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Similar patterns were observed at subsurface 5 15-cm depth soils.
A methodology is developed to analyze potency of fatigue crack nucleation at subsurface inclusions.
Inclusions at subsurface are common sites for fatigue crack nucleation in these alloys when cycles to failure was >107 cycles.
Under these circumstances, fatigue cracks nucleate at subsurface porosity and show a typical fish-eye pattern of fracture surface.
A computational strategy is developed to characterize the driving force for fatigue crack nucleation at subsurface primary inclusions in carburized and shot peened C61® martensitic gear steels.
Quantitative microscopic investigations of the distribution of the α- and β-phase of Ti6Al4V show that inhomogeneities in the phase distribution exist at subsurface crack initiation sites.
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However, the most stable state was found with a formation energy of about -0.57 eV when a VO was located at the subsurface nearly at the center of two Pd atoms, as seen in Figure 2 group II (b).
The oldest known age of the Benin Formation at the surface is Miocene while at the subsurface is Oligocene.
Panels (a2) to (c2) represent the PDOSs of Pd-2, which is located at the third FeO2 layer (a2), at the subsurface (b2), or the first FeO2 layer (c2).
Vertical mixing is particularly intense in the boundary zone between the equatorial under current at the subsurface and the south equatorial current at the surface.
The Ge-II structure (in yellow) initially appears centrally at the subsurface region beneath the indenter instead of at the region right under the tool.
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