Nanoscale Titanium Dioxide (nTiO2) Transport in Natural Sediments: Importance of Soil Organic Matter and Fe/AI Oxyhydroxides

Many engineered nanoparticle (ENP) transport experiments use quartz sand as the transport media; however, sediments are complex in nature, with heterogeneous compositions that may influence transport. Nanoscale titanium dioxide (nTiO(2)) transport in water-saturated columns of quartz sand and variations of a natural sediment was studied, with the objective of understanding the influence of soil organic matter (SOM) and Fe/Al-oxyhydroxides and identifying the underlying mechanisms. Results indicated nTiO(2) transport was strongly influenced by pH and sediment composition. When influent pH was 5, nTiO(2) transport was low because positively charged nTiO(2) was attracted to negatively charged minerals and SOM. nTiO(2) transport was slightly enhanced in sediments with sufficient SOM concentrations due to leached dissolved organic matter (DOM), which adsorbed onto the nTiO(2) surface, reversing the zeta potential to negative. When influent pH was 9, nTiO(2) transport was generally high because negatively charged medium repelled negatively charged nTiO(2). However, in sediments with SOM or amorphous Fe/Al oxyhydroxides depleted, transport was low due to pH buffering by the sediments, causing attraction between nTiO(2) and crystalline Fe oxyhydroxides. This was counteracted by DOM adsorbing to nTiO(2), stabilizing it in suspension. Our research demonstrates the importance of SOM and Fe/Al oxyhydroxides in governing ENP transport in natural sediments.