The Cotterell/Rice[] prescription for the local stress intensity factor of a kinking crack when applied to an interface is given by[]
is the (complex) remote load stress intensity factor of the bulk
material (i.e. without the interface) written as
.
is the phase angle of the
remote load. The stress intensity factor of the unkinked interfacial crack is
written as
with the connection given above to the local
stress intensity,
, and to the shear stress,
. This definition for the stress intensity factor
differs slightly from that in common use[], but is appropriate for the
crack and load geometry in use in this work.
In these equations, the additional phase angle at
the crack tip generated by the elastic mismatch at the interface is
given by
.
is a singular logarithmic function
of the distance,
, from the crack tip-the mode mixing anomaly
characteristic of interfacial cracks in the continuum limit.
is a constant which depends on the
elastic mismatch, where
and
are the standard isotropic
elastic parameters for the two materials. The second form for
in the last equation in (3) refers to the 2D
hexagonal lattice, with the two spring constants,
and
.
The approximation by Cotterell and Rice[] is to
recognize that the shear
stress when normalized by the square root of the radius has the
dimensions of the stress intensity factor, and when written in terms
of the angular variables, and
, has the actual character
of the appropriate tensile or shear stress intensity factor for the
branching crack. This approximation is rigorous, of course, in the
limit of small
.
Explicit expressions for the 's are given by[]
It is more useful to write these complicated expressions in terms of a set of angular phase shifts in the form
These last equations are written for a critical value of the local stress
intensity factor (with a prime) corresponding to emission, cleavage,
etc. The total local phase shift for the crack is composed of the
separate contributions from the phase shift for the remote load, ; the
geometrical contribution due to the kink angle,
; and the
interfacial phase shift,
, written in terms of the core size,
.
is a function of the interface mismatch, as well
as the kink angle,
.
Earlier[], we have found that the core size,
,
can simply be set equal to the range parameter in the force
law. The reader should note that the stress field of the
kinked crack is not phase shifted by the length of the kink, because the
crack is now off the interface in homogeneous material. However, the
stress intensity factor in (3) does contain the phase
shift[]. The physical reason why the
local stress intensity of the kinked crack is phase shifted by the
interfacial mismatch is that the kinked crack is ``loaded'' by
the phase shifted stress field of the parent interface crack.
The criteria for critical events in terms of the local stress intensity factors are written with the subscripts corresponding to cleavage or emission. Thus
for cleavage, and
for emission.
In these equations, an appropriate shear modulus must be taken. If
the crack is kinked off the interface into material 2, then
, while if the crack is on the interface, then
, and the prime on the
represents taking the appropriate plane strain or plane stress
elastic modulus. In plane stress, which must be used in the 2D
simulations,
, where
and
have their
standard elasticity definitions. The appropriate ``right hand sides''
for the lattice resistance in these equations are to be determined
by computer simulations.
The accuracy of these Cotterell/Rice expressions are easily checked in
the zero mismatch case from their paper, where comparisons are graphed
as a function of the branching angle[]. The main deviation
appears in the value for , where the analytic
expression is about 10%higher than the correct numerical value
at
. All other
's are accurate to
within a percent or so.