Abstract
Diffusive gradients in thin films (DGT) technique was used to determine pore water profile and to assess remobilization character of metals at sediment/water interface. The remobilization of Mn was due to redox reaction in profile, which engendered two large peaks: one with DGT concentration of 1355 µg L−1 at depth of −4.75 cm in sediment and the other with DGT concentration of 1040 µg L−1 at depth of −3.25 cm in sediment pore water. Fe reduction zone had a large peak of Fe (3209 µg L−1) at depth of −4.75 cm in sediment. Fe DGT-profile also indicated the little peaks and low values of dissolved Fe concentration in Fe-reduction/S-reduction boundary zone in sediment. Detailed correspondence of trace metals with Fe or Mn features in DGT-profiles suggested that their release is related to the reductive dissolution of Fe- or Mn-oxide.
Similar content being viewed by others
References
Bender M, Martin W, Hess J, Sayles F, Ball L, Lambert C (1987) A whole core squeezer for interfacial pore-water sampling. Limnol Oceanogr 32:1214–1225
Bowen H (1979) Environmental chemistry of the elements. Academic Press, London, p 333
Canfield DE, Raiswell R (1991) Pyrite formation and fossil preservation. In: Allison PA, Briggs DEG (eds) Taphonomy: Releasing the data locked in the Fossil record. Plenum Press, New York, pp 337–387
Claypool GE, Kaplan IR (1974) In: Kaplan IR (ed) The origin and distribution of methane in marine sediments: Natural gases in marine sediments. Plenum, New York, pp 99–139
Dahlqvist R, Zhang H, Ingri J, Davison W (2002) Performance of the diffusive gradients in thin films technique for measuring Ca and Mg in freshwater. Anal Chim Acta 460:247–256
Davison W, Zhang H (1994) In situ speciation measurements of trace components in natural-waters using thin-film gels. Nature 367:546–548
Fones GR, Davison W, Hamilton-Taylor J (2004) The fine-scale remobilization of metals in the surface sediment of the North-East Atlantic. Continental Shelf Res 24:1485–1504
Förstner U (2004) Traceability of sediment analysis. Trends Analytic Chem 23:217–236
Froelich PN, Klinkhammer GP, Bender ML, Luedtke NA, Heath GR, Cullen D, Dauphin P (1979) Early oxidation of organic matter in pelagic sediments of the eastern equatorial Atlantic: suboxic diagenesis. Geochim Cosmochim Acta 43:1075–1090
Gao Y, Baeyens W, De Galan S, Poffijn A, Leermakers M (2010) Mobility of radium and trace metals in sediments of the Winterbeek: application of sequential extraction and DGT techniques. Environ Poll 158:2439–2445
Hamilton-Taylor J, Davison W (1985) Redox-driven cycling of trace elements in lakes: Physics and Chemistry of Lakes. In: Lerman A, et al. (eds), Springer, pp 217–263
Hesslein RH (1976) An in situ sampler for close interval pore water studies. Limnol Oceanogr 21:912–914
Hyacinthe C, Anschultz P, Carbonel P, Jouanneau JM, Jorissen FJ (2001) Early diagenetic processes in the muddy sediments of the Bay of Biscay. Marine Geol 177:111–128
Jacobsen ST (1992) Chemical reaction and air change during the decomposition of organic matter. Res Conserv Recycl 6:529–539
Jorgensen BB (1977) The sulphur cycle of a coastal marine sediment (Limfjorden, Denmark). Limnol Oceanogr 22:814–832
Kress N, Herut B, Galil BS (2004) Sewage sludge impact on sediment quality and benthic assemblages off the Mediterranean coast of Israel—a long-term study. Mar Environ Res 57:213–233
Krom MD, Mortimer RJG, Hayes SWP, Davies IM, Davison W, Zhang H (2002) In situ determination of dissolved iron production in recent marine sediments. Aquatic Sci 64:282–291
Levy JL, Zhang H, Davison W, Galceran J, Puy J (2012) Kinetic signatures of metals in the presence of Suwannee river fluvic acid. Environ Sci Technol 46:3335–3342
Li WJ, Zhao HJ, Teasdale PR, Jonh R, Wang FY (2005) Metal speciation measurement by diffusive gradients in thin films technique with different binding phases. Anal Chim Acta 533:193–202
Lin J, Liu CQ, Zhu ZZ (2008) Historical eutrophication in Lake Taihu: evidence from biogenic silica and total phosphorus accumulation in sediments from northern part of Lake Taihu. Environ Geol 55:1493–1500
Myers CR, Nealson KH (1993) Biological and chemical mechanisms of manganese reduction in aquatic and sediment systems: Transport and transformation of contaminations near the sediment-water interface. In: DePinto, JV, Lick W, Paul JF (eds), Lewis, pp 205–223
Naylor C, Davison W, Motelica-Heino M, Van den Berg GA, Van der Heijdt LM (2004) Simultaneous release of sulfide with Fe, Mn, Ni and Zn in marine harbor sediment measured using a combined metal/sulfide DGT probe. Sci Total Environ 328:275–286
Pempkowiak J, Sikora A, Biernacka E (1999) Speciation of heavy metals in marine sediments vs their bioaccumulation by mussels. Chemosphere 39:313–321
Pyzik AJ, Sommer SE (1981) Sedimentary iron monosulphides: kinetics and mechanism of formation. Geochim Cosmochim Acta 45:687–698
Rickard D (1997) Kinetics of pyrite formation by the H2S oxidation of iron(II) monosulfide in aqueous solutions between 25 and 125 °C: the rate equation. Geochim Cosmochim Acta 61:115–134
Santschi P, Hohener P, Benoit G, Buchholtzten-Brink M (1990) Chemical processes at the sediment-water interface. Mar Chem 30:269–315
Shpard FP (1954) Nomenclature based on sand-silt-clay ratios. J Sed Petrol 24:151–158
Tankere-Muller S, Zhang H, Davison W, Finke N, Larsen O, Stahl H, Glud RN (2007) Fine scale remobilisation of Fe, Mn Co, Ni, Cu and Cd in contaminated marine sediment. Mar Chem 106:192–207
Tessier A (1992) Sorption of trace elements on natural particles in toxic environments: environmental particles. In: Buffle J, van Leeuwen HP (eds), Lewis, pp 425–453
The specification for marine monitoring, 2008. GB 17378.5-2007, The 5th part: Deposit analysis. Beijing, p 104
Vershinn AV, Rozanov AG (1982) On the problem of Eh measurement by the Pt electrode and estimation of oxdition-reduction conditions in marine media. Geokbimiya 1:121–128
Watson PG, Frickers TE (1990) A multilevel, in situ pore water sampler for use in intertidal sediments and laboratory microcosms. Limnol Oceanogr 35(6):1381–1389
Wu ZH (2011) Metal pollution in surficial sediment of Liaodong bay and estuary in Yingkou and transference character at the sediment/water interface. Ph.D. Thesis, Beijing Normal University, Beijing
Wu ZH, Wang SR, Jiao LX, Wu FC (2014) The simultaneous measurement of phosphorus, sulfide and trace metals by ferrihydrite/AgI/chelex-100 DGT (diffusive gradients in thin films) probe at sediment/water interface (SWI) and remobilization assessment. Water Air Soil Poll 225:2188–2204
Wu ZH, Wang SR, Jiao LX (2015) Geochemical behavior of metals-sulfide-phosphorus at SWI (sediment/water interface) assessed by DGT (diffusive gradients in thin films) probes. J Geochem Explor. doi:10.1016/j.gexplo.2015.05.005
Zhang H, Davison W, Miller S, Tych W (1995) In situ high resolution measurements of fluxes of Ni, Cu, Fe, and Mn and concentrations of Zn and Cd in pore waters by DGT. Geochim Cosmochim Acta 59:4181–4192
Zhang H, Davison W, Knight B, McGrath S (1998) In situ measurement of solution concentrations and fluxes of trace metals in soils using DGT. Environ Sci Technol 32:704–710
Zhang H, Davison W, Mortimer RJG, Krom MD, Hayes PJ, Davies IM (2002) Localised remobilization of metals in a marine sediment. Sci Total Environ 296:175–187
Acknowledgments
The research was financially supported by the Major Science and Technology Program for Water Pollution Control and Treatment (2012ZX07202002), the National Key Basic Research and Development Plan of China (973 Program, 2004CB418502), and China Postdoctoral Science Foundation (2013M541002).
Author information
Authors and Affiliations
Corresponding author
Electronic supplementary material
Below is the link to the electronic supplementary material.
Rights and permissions
About this article
Cite this article
Wu, Z., Jiao, L., Wang, S. et al. Multi-metals Measured at Sediment–Water Interface (SWI) by Diffusive Gradients in Thin Films (DGT) Technique for Geochemical Research. Arch Environ Contam Toxicol 70, 429–437 (2016). https://doi.org/10.1007/s00244-015-0184-1
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00244-015-0184-1