Abstract
Fatigue crack growth rates have been determined on standard specimens containing long cracks (∼5–10mm) and on specimens containing two‐dimensional short cracks (∼0.10–0.50mm). Large differences have been observed indicating that at a given stress intensity factor short cracks propagate much faster than long cracks. Mouth opening displacement measurements for both specimen geometries have shown that the crack closure effect is largely responsible for the observed effect. These results are used to rationalize the behaviour of short cracks initiated from natural sites which were either graphite nodules or microshrinkage pores. The three‐dimensional aspect of these natural small cracks is analysed and discussed in detail.
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