There has been an increase in demand worldwide for efficient use of natural gas. Thus, studies have been investigating the oxidative coupling of methane (OCM) to higher hydrocarbons, which can directly form a C−C bond in a single reactor at high temperatures. However, the OCM reaction still has a drawback of low product selectivity due to overoxidation of the C 2 products. Among the OCM catalysts investigated, alkali-based catalysts, especially Na 2 WO 4 and K 2 WO 4 , have demonstrated a high C 2 yield via a unique response to H 2 O, one of the dominant products of the OCM reaction. It was postulated that the catalyst forms highly reactive OH radicals from O 2 and H 2 O, which is responsible for its high selectivity and conversion rate. Previous studies with near-ambient-pressure X-ray photoelectron spectroscopy suggested the involvement of alkali (su)peroxide formation. Based on this, density functional theory calculation was applied to examine an unmolten K 2 WO 4 surface (in contrast to molten Na 2 WO 4 ). To construct the crystal structure for calculation, in situ Xray diffraction measurement was used, which provided the crystal phase of hexagonal K 2 WO 4 at temperatures relevant to OCM. This phase resulted from the transformation of monoclinic K 2 WO 4 under ambient conditions. Generally, a stable surface was found to occur with K atoms on the outer surface rather than with the O-or W-exposed surfaces. After considering various intermediates with different positions, a plausible surface pathway that leads to H 2 O 2 through adsorptions of H 2 O and O 2 was suggested. The calculation results support the hypothesis of the involvement of OH radicals in the OCM through a unique water-activation pathway.