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Disturbances to metal partitioning during toxicity testing of iron(II)‐rich estuarine pore waters and whole sediments

Metal partitioning is altered when suboxic estuarine sediments containing Fe(II)‐rich pore waters are disturbed during collection, preparation, and toxicity testing. Experiments with model Fe(II)‐rich pore waters demonstrated the rates at which adsorptive losses of Cd, Cu, Ni, Mn, Pb, and Zn occur upon exposure to air. Experiments with Zn‐contaminated estuarine sediments demonstrated large and often unpredictable changes to metal partitioning during sediment storage, removal of organisms, and homogenization before testing. Small modifications to conditions, such as aeration of overlying waters, caused large changes to the metal partitioning. Disturbances caused by sediment collection required many weeks for reestablishment of equilibrium. Bioturbation by benthic organisms led to oxidation of pore‐water Fe(II) and lower Zn fluxes because of the formation of Fe hydroxide precipitates that adsorb pore‐water Zn. For five weeks after the addition of organisms to sediments, Zn fluxes increased slowly as the organisms established themselves in the sediments, indicating that the establishment of equilibrium was not rapid. The results are discussed in terms of the dynamic nature of suboxic, Fe(II)‐rich estuarine sediments, how organisms perturb their environment, and the importance of understanding chemistry in toxicity testing with whole sediments or pore water. Recommendations are provided for the handling of sediments for toxicity testing.