Nonlinear Response of Soil Hydrothermal Processes to Rock Fragment Content: Evidence From Soil Column Experiments
Rock fragments (RFs; mineral particles with diameter ≥ 2 mm) are a ubiquitous component of soils and strongly influence hydrothermal processes by altering pore structure and physical properties. However, the nonlinear and dynamic responses of soil hydrothermal processes to variations in rock fragment content (RFC)...