Fate of 137Cs, 90Sr and 239+240Pu in soil profiles at a water recharge site in Basel, Switzerland

Johannes Abraham, Katrin Meusburger, Judith Kobler Waldis, Michael E Ketterer, Markus Zehringer

Research output: Contribution to journalArticle

4 Citations (Scopus)

Abstract

An important process in the production of drinking water is the recharge of the withdrawn ground water with river water at protected recharge fields. While it is well known that undisturbed soils are efficiently filtering and adsorbing radionuclides, the goal of this study was to investigate their behaviour in an artificial recharge site that may receive rapid and additional input of radionuclides by river water (particularly when draining a catchment including nuclear power plants (NPP)). Soil profiles of recharge sites were drilled and analysed for radionuclides, specifically radiocesium (137Cs), radiostrontium (90Sr) and plutonium (239+240Pu). The distribution of the analysed radionuclides were compared with an uncultivated reference soil outside the recharge site. The main activity of 137Cs was located in the top soil (4.5–7.5 cm) and reached down to a depth of 84 cm and 48 cm for the recharge and the reference site, respectively. The found activities of 239+240Pu originate from the global fallout after 1950. 239+240Pu appeared to be strongly adsorbed onto soil particles. The shape of the depth profile was similar to 137Cs, but also similar between the recharge and the reference site. In contrast, 90Sr showed a uniform distribution over the entire depth of the recharge and reference profiles indicating that 90Sr already entered the gravel zone and the ground water. Elevated inventories of the radionuclides were observed for the recharge site. The soil of the recharge field exhibited a threefold higher activity of 137Cs compared to the reference soil. Also for 239+240Pu higher inventories where observed for the recharge sites (40%). 90Sr behaved differently, showing similar inventories between reference and recharge site. We estimate that 75–89% of the total inventory of 137Cs in the soil at the recharge site (7.000 Bq/m2) originated from the fallout of the Chernobyl accident and from emissions of Swiss NPPs. This estimate is based on the actual activity ratio of 137Cs/239+240Pu of 22 for global fallout. The investigations identified radiostrontium as potential threat to the ground water.

Original languageEnglish (US)
Pages (from-to)85-94
Number of pages10
JournalJournal of Environmental Radioactivity
Volume182
DOIs
StatePublished - Feb 1 2018
Externally publishedYes

Fingerprint

Switzerland
soil profile
recharge
Soil
Soils
Radioisotopes
Water
Fallout
Groundwater
radionuclide
Equipment and Supplies
water
fallout
Rivers
soil
Nuclear Power Plants
Plutonium
groundwater
river water
Gravel

Keywords

  • Cesium-137
  • Chernobyl
  • Global fallout
  • NPP accidents
  • Plutonium
  • Strontium-90
  • Surface groundwater recharge

ASJC Scopus subject areas

  • Environmental Chemistry
  • Waste Management and Disposal
  • Pollution
  • Health, Toxicology and Mutagenesis

Cite this

Fate of 137Cs, 90Sr and 239+240Pu in soil profiles at a water recharge site in Basel, Switzerland. / Abraham, Johannes; Meusburger, Katrin; Waldis, Judith Kobler; Ketterer, Michael E; Zehringer, Markus.

In: Journal of Environmental Radioactivity, Vol. 182, 01.02.2018, p. 85-94.

Research output: Contribution to journalArticle

Abraham, Johannes ; Meusburger, Katrin ; Waldis, Judith Kobler ; Ketterer, Michael E ; Zehringer, Markus. / Fate of 137Cs, 90Sr and 239+240Pu in soil profiles at a water recharge site in Basel, Switzerland. In: Journal of Environmental Radioactivity. 2018 ; Vol. 182. pp. 85-94.
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