Surface strain has recently been shown to have a significant effect on the reactivity of transition-metal surfaces, [1] and numerous examples of strain effects on both the thermochemistry and kinetics of surface reactions have been identified. [2][3][4][5][6][7] Several of these studies focused on strain induced by epitaxial metal overlayers, but recently it has been demonstrated that strain from another source, namely, dislocations that intersect crystal surfaces, likewise causes significant changes in surface reactivity. [8] This suggests that a careful study on the effect of strain on catalytic processes might yield substantial insights into the effect of defects on these processes. Defects, in turn, have been shown to dominate the reactivity of certain surface reactions. [9] In particular, an analysis of the manner in which strain influences the population of subsurface species in transition metals could contribute to an understanding of the more general problem of how dislocation-induced surface defects mediate the transfer of adsorbates to subsurface regions. Such an analysis could permit a comparison between the behavior of subsurface species on single-crystal and polycrystalline metals, [10,11] and it could have broad application to a number of technologically important problems, including the catalytic reactivity of subsurface oxygen and carbon in connection with corrosion, oxidation, or carbonylation processes, [12,13] subsurface hydrogen reactivity for hydrogenation and hydrogenolysis reactions, [14][15][16][17][18][19] hydrogen storage in and embrittlement of metals, [11,20,21] and the purification of hydrogen fuel streams with Pd-alloy membranes. [22,23] Here we analyze the effect of strain on the creation of subsurface species in metals by focusing on the hydrogen/ nickel system and using periodic, self-consistent density functional theory (DFT) calculations. As recent atomically resolved STM images of surface defects on Ru(0001) showed regions with lattice stretching of up to 10 % in the immediate vicinity of these defects, [8] we focused our studies on Ni(111) slabs with 3 and 10 % expansive strain. We show that, while very high H 2 pressures are required to produce subsurface hydrogen on perfect, unstretched Ni(111) surfaces, [24] only modest pressures (on the order of tens of bar) are required for subsurface hydrogen to form on the stretched Ni surfaces that might exist in the vicinity of defects. We also demonstrate that strain qualitatively changes both the site preferences of subsurface hydrogen and the character of the stable surface and subsurface phases of the H/Ni(111) system. We discuss these results in the context of defect-mediated penetration of hydrogen into subsurface regions of both single-crystal and polycrystalline nickel catalysts, and we comment on the implications of the results for other processes involving various subsurface species in transition metals.A summary of the low-coverage (q = 0.25 ML (ML = monolayer), corresponding to one H atom per four surface Ni atoms) data fo...