“…These attachment mechanisms between PNPs and the substrate are often similar to the interactions between PNPs and colloidal or aqueous components. In a simple system consisting of only pure water and clean silica sand, positively charged PNPs will be attracted to and retained by the negatively charged sand without any additional intervening processes. , Conversely, the electrostatic repulsion between negatively charged PNPs and the sand will stabilize the PNPs in solution and may improve their mobility. ,,,, Unmodified polystyrene (100 nm) nanoparticles, for example, were found to exhibit behavior similar to a conservative tracer during transport through a natural desert soil (with low OM and clay content) at a low ionic strength and a high pH, which is attributed to the negative ζ potential of both the soil and PNPs . When the fluid phase has a more complex composition, the presence of metal cations can limit the electrostatic repulsion between the particles through charge screening, increasing the relative effects of van der Waals interactions between PNPs and the substrate. ,,, Cations, like Ca 2+ , and dissolved organic matter may also be adsorbed by the PNPs and/or the substrate, mitigating the repulsion between them and facilitating sorption, or directly causing adsorption via cation or polymer bridging. ,,,, While DOM typically limits PNP mobility in soils, particulate organic matter, and in some cases even DOM, can actually increase PNP mobility by becoming attached to the PNP and/or substrate surfaces, resulting in steric or electrostatic repulsion between the PNPs and the substrate. ,,− While clean sand can provide initial insights into the mechanisms affecting PNP mobility in soil, natural systems are much more complex.…”