Abstract
Unidirectional alternating (100)-(010) faceting has been observed for the clean TaC(110) surface using both high-resolution low-energy electron diffraction and scanning tunneling microscopy. Facets propagate periodically along the [11\ifmmode\bar\else\textasciimacron\fi{}0] direction and form a ridge-and-valley grating, characterized by an average periodicity of \ensuremath{\sim}6 lattice spacings in the [11\ifmmode\bar\else\textasciimacron\fi{}0] direction, where (110) terraces are completely absent. This faceted surface is shown to be an energetically favored structure.
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