Abstract
The impact of increasing anthropogenic hydrogen (H(2)) emissions on Earth's radiative balance depends on the soil microbial H(2) sink-the largest and most uncertain term in the global H(2) budget. Soil moisture is a primary but poorly quantified control regulating the soil sink. Here, we assess the sensitivity of microbial H(2) oxidation to soil moisture in laboratory experiments with temperate and arid soils spanning distinct textures. We report H(2) oxidizer activity down to -70 to -100 MPa water potentials across soils, which are among the driest conditions reported for microbial activity and are much drier than assumed in global simulations of H(2). Using genome-resolved meta-omics, we link H(2) oxidation dynamics in temperate soils to specific desiccation-adapted microbial taxa that contribute differentially to H(2) uptake along the moisture gradient. Through global simulations, we show that our observationally constrained drier moisture threshold increases the contribution of arid and semi-arid regions for soil H(2) uptake by 4-7 percentage points (pp), while decreasing the contribution of temperate and continental regions (-7 pp). Our results highlight the importance of H(2) uptake under extreme hydrological conditions, particularly the roles of desertification, dryland expansion, and H(2)-oxidizer ecophysiology in modulating long-term changes in H(2) uptake.