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

Research output: Contribution to journalArticleResearchpeer review

Authors

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

External Research Organisations

  • Federal Institute for Geosciences and Natural Resources (BGR)
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Details

Original languageEnglish
Pages (from-to)1253-1262
Number of pages10
JournalJournal of Environmental Quality
Volume41
Issue number4
Publication statusPublished - 1 Jul 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 subject areas

Sustainable Development Goals

Cite this

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, Vol. 41, No. 4, 01.07.2012, p. 1253-1262.

Research output: Contribution to journalArticleResearchpeer 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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