
Part II. The same specimen preparation for the bicrystals is used in
Part II, and thus Part I also serves to explain that.
The ˙ =5 (013) tilt boundary was again selected for this pur-
pose because of the great disparity in self-diffusivity in the parallel
and perpendicular directions found previously in this boundary
in another FCC material, silver. The calculated [8] atomic struc-
ture of this boundary in an FCC lattice is shown in Fig. 1(a),
and the diffusion results of Mishin and Herzig [9] are shown in
Fig. 1(b). The presence of “diffusion pipes” along the tilt axis is
readily apparent, and the diffusivity along these “pipes” is about
double that in the perpendicular direction for self-diffusion in
silver.
0921-5093/$ – see front matter © 2008 Elsevier B.V. All rights reserved.
doi:10.1016/j.msea.2008.12.002