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Nonetheless, a mechanistic comprehension of the basis for such heterogeneity is lacking. Here, we incorporate deposit CH4 information through the Hanford reach of the Columbia River with a biogeochemical-transport model to exhibit that vertical hydrologic exchange moves (VHEFs), driven by the difference between river stage and groundwater amount, determine CH4 flux at the sediment-water program. CH4 fluxes show a nonlinear relationship because of the magnitude of VHEFs, w