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Journal of the European Ceramic Society
journal homepage: www.elsevier.com/locate/jeurceramsoc
Original Article
Relationship of energy to geometry in brittle fracture
J.J. Mecholsky Jr.
a,
*, N.A. Mecholsky
b
, D.P. DeLellis
a
a
Materials Science and Engineering Department, University of Florida, Gainesville FL 32611 USA
b
Vitreous State Laboratory, The Catholic University of America, Washington, DC 20012, USA
ARTICLE INFO
Keywords:
Fracture
Fractal geometry
Crack branching
Fractography
Fracture energy
ABSTRACT
Numerous investigators have noticed that there is a relationship between the energy of branching and the energy
of initiation during a fracture event in materials that fail in a brittle manner. Usually, this is measured in terms of
the stress intensities, i.e., K
B
/K
c
. The ratio has been reported between 3 and 4, implying a constant value.
However, data suggests that it is a constant for a material, but not a universal constant. The fractal dimension of
the fracture surface is related to the critical stress intensity factor. It is a measure of the tortuosity of the fracture
surface. We show that the K
B
/K
C
ratio is directly related to the square root of the fractal dimensional increment,
indicating a relationship between the energy of crack propagation and the tortuosity of the fracture surface.
1. Background
Since the discovery of the fractal nature of fracture surfaces by
Mandelbrot, Passoja and Paullay [1], there have been numerous papers
on fractal fracture of materials [2–10]. The most alluring aspect of the
fractal nature is the scaling of geometry on the fracture surface [11].
This scaling aspect is most intriguingly observed in materials that fail in
a brittle manner, e.g., glass, glass ceramics and ceramics [12]. When a
brittle material fractures, there is usually one source of the initial
fracture. The crack then grows in a radial pattern and forms what has
been termed the mirror, mist and hackle regions. If enough energy is
available, the crack macroscopically branches. These are the branches
that are visibly obvious to any observer. Many studies have identified
these regions in numerous materials [13]. Further studies [14,15] have
demonstrated that there is scaling relationships between the size of the
fracture initiating crack and the distance to the boundaries, r
j
, between
the mirror-mist, mist-hackle, and hackle-crack branching boundaries
c/r
j
=C
j
for j=1,2,3 (1)
where C
j
is the corresponding constant for the mirror-mist (1), mist-
hackle (2), and hackle-crack branching (3) boundaries, respectively.
The fractal dimensions of fracture surfaces have been measured for
a number of materials including metals, polymers, and ceramics
[6,9,16,17]. Here, the term “ceramics” includes inorganic glasses, glass
ceramics, and single crystal ceramics. It has been shown [18] that the
fractal dimension in the form of the fractal dimensional increment is
directly related to the energy of fracture, γ:
2γ =a
0
ED* (2)
where a
0
is a characteristic dimension of the structure, E is the elastic
modulus, and D* is the fractal dimensional increment. The fractal di-
mensional increment is the fractional part of the fractal dimension of
the fracture surface, i.e., 2 + D*. It is known to be constant for non-R-
curve materials. Similar to Eq. (2), it can be shown that D* is related to
the critical stress intensity factor by the following relationship [3]:
K
c
=a
0
1/2
E D*
1/2
. (3)
It was later shown [19] that
c/r
B
= (Y
B
/Y
c
)
2
(a
0
/b
0
) D* (4)
where Y
B
is the geometric factor at branching, Y
c
is the geometric factor
at the initiation of fracture, a
0
is the characteristic dimension in Eq. (2)
and b
0
½
is the slope of the crack branching stress intensity, K
B
, and
elastic modulus, E, graph [20–22], i.e.,
K
B
/E=Y
B
A
B
/ E = (b
0
)
1/2
. (5)
A
B
is the “mirror” constant at branching. Eq. (4) indicates that the
scaling in the plane of fracture is related to the tortuosity of the fracture
surface, i.e., the scaling perpendicular to the apparent planar fracture
surface.
There have been many studies attempting to relate the crack
branching phenomenon to the initiation of fracture [23,24]. Some re-
late this to the dynamics of the fracture process [24,25], others to the
details of the stress at the tip of the propagating crack [26,27], and still
others to the velocity of crack propagation [28–31]. Fractographic
https://doi.org/10.1016/j.jeurceramsoc.2020.05.002
Received 26 March 2020; Received in revised form 21 April 2020; Accepted 2 May 2020
⁎
Corresponding author.
E-mail address: jmech@mse.ufl.edu (J.J. Mecholsky).
Journal of the European Ceramic Society 40 (2020) 4602–4604
Available online 08 June 2020
0955-2219/ © 2020 Elsevier Ltd. All rights reserved.
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