Degradation mechanisms: biopolymers break down in soil through enzymatic hydrolysis (polysaccharides), oxidative degradation (lignins) or a combination of processes. The rate depends heavily on temperature, moisture and the microbiome. In anaerobic substrates (landfills, waterlogged soils) degradation can be considerably slower — for those sites the service life and residual concentration have to be assessed per project.
Soil-polymer interaction: polysaccharides adsorb preferentially onto positively charged surfaces (iron oxides, aluminium oxides) through electrostatic interaction and hydrogen bonding. In acidic soils (pH < 5.5) the surface charge shifts — adsorption strength, and with it service life, falls. Formulations for acidic substrates require pH correction or a different binder class.
IPEC formation (interpolyelectrolyte complexes): where anionic and cationic polymer components are used together, insoluble complexes can form spontaneously, disrupting application or triggering unwanted precipitation reactions in the soil. SRBT accounts for this during formulation development — mixing sequence, pH and ionic strength of the mixing water are application parameters, not side conditions.
Mineral reinforcement: clay minerals such as bentonite or metakaolin form charged complexes with biopolymers (biocomposites) whose mechanical properties clearly exceed those of the individual components. Bentonite swells on contact with water and closes microcracks in the binder matrix — a self-healing effect that pure polymer films do not have.