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Microstructural Alterations in Hertzian Fatigue
Robert Errichello, GEARTECH
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Martensite Decay Under Moderately High Hertzian
Stress
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Classic Subsurface-Initiated
Macropitting
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Subsurface Orthogonal Shear Stress, o
= 0.256po = maximum alternating orthogonal shear stress (basis of L-P theory) o y = 0.85b = locations of o o z = -0.50b = depth of o o 2 = 0.512po = range of o o
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Morphology of Classic Subsurface-Initiated Macropitting
A
B
C D
D E
F
A- Macropit entry (end first reached by roller) B- Origin located at inclusions at depth of max orthogonal shear stress o C- Typical near-radial branch cracks D- Serration on crater bottom formed by change in crack direction E- Macropit bottom consisting of series of cracks at depth of max shear stress 45 F- Macropit exit formed by crack rising in the rolling direction at 30
Ref: T.E. Tallian, Failure Atlas for Hertz Contact Machine Elements, ASME, 1999.
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Morphology of Butterflies
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Morphology of IrWEAs & WECs
30