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Compatible strain evolution in two phases due to epsilon martensite transformation in duplex TRIP-assisted stainless steels with high hydrogen embrittlement resistance
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The microscopic strain evolution is revealed by in-situ synchrotron XRD with EBSD.

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The γ → α′ transformation shows a shift of strain localization from austenite to ferrite.

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The γ → ε → α′ transformation shows a self-compatible strain evolution in multiphase.

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The compatible strain evolution can prevent the nucleation and growth of HICs.

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