Integrated Monitoring of Particle-Associated
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Integrated monitoring of par/cle-associated transport of persistent organic pollutants (PAHs as case study) in contras/ng catchments in Southwest Germany Barbara Beckingham 1,2 *, Peter Grathwohl 1,2 , Hermann Rügner 2, Marc Schwientek 2, Bertram Kuch 2,3 1 Center for Applied Geoscience, University of Tübingen; 2 Water Earth System Science (WESS) Cluster, Tübingen, Germany; 3 ISWA, University of Stuttgart, Stuttgart, Germany * Currently at College of Charleston, Charleston, SC Introduction Results 1000 10 2 Strongly sorbing hydrophobic pollutants such as polycylic aromatic hydrocarbons Ammer (R = 0.96) 2 2 Körsch (R = 0.97) ) Echaz (R = 1.0) 2 (PAHs) are primarily subjected to particle-associated transport and thus are -1 Neckar (R = 0.80) Steinlach (R 2 = 0.93) g l 2 µ 1 2 Ammer springs (R = 0.92) mobilized especially during high flow conditions when soils and sediments undergo 100 Goldersbach (R = 0.62) erosion and urban runoff is intensified. Whereas soil pollutants reach rivers only ) slowly by erosion, untreated surface runoff from sealed urban space and -1 PAH15 ( PAH15 0.1 1,2 stormwater releases are major immediate sources of particle bound pollutants. 10 W,tot Chemical loads to rivers in general may increase with increasing population C Ammer 0.01 density or urban development of watersheds due to abundance of sources and Echaz TSS (mg l (mg TSS impervious surface.3-5 Given the scope of anthropogenic impact, integrated and 1 Neckar Steinlach 0.001 cost-effective strategies for contaminant monitoring in catchments are needed.6 Ammer Springs 1 10 100 1000 1 10 100 1000 Goldersbach TSS (mg l-1) TSS (mg l-1) 0.1 Hypothesis 10 0.1 1 10 100 1000 2 Ammer (R 2 = 0.76) Echaz (R = 0.99) 2 Transport of PAHs is dominated by urban particles (loaded with PAH concentration turbidity (FNU) ) 2 Steinlach (R = 0.84) -1 Neckar (R = 0.79) 2 2 C ) compared to less polluted background particles. PAH concentrations on g l 1 Goldersbach (R = 0.66) Ammer springs (R = 0.75) sus,u Figure 2. TSS and turbidity are well correlated µ suspended solids (Csus) are expected to be proportional to catchment population across all catchments investigated. (Inh) per mass flux of suspended particles (MTSS). 0.1 Figure 3. From linear regressions of total PAHs ( PAH15 W,tot in water vs. particle load (TSS or turbidity) C 0.01 suspended solids PAHs (Csus) are calculated. These are different in different catchments. Sampling Campaigns 0.001 0.1 1 10 100 1000 0.1 1 10 100 1000 - Monthly water samples were collected in 2009 – 2011 at approx. 40 locations turbidity (NTU) turbidity (NTU) within 5 catchments in southern Germany - Turbidity, unfiltered water PAH concentrations, dissolved organic carbon (DOC) and total suspended solids (TSS; only during 4 sampling events) were measured. - Discharge was obtained from gauging stations near catchment outlets. - Total sediment PAH concentrations at 35 locations in the Goldersbach and in the Ammer (main stem, tributaries) were measured in 2010. Figure 1. Selected catchments: similar geography/climate but different land use. Figure 4. Suspended solids PAHs increase with Figure 5. Springs and tributaries without impact of sewer overflows/waste the number of inhabitants per unit of TSS flux for water treatment plants typically have lower sediment PAH concentrations. catchments. Conclusions - Strong linear correlations between total PAHs in water and suspended solid loads indicate predominance of particle-facilitated transport in catchments. - The degree of urban pressure in catchments influences the loading of hydrophobic contaminants like PAHs. This relationship should be tested in catchments with more varied land use, geology and climate characteristics. - TSS correlation with turbidity highlights a convenient measure for assessing particle associated fluxes of pollutants with high temporal/spatial resolution. Contact References WESS Partners Acknowledgements * Dr. Barbara Beckingham 1. Menzie et al. 2002. Estuaries. 25, 165-176. This work was supported by a grant from the Ministry of College of Charleston 2. Foster et al. 2000. Appl. Geochem. 15, 901-905. Science, Research and Arts of Baden-Württemberg (AZ Zu Department of Geology & Environmental Geosciences 3. Barber et al. 2006. Environ. Sci. Technol. 40, 475-486. 33-721.3-2) and the Helmholtz Center for Environmental 202 Calhoun St. Charleston, SC 29401 4. Kannan et al. 2005. Environ. Sci. Technol. 39, 4700-4706. Research, Leipzig (UFZ). [email protected] 5. Chalmers et al. 2007. J. Contam. Hydrol. 91, 4-25. 6. Schwientek et al. 2013. Environ. Poll. 172, 155-162. .