Application of Groundwater Thresholds for Trace Elements on Percolation Water: A Case Study on Percolation Water from Northern German Lowlands

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Autoren

  • L. Godbersen
  • W. H.M. Duijnisveld
  • J. Utermann
  • H. E. Gäbler
  • G. Kuhnt
  • J. Böttcher

Externe Organisationen

  • Bundesanstalt für Geowissenschaften und Rohstoffe (BGR)
Forschungs-netzwerk anzeigen

Details

OriginalspracheEnglisch
Seiten (von - bis)1253-1262
Seitenumfang10
FachzeitschriftJournal of Environmental Quality
Jahrgang41
Ausgabenummer4
PublikationsstatusVeröffentlicht - 1 Juli 2012

Abstract

The German insignifi cance thresholds (GFS) for groundwater, derived with an added risk approach, will soon be adopted as trigger values for percolation water entering groundwater. Th e physicochemical properties of the vadose zone diff er considerably from those of groundwater, which may lead to diffi culties in the applicability of groundwater-derived GFS to percolation water. To test the applicability of the GFS to percolation water regarding the concentration level and the fi eld-scale variability, 46 sites in Northern Germany were sampled, including arable land, grassland, and forest, situated on three spatially dominant parent materials: sand, glacial loam, and loess. Concentrations of As, Ba, Cd, Co, Cr, Cu, Mo, Ni, Pb, Sb, Sn, V, Zn, and F were analyzed in percolation water from the transition between the unsaturated to the saturated zone. We compared median and 90th percentile values of the background concentrations with the GFS. In more than 10% of all samples, background concentrations of Cd, Co, Ni, V, or Zn exceeded the GFS. We evaluated the applicability of the GFS on fi eld-scale medians of background concentrations taking fi eld-scale interquartile distance and the bootstrap percentile confi dence interval of the fi eld scale median of trace element background concentrations into consideration. Statements about exceedance or nonexceedance of GFS values could only be made with acceptable statistical uncertainty (α ≤ 0.1) when operational median concentrations were about one third higher or lower than the corresponding GFS.

ASJC Scopus Sachgebiete

Ziele für nachhaltige Entwicklung

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Application of Groundwater Thresholds for Trace Elements on Percolation Water: A Case Study on Percolation Water from Northern German Lowlands. / Godbersen, L.; Duijnisveld, W. H.M.; Utermann, J. et al.
in: Journal of Environmental Quality, Jahrgang 41, Nr. 4, 01.07.2012, S. 1253-1262.

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Godbersen L, Duijnisveld WHM, Utermann J, Gäbler HE, Kuhnt G, Böttcher J. Application of Groundwater Thresholds for Trace Elements on Percolation Water: A Case Study on Percolation Water from Northern German Lowlands. Journal of Environmental Quality. 2012 Jul 1;41(4):1253-1262. doi: 10.2134/jeq2011.0218
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abstract = "The German insignifi cance thresholds (GFS) for groundwater, derived with an added risk approach, will soon be adopted as trigger values for percolation water entering groundwater. Th e physicochemical properties of the vadose zone diff er considerably from those of groundwater, which may lead to diffi culties in the applicability of groundwater-derived GFS to percolation water. To test the applicability of the GFS to percolation water regarding the concentration level and the fi eld-scale variability, 46 sites in Northern Germany were sampled, including arable land, grassland, and forest, situated on three spatially dominant parent materials: sand, glacial loam, and loess. Concentrations of As, Ba, Cd, Co, Cr, Cu, Mo, Ni, Pb, Sb, Sn, V, Zn, and F were analyzed in percolation water from the transition between the unsaturated to the saturated zone. We compared median and 90th percentile values of the background concentrations with the GFS. In more than 10% of all samples, background concentrations of Cd, Co, Ni, V, or Zn exceeded the GFS. We evaluated the applicability of the GFS on fi eld-scale medians of background concentrations taking fi eld-scale interquartile distance and the bootstrap percentile confi dence interval of the fi eld scale median of trace element background concentrations into consideration. Statements about exceedance or nonexceedance of GFS values could only be made with acceptable statistical uncertainty (α ≤ 0.1) when operational median concentrations were about one third higher or lower than the corresponding GFS.",
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AU - Godbersen, L.

AU - Duijnisveld, W. H.M.

AU - Utermann, J.

AU - Gäbler, H. E.

AU - Kuhnt, G.

AU - Böttcher, J.

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