Dynamic colloid--water partitioning of pyrene through a coastal Baltic spring bloom

Colloidal organic particles constitute the dominant portion of particulate organic matter in surface seawater, but their influence on the phase speciation and bioavailability of hydrophobic organic compounds (HOCs) is sparsely evaluated. Studies on colloid-water partitioning have been focused on other regimes and have largely been performed on chemically defined subportions of total colloids such as the humic fraction. Available estimates of colloid-water partition coefficients (Kcoc) are highly variable and not easily explained by regularly applied Kow-Koc relationships. Here, pyrene was partitioned to bulk natural colloids isolated using cross-flow ultrafiltration techniques from the surface water of a coastal bay. A key objective was to elucidate biogeochemical controls on the changing colloid-sorbent qualities over the course of the dynamic allochtonous-autochtonous transition of a well-constrained boreal coastal spring bloom. The pyrene Kcoc was found to decrease from 12.9+/-0.9 x 10(3) Lw/kg(oc) in the terrestrial runoff dominated regime to values around 2.9+/-0.7 x 10(3) Lw/kg(oc), once phytoplankton production became the governing source of organic matter to the surface waters. The changing Kcoc was well correlated with the molar extinction coefficient at 280 nm of the colloidal organic carbon. This study supports other reports of an improved prediction of HOC phase speciation through this simple molecular proxy of the "quality" of organic sorbents. While being poor sorbents on a carbon atom basis, relative to soils and sediments, coastal marine colloids, by their shear abundance, may significantly attenuate the truly dissolved exposures of HOCs with log Kow above 5.