Multi-metals Measured at Sediment–Water Interface (SWI) by Diffusive Gradients in Thin Films (DGT) Technique for Geochemical Research
详细信息    查看全文
  • 作者:Zhihao Wu ; Lixin Jiao ; Shengrui Wang
  • 刊名:Archives of Environmental Contamination and Toxicology
  • 出版年:2016
  • 出版时间:February 2016
  • 年:2016
  • 卷:70
  • 期:2
  • 页码:429-437
  • 全文大小:696 KB
  • 参考文献:Bender M, Martin W, Hess J, Sayles F, Ball L, Lambert C (1987) A whole core squeezer for interfacial pore-water sampling. Limnol Oceanogr 32:1214–1225CrossRef
    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 337–387CrossRef
    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 99–139CrossRef
    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 460:247–256CrossRef
    Davison W, Zhang H (1994) In situ speciation measurements of trace components in natural-waters using thin-film gels. Nature 367:546–548CrossRef
    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 24:1485–1504CrossRef
    Förstner U (2004) Traceability of sediment analysis. Trends Analytic Chem 23:217–236CrossRef
    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 43:1075–1090CrossRef
    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 158:2439–2445CrossRef
    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 21:912–914CrossRef
    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 177:111–128CrossRef
    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 22:814–832CrossRef
    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 57:213–233CrossRef
    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 64:282–291CrossRef
    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 46:3335–3342CrossRef
    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 533:193–202CrossRef
    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 55:1493–1500CrossRef
    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 328:275–286CrossRef
    Pempkowiak J, Sikora A, Biernacka E (1999) Speciation of heavy metals in marine sediments vs their bioaccumulation by mussels. Chemosphere 39:313–321CrossRef
    Pyzik AJ, Sommer SE (1981) Sedimentary iron monosulphides: kinetics and mechanism of formation. Geochim Cosmochim Acta 45:687–698CrossRef
    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 61:115–134CrossRef
    Santschi P, Hohener P, Benoit G, Buchholtzten-Brink M (1990) Chemical processes at the sediment-water interface. Mar Chem 30:269–315CrossRef
    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 106:192–207CrossRef
    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):1381–1389CrossRef
    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 225:2188–2204CrossRef
    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 59:4181–4192CrossRef
    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 32:704–710CrossRef
    Zhang H, Davison W, Mortimer RJG, Krom MD, Hayes PJ, Davies IM (2002) Localised remobilization of metals in a marine sediment. Sci Total Environ 296:175–187CrossRef
  • 作者单位:Zhihao Wu (1) (2)
    Lixin Jiao (1)
    Shengrui Wang (1)
    Yuanzhi Xu (1)

    1. State Key Laboratory of Environmental Criteria and Risk Assessment, State Environmental Protection Key Laboratory for Lake Pollution Control, Research Center of Lake Eco-environment, Chinese Research Academy of Environmental Sciences, Beijing, 100012, People’s Republic of China
    2. State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing, 100875, People’s Republic of China
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Environment
    Terrestrial Pollution
    Agriculture
    Ecology
    Forestry
    Environment
    Soil Science and Conservation
  • 出版者:Springer New York
  • ISSN:1432-0703
文摘
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. Electronic supplementary materialThe online version of this article (doi:10.​1007/​s00244-015-0184-1) contains supplementary material, which is available to authorized users.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700