Soil Texture Regulates Bacterial Motility and Chemotactic Recruitment to Plant Roots

Soil microbial communities regulate critical ecological processes, including nutrient cycling, carbon sequestration, and plant growth. However, due to the opacity and structural complexity of soil, how physical constraints imposed by pore geometry influence bacterial motility and chemotactic recruitment to plant roots remains poorly understood. We use a transparent soil mimic composed of cryolite grains that replicates the structural characteristics of natural soils while enabling direct visualization of bacterial dynamics. Using as a model bacterium, we combine macroscopic spreading assays with microscopic tracking of cellular trajectories to characterize how soil texture affects motility across pore scales. We find that bacterial motility shifts from run-and-tumble behavior in large, open pores to frequent trapping in smaller, more confined spaces. This transition is governed by the pore size distribution and leads to reduced effective diffusivity and slower population-scale spreading. Moreover, pore-scale confinement hinders the chemotactic recruitment of bacteria to roots: recruitment is robust in sandy and loamy soils but negligible in highly confining textures. Our results establish soil texture as a critical factor regulating microbial dynamics and ecological interactions in the rhizosphere. This mechanistic understanding complements genomic surveys by identifying physical confinement as an ecological filter that shapes root-associated microbiomes. These findings highlight the essential and previously underappreciated role of soil texture, suggesting new strategies for managing microbial communities to promote plant health and sustainable agriculture.