A diffusion-driven CH4–O2 boundary structures methane oxidation and carbon transformation in upland soils
This study uses a controlled natural gas release to show that methane attenuation in aerated upland soils is governed by a spatially constrained CH4–O2 boundary. Within this overlap zone, gas diffusion, oxygen availability, carbonate restructuring, and methanotroph activity interact to shape methane oxidation and carbon transformation.