Issue 78
T. Nasri et alii, Frattura ed Integrità Strutturale, 78 (2026) 275-297; DOI: 10.3221/IGF-ESIS.78.17
The large grain size scatter (±203 µm for L d and ±47 µm for TL d ) uncertainty in ξ that propagates into coefficient identification. The relative uncertainty propagates as:
δξ δ d 47
203 395
d 154
and
30% type A ,
51% type B
(7)
ξ
This intrinsic microstructural uncertainty partly explains the scatter of μ ᵢ around the fitted Chebyshev curve, which is more pronounced for type B (NRMSE = 8.50 %) than for type A (NRMSE = 7.87%). Chebyshev-enriched Paris model The enriched model takes the form of the classical Paris law multiplied by a microstructural modulation factor μ ( ξ ) :
/ · ( ) n da dN C K
(8)
with the modulation factor expressed as an expansion on the Chebyshev basis:
N
0 1 k
· a T
(9)
k k
Combining these elements, the complete enriched model reads:
N
da
a d
n
with f
· C K
a T
· 1
1, 1
(10)
k k
dN
k
0
This is the central equation of the proposed model. When all k a = 0, d a /dN = C·( Δ K) ⁿ exactly, confirming that the enriched model is a conservative extension of the classical Paris law. The multiplicative term [1 + Σ a ₖ T ₖ ( ξ )] amplifies or attenuates the Paris prediction according to the crack position in the microstructure, reflecting intragranular accelerations and grain boundary retardations. Physical admissibility further requires μ ( ξ ) to remain strictly positive over the entire domain:
N
min
a T
1
0
(11)
min
k k
1,1
k
0
This positivity condition is verified numerically over a fine grid of 10 000 points uniformly distributed on [ − 1, 1] after each identification. For both specimen types, μ min > 0 is satisfied, guaranteeing that the model never predicts a zero or negative propagation rate: μ min = 0.252 for type A (reached near ξ ≈ − 0.85, corresponding to the initiation region close to the hole edge) and μ min = 0.152 for type B (reached near ξ ≈ +0.72, in the post-GB ₁ deceleration zone). For high-degree polynomials, Runge-type oscillations are mitigated by the Chebyshev basis itself, whose minimax property (Eq 5) minimises the maximum deviation between knots, bounding inter-point excursions to a fraction of the observed μ min margins. Finally, the model relies on a clear scale separation: C and n describe the macroscopic average behaviour identified directly on each holed specimen type, while the coefficients k a describe microstructural fluctuations at the mesoscopic (grain-by-grain) scale. Physical interpretation of the model components The variable ( / ) f a d is directly linked to the grain size d in the propagation direction. Changing the propagation direction changes d , and therefore modifies the physical scale on which the polynomial oscillations develop. The ratio / d d = 2.56 implies that, for the same number of grains crossed, ξ A evolves over a 2.56 times smaller physical scale than ξ B in terms of physical crack length. Combined with the number of grains actually crossed ( N g-A = 3.72 > N g-B = 1.55), this physical scale difference was initially thought to explain a higher optimal order for type A. However, both orientations converge to the same statistically optimal order, N = 21.
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