Methods involving polyoxymethylene (POM) as a passive sampler are increasing in popularity to assess contaminant freely dissolved porewater concentrations in soils and sediments. These methods require contaminant-specific POM-water partition coefficients, K POM . Certain methods for determining K POM perform reproducibly (within 0.2 log units). However, other methods can give highly varying K POM values (up to 2 log units), especially for polycyclic aromatic hydrocarbons (PAHs). To account for this variation, the authors tested the influence of key methodological components in K POM determinations, including POM thickness, extraction procedures, and environmental temperature and salinity, as well as uptake kinetics in mixed and static systems. All inconsistencies in the peer-reviewed literature can be accounted for by the likelihood that thick POM materials (500 mm or thicker) do not achieve equilibrium (causing negative biases up to 1 log unit), or that certain POM extraction procedures do not ensure quantitative extraction (causing negative biases up to 2 log units). Temperature can also influence K POM , although all previous literature studies were carried out at room temperature. The present study found that K POM values at room temperature are independent (within 0.2 log units) of POM manufacture method, of thickness between 17 mm and 80 mm, and of salinity between 0% and 10%. Regarding kinetics, monochloro-to hexachloropolychlorinated biphenyls (PCBs) were within 0.2 log units of equilibrium after 28 d in the mixed system, but only dichloro-PCBs achieved near equilibrium after 126 d in the static system. Based on these insights, recommended methods and K POM values to facilitate interlaboratory reproducibility are presented. Environ Toxicol Chem 2015;34:710-720. # 2015 SETAC