Formation of stable soil structural units through binding of soil particles by organic compounds and microbial processes
Loss of biodiversity and decreased soil nitrogen retention when nitrogen availability exceeds plant demand
Process by which ant foraging and nesting activities alter soil chemistry by accumulating organic matter and nutrients near colonies
The degree to which soil carbon dioxide efflux rates change with soil temperature, typically quantified as Q10 or temperature response function parameters
The dissolved phosphorus fraction immediately available for biological uptake, measured as the proximate cause of bloom formation
Process starting with PAH which stack into particles, then spheres, then agglomerates, finally mature soot