Variability in zinc tolerance, measured as incorporation of radio-labeled carbon dioxide and thymidine, in periphyton communities sampled from 15 European river stretches.

Fifteen European rivers and streams belonging to watersheds in Sweden, the Netherlands, and Spain respectively, were sampled by allowing periphyton to colonize submerged glass substrata. Their zinc tolerances were quantified in short-term laboratory tests, where inhibition of photosynthesis in microalgae and thymidine incorporation in bacterial DNA was measured, and expressed as EC50 values. The variability in zinc tolerances was high reaching 1.5-2.5 orders of magnitude, ranging from 25-8145 microM for photosynthesis and 15-467 microM for thymidine assays. Based on the observed variability, uncertainty factors were estimated for the extrapolation of zinc toxicity data from river to river, both regionally and interregionally. Under the assumption to protect 95% of the observed communities the regional uncertainty factors were 1.7-4.3 and the interregional 2.4-8.6. The sampling sites were characterized in terms of biotope physiography, water chemistry, periphyton biomass, trace element content, and species composition. Multivariate analysis of the data using PLS (Projection to Latent Structure), was used to generate hypotheses about the relation between periphyton zinc tolerance and the 123 so-called predictor variables. Zinc contamination, phosphate, nitrogen nutrients, pH, calcium, bicarbonate, dissolved organic carbon, and various diatom species are important predictors for zinc tolerance in the entire data set representing all 15 river stretches. Regional models suggested that very different factors determined the zinc tolerance in the Swedish and Dutch periphyton. The results are interpreted in terms of Pollution-Induced Community Tolerance (PICT) and the bioavailability of zinc.

Lead speciation in artificial human digestive fluid.

For children, soil ingestion via hand-to-mouth behavior can be a main route of exposure to contaminants such as lead. The ingested lead can be mobilized from the soil and form new species during the digestion process. Speciation is known to affect the availability of metals for transport across biological membranes. In the present study, in vitro digestions were performed with (artificially contaminated) standard soil. Lead speciation was investigated in the artificial human intestinal fluid, i.e., chyme, to gain insight into the lead species and lead fractions that may be available for transport across the intestinal epithelium. To that end, both a lead ion selective electrode (Pb-ISE) and a voltammetric technique (differential pulse anodic stripping voltammetry, DPASV) were used. The results indicate that in chyme only a negligible lead fraction is present as free Pb(2+), whereas lead phosphate and lead bile complexes are important fractions. The lead phosphate complexes appear to be voltammetrically labile, i.e., in dynamic equilibrium with Pb(2+). Labile complexes can dissociate and the produced metal ions can subsequently be transported across the intestinal epithelium. Lead bile complexes may behave in a similar manner, or this organometal complex may be able to traverse the intestinal membrane. Therefore, substantially more than only the free metal ion should be considered available for transport across the intestinal epithelium.

Dissolution kinetics of heavy metals in Dutch carbonate- and sulfide-rich freshwater sediments.

In two sulfide-rich freshwater sediments from the Biesbosch and Kromme Rijn River in the Netherlands differing in carbonate content and acid volatile sulfide (AVS) content, metal and sulfide dissolution kinetics were studied at different acid concentrations by varying both the procedure of acid addition and the extraction time. The establishment of equilibrium was monitored by measuring the pH in time, which reached a near constant value. The equilibrium pH was reached quickly when large amounts of acid were added and slowly when small amounts of acid were added. This observation was confirmed by the yield of extracted metals after either a 45-min or 24-h extraction over a pH range from 0 to 5. The pH factor seemed to be of more influence than time for the dissolution of metals. The amount of extracted metals was highly dependent on the metal itself due to its physico-chemical behavior. Although the sediments studied varied in carbonate content, acid volatile sulfide (AVS), and total metal content, the extracted fraction of metals compared with their total content in the sediment was similar for most metals. Finally, the AVS content as well as the ratio of simultaneously extracted metals (SEM; sum of Cd, Cu, Ni, Pb, and Zn) to AVS decreased with increasing pH. Because the SEM to AVS ratio may be used to set environmental quality criteria for the sediment compartment, this observation is of significance.