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1000 Titel
  • Fate of nitrate during groundwater recharge in a fractured karst aquifer in Southwest Germany
1000 Titelzusatz
  • Destino del nitrato cuando se recarga el agua subterránea en un acuífero kárstico fracturado en el suroeste de Alemania
  • 德国西南部裂隙岩溶含水层地下水补给过程中的硝酸盐归宿
  • Devenir des nitrates lors de la recharge en eau souterraine d’un aquifère karstique fracturé dans le Sud-Ouest de l’Allemagne
  • Destino do nitrato durante recarga de águas subterrâneas em um aquífero cárstico fissural no sudoeste da Alemanha
1000 Autor/in
  1. Visser, Anna-Neva |
  2. Lehmann, Moritz F. |
  3. Rügner, Hermann |
  4. D’Affonseca, Fernando Mazo |
  5. Grathwohl, Peter |
  6. Blackwell, Nia |
  7. Kappler, Andreas |
  8. Osenbrück, Karsten |
1000 Erscheinungsjahr 2021
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2021-02-18
1000 Erschienen in
1000 Quellenangabe
  • 29(3):1153-1171
1000 Copyrightjahr
  • 2021
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.1007/s10040-021-02314-2 |
1000 Publikationsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • Over the past decades, fractured and karst groundwater systems have been studied intensively due to their high vulnerability to nitrate (NO₃⁻) contamination, yet nitrogen (N) turnover processes within the recharge area are still poorly understood. This study investigated the role of the karstified recharge area in NO₃⁻ transfer and turnover by combining isotopic analysis of NO₃⁻ and nitrite (NO₂⁻) with time series data of hydraulic heads and specific electrical conductivity from groundwater monitoring wells and a karstic spring in Germany. A large spatial variability of groundwater NO₃⁻ concentrations (0.1–0.8 mM) was observed, which cannot be explained solely by agricultural land use. Natural-abundance N and O isotope measurements of NO₃⁻ (δ¹⁵N and δ¹⁸O) confirm that NO₃⁻ derives mainly from manure or fertilizer applications. Fractional N elimination by denitrification is indicated by relatively high δ¹⁵N- and δ¹⁸O-NO₃⁻ values, elevated NO₂⁻ concentrations (0.05–0.14 mM), and δ¹⁵N-NO₂⁻ values that were systematically lower than the corresponding values of δ¹⁵N-NO₃⁻. Hydraulic and chemical response patterns of groundwater wells suggest that rain events result in the displacement of water from transient storage compartments such as the epikarst or the fissure network of the phreatic zone. Although O₂ levels of the investigated groundwaters were close to saturation, local denitrification might be promoted in microoxic or anoxic niches formed in the ferrous iron-bearing carbonate rock formations. The results revealed that (temporarily) saturated fissure networks in the phreatic zone and the epikarst may play an important role in N turnover during the recharge of fractured aquifers.
1000 Sacherschließung
lokal Groundwater recharge
lokal Germany
lokal Karst
lokal Nitrate
lokal Report
lokal Stable isotopes
1000 Liste der Beteiligten
  1. https://orcid.org/0000-0002-8447-5825|https://frl.publisso.de/adhoc/uri/TGVobWFubiwgTW9yaXR6IEYu|https://frl.publisso.de/adhoc/uri/UsO8Z25lciwgSGVybWFubg==|https://frl.publisso.de/adhoc/uri/ROKAmUFmZm9uc2VjYSwgRmVybmFuZG8gTWF6bw==|https://frl.publisso.de/adhoc/uri/R3JhdGh3b2hsLCBQZXRlcg==|https://frl.publisso.de/adhoc/uri/QmxhY2t3ZWxsLCBOaWE=|https://frl.publisso.de/adhoc/uri/S2FwcGxlciwgQW5kcmVhcw==|https://frl.publisso.de/adhoc/uri/T3NlbmJyw7xjaywgS2Fyc3Rlbg==
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1000 Erstellt am 2023-04-28T12:59:24.925+0200
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1000 Zuletzt bearbeitet 2023-10-20T18:11:51.033+0200
1000 Objekt bearb. Fri Oct 20 18:11:51 CEST 2023
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