Multiscale Characterizations of Surface Anisotropies

被引:22
作者
Bartkowiak, Tomasz [1 ]
Berglund, Johan [2 ,3 ]
Brown, Christopher A. [4 ]
机构
[1] Poznan Univ Tech, Inst Mech Technol, PL-60965 Poznan, Poland
[2] Rise Res Inst Sweden, Dept Mfg, SE-43153 Molndal, Sweden
[3] Chalmers Univ Technol, Dept Ind & Mat Sci, SE-41296 Gothenburg, Sweden
[4] Worcester Polytech Inst, Surface Metrol Lab, Worcester, MA 01609 USA
关键词
surface texture; anisotropy; multiscale; TOPOGRAPHY; PARAMETERS; ROUGHNESS; SCALES;
D O I
10.3390/ma13133028
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Anisotropy can influence surface function and can be an indication of processing. These influences and indications include friction, wetting, and microwear. This article studies two methods for multiscale quantification and visualization of anisotropy. One uses multiscale curvature tensor analysis and shows anisotropy in horizontal coordinates i.e., topocentric. The other uses multiple bandpass filters (also known as sliding bandpass filters) applied prior to calculating anisotropy parameters, texture aspect ratios (Str) and texture directions (Std), showing anisotropy in horizontal directions only. Topographies were studied on two milled steel surfaces, one convex with an evident large scale, cylindrical form anisotropy, the other nominally flat with smaller scale anisotropies; a mu EDMed surface, an example of an isotropic surface; and an additively manufactured surface with pillar-like features. Curvature tensors contain the two principal curvatures, i.e., maximum and minimum curvatures, which are orthogonal, and their directions, at each location. Principal directions are plotted for each calculated location on each surface, at each scale considered. Histograms in horizontal coordinates show altitude and azimuth angles of principal curvatures, elucidating dominant texture directions at each scale. Str and Std do not show vertical components, i.e., altitudes, of anisotropy. Changes of anisotropy with scale categorically failed to be detected by traditional characterization methods used conventionally. These multiscale methods show clearly in several representations that anisotropy changes with scale on actual surface measurements with markedly different anisotropies.
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页数:19
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