Crack Paths 2006
P R A C T I C AELX A M P L E
The developed model has been used for simulation of the surface fatigue crack growth
on a real spur gear pair, which has been experimentally tested. The gear pair is made of
carburized steel 16MnCr5 (according to the ISO standard) with Young’s modulus
E=2.06105 N/mm2and Poisson ratio Q=0.3. The maximumcontact pressure p0=1550
N/mm2is acting at the inner point of single teeth pair engagement (point B), with the
equivalent radius of gear teeth flanks R*=10 m mand half-length of the contact area
b=0,274 mm. The Hertzian normal loading distribution p(x) along the entire contact
width of the gear flanks has then been determined using eq. (1).
For all computations, the coefficient of friction P=0.04 has been used, which is the
average value for well-lubricated gears [11]. Therefore, the tangential loading q(x) has
been determined using eq. (3).
The influence of EHD-lubrication on the normal loading distribution p(x) has been
estimated using eqs. (4) to (8) for the lubricant oil ISO-VG-220, with the kinematic
viscosity Q40 = 220 mm2/s, density U15 = 0.9 kg/dm3 and pressure-viscosity coefficient D=0.1810 7 m2/N. The mean surface velocity of the contacting surfaces has been taken
as a constant value u=5 m/s, which is a commonvalue for gears [11]. Using these
parameters, the dimensionless pressure spike amplitude Y and the dimensionless
pressure spike location X (see Figure 1) are equal to X= 0.9462 and Y= 0.8146,
respectively.
The hardness distribution H and the carbon content C (%) in the surface layer of the
gear teeth flanks have been determined using the theory described in [9], where the
following values have been measured previously: H1=765 HV, H2=770 HV, H3=450
HV,Deff=1.25 mm,D2 =0.1 m m(see Figure 3). The distribution of residual stresses on
the basis of hardness distribution is shown in Figure 4.
-800
10%retained austenite
-76500
Pa ]
s s e s [ M
d u a l s t r e
-400
-300
R e s i
-200
-100
0
0.00.20.40.60.81.01.21.41.61.82.02.22.42.62.83.03.2
DepthD[mm]
Figure 4. Distribution of the residual stresses along depth D
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