An Assessment of the Greenwood-Williamson and Other Asperities Models, With Special Reference to Electrical Conductance

[+] Author and Article Information
M. Ciavarella

 Politecnico di BARI, V.le Gentile 182, 70125 Bari, Italymciava@poliba.it

F. Leoci

 Politecnico di BARI, V.le Gentile 182, 70125 Bari, Italy

J. Tribol 128(1), 10-17 (Sep 17, 2005) (8 pages) doi:10.1115/1.2125947 History: Received February 02, 2005; Revised September 17, 2005

Although in principle simple and neat results are obtained with the classical Greenwood-Williamson (GW) model (linearity of real contact area and conductance with load), the definition of asperity as local maxima of the surface leads to uncertain results for multiscale surfaces, as suspected already by Greenwood in a recent self-assessment of his theory [Greenwood, J. A., and Wu, J.J., 2001, “Surface roughness and contact: an apology  ,” Meccanica36(6), pp. 617–630]. Quoting the conclusions in the latter paper “The introduction by Greenwood and Williamson in 1966 of the definition of a ‘peak’ as a point higher than its neighbours on a profile sampled at a finite sampling interval was, in retrospect, a mistake, although it is possible that it was a necessary mistake”. Greenwood and Wu suggest that an alternative definition of asperity captures the mechanics of the contact more correctly, that of Aramaki-Majumbdar-Bhushan (AMB). Here, numerical experiments confirm that with a Weierstrass series fractal profile (taken as a 2D slice of a true fractal surface but then used to define a set of circular asperities), load and conductance for numerically measured asperities defined “à la Greenwood-Williamson” (3PP, 3-point peaks) differ significantly from the results obtained with the Aramaki-Majumbdar-Bhushan definition of asperity. The AMB definition, which is based on the bearing area intersection best parabola fitting, gives finite limits for all quantities and varies very little with small scale terms, and tends to coincide with the 3PP method only at unrealistically large fractal dimensions D, or at unrealistically large separations. However, it remains unclear how the AMB results compare with the proper treatment of the problem when interaction effects are fully taken into account.

Copyright © 2006 by American Society of Mechanical Engineers
Your Session has timed out. Please sign back in to continue.



Grahic Jump Location
Figure 1

The dimensionless parameters σw=m0,W∕g0 (a), σwp=m2,W∕(g0∕λ0) (b), and bandwidth parameter α (c), as a function of the number of terms N (from 1 to 10), of a Weierstrass series with γ=2. The three lines correspond to D=1.05, 1.5, and 1.95, respectively.

Grahic Jump Location
Figure 2

Example of Weierstrass series with γ=2 and for some fractal dimensions (D=1.05, 1.5, 1.95, respectively for a,b,c), plotted with the approximating parabolas (dashed line) at the 3PP peaks (solid line) for N=6 and 640 sample points

Grahic Jump Location
Figure 3

Example calculations of Weierstrass series with γ=2 and N=4,6,8,10 with fractal dimensions D=1.05, 1.5, 1.95, respectively, in each block of results (a,b,c). The asperity definition is 3PP, i.e., 3 points peaks.

Grahic Jump Location
Figure 4

Example calculations of Weierstrass series with γ=2 and N=4,6,8,10 with fractal dimensions D=1.05, 1.5, 1.95, respectively, in each block of results (a,b,c). The asperity definition is AMB, i.e., best fitting parabolas of the bearing area intersection.

Grahic Jump Location
Figure 5

Example results for Weierstrass series with γ=2 and both AMB and 3PP definitions of asperities. D=1.05 (a), 1.5 (b) and 1.95 (c). Weierstrass series with N=10 terms. The same set of random phases is used in both methods.



Some tools below are only available to our subscribers or users with an online account.

Related Content

Customize your page view by dragging and repositioning the boxes below.

Related Journal Articles
Related eBook Content
Topic Collections

Sorry! You do not have access to this content. For assistance or to subscribe, please contact us:

  • TELEPHONE: 1-800-843-2763 (Toll-free in the USA)
  • EMAIL: asmedigitalcollection@asme.org
Sign In