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<metadata xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/"><dc:title>Estimate of Coffin–Manson curve shift for the porous alloy AlSi9Cu3 based on numerical simulations of a porous material carried out by using the Taguchi array</dc:title><dc:creator>Tomažinčič,	Dejan	(Avtor)
	</dc:creator><dc:creator>Klemenc,	Jernej	(Avtor)
	</dc:creator><dc:subject>low-cycle fatigue</dc:subject><dc:subject>aluminium alloys</dc:subject><dc:subject>porosity</dc:subject><dc:subject>Coffin–Manson relationship</dc:subject><dc:subject>Taguchi</dc:subject><dc:subject>multivariate regression analysis</dc:subject><dc:description>In real engineering applications, machine parts are rarely completely homogeneous; in most cases, there are at least some minor notch effects or even more extensive inhomogeneities, which cause critical local stress concentrations from which fatigue fractures develop. In the present research, a shift of the Coffin–Manson ε$_a$–N material curve in a structure with random porosity subjected to dynamic LCF loads was studied. This allows the rest of the fatigue life prediction process to remain the same as if it were a homogeneous material. Apart from the cyclic σ–ε curve, which is relatively easy to obtain experimentally, the ε$_a$–N curve is the second most important curve to describe the correlation between the fatigue life N and the strain level ε$_a$. Therefore, the correct shift of the ε$_a$–N curve of the homogeneous material to a position corresponding to the porous state of the material is crucial. We have found that the curve shift can be efficiently performed on the basis of numerical simulations of a combination of five porosity-specific geometric influences and the associated regression analysis. To model the modified synthetic ε$_a$–N curve, five geometric influences of porosity by X-ray or µ-CT analysis are quantified, and then the porosity-adjusted coefficients of the Coffin–Manson equation are calculated. The proposed approach has been successfully applied to standard specimens with different porosity topography.</dc:description><dc:date>2022</dc:date><dc:date>2022-03-21 09:36:14</dc:date><dc:type>Članek v reviji</dc:type><dc:identifier>135574</dc:identifier><dc:identifier>UDK: 620.178.3:669.715</dc:identifier><dc:identifier>ISSN pri članku: 1996-1944</dc:identifier><dc:identifier>DOI: 10.3390/ma15062269</dc:identifier><dc:identifier>COBISS_ID: 101646083</dc:identifier><dc:language>sl</dc:language></metadata>
