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The specific formation time strongly depends on the flow strength.
Both flow strength and hardening rate are size-dependent and increase with decreasing pillar size.
The ferrite phase in the two steels was found to have similar flow strength.
The dependences of particle deformation and migration on geometric confinement, flow strength, and fluid rheology are investigated.
Apart from these subtle variations, the area experienced large changes in flow strength due to seasonal differences in fluvial discharge.
Systematic changes in flow strength are documented by downstream cyclic variations in organic debris, bottomset thickness, and foreset dip.
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These flow strengths are comparable to those for pure electrodeposited nanocrystalline (d = 20 nm) Cu and Ni, respectively.
The combined effects of lattice friction, source-truncation hardening and forest hardening are found to be insufficient to fully account for the large flow strengths in smaller microcrystals.
The anisotropy of the yield and flow strengths is reversed and the planar anisotropy is reduced (r ∼ 1) in comparison to conventional alloys.
A Tabor factor of 2.7 often assumed in the literature may be inappropriate if the ratio of constituent flow strengths is large (>1.5 1).
For comparison, measured hardness and flow strengths of Al, Au, Fe 3%Si, Ti, W and Si nanostructures are reported in the 2 100 nm length scale regime.
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