Ck. Gurumurthy et al., Water-assisted sub-critical crack growth along an interface between polyimide passivation and epoxy underfill, INT J FRACT, 109(1), 2001, pp. 1-28
Direct chip attach (DCA) microelectronic packaging technology is gaining pr
ominence due to its numerous advantages. Delamination (debonding) of the un
derfill epoxy/ polyimide passivation interface of a DCA during hydro-therma
l reliability testing has always been one of the salient problems. We have
studied the water-assisted sub-critical crack growth along this interface a
nd our measurement offers important clues as to the origins of the poor hyd
ro-thermal testing results for these interfaces. A modified asymmetric doub
le cantilever beam (ADCB) testing technique has been used to measure the su
b-critical crack growth velocity v at various relative humidities and tempe
ratures as a function of the crack driving force (strain energy release rat
e) G*. The presence of a significant partial pressure of water p(H2O) produ
ces a marked decrease (by up to a factor of 12) in the threshold G* for cra
ck growth at measurable velocities. Above the threshold log v rises linearl
y with rootG* but then enters a regime where the crack velocity (v = v*) is
almost independent of rootG*. Finally, at the values of G* corresponding t
o rapid crack propagation in the absence of water, log v increases very rap
idly with G*. By analogy to the classic work on water-assisted sub-critical
crack growth in silica-based glasses, where very similar features are obse
rved, we believe that the sub-critical crack growth along the polyimide-epo
xy interface results from stress-assisted hydrolysis of primary covalent bo
nds, in our case ester bonds across the interface. The regime of rootG* jus
t above the threshold corresponds to a physicochemical situation where the
water activity (p(H2O)) at the crack tip is the same as that of the gaseous
environment. In the regime where v = v* approximate to constant, the water
activity at the crack tip is below that in the environment and the crack g
rowth velocity is limited by the transport of water vapor to the bonds ahea
d of the crack tip. We develop a model of this crack growth following Wiede
rhorn 1967 that allows us to predict the sub-critical crack growth as a fun
ction of G* for arbitrary relative humidity and temperature conditions.