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Status: Bibliographieeintrag

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Verfasst von:Broers, Hans Peter [VerfasserIn]   i
 Sültenfuß, Jürgen [VerfasserIn]   i
 Aeschbach, Werner [VerfasserIn]   i
 Kersting, Arne [VerfasserIn]   i
 Menkovich, Armin [VerfasserIn]   i
 de Weert, Jasperien [VerfasserIn]   i
 Castelijns, Jeroen [VerfasserIn]   i
Titel:Paleoclimate signals and groundwater age distributions from 39 public water works in the Netherlands
Titelzusatz:insights from noble gases and carbon, hydrogen and oxygen isotope tracers
Verf.angabe:Hans Peter Broers, Jürgen Sültenfuß, Werner Aeschbach, Arne Kersting, Armin Menkovich, Jasperien de Weert, and Jeroen Castelijns
E-Jahr:2021
Jahr:27 June 2021
Umfang:26 S.
Teil:volume:57
 year:2021
 number:7
 month:07
 elocationid:e2020WR029058
 pages:1-26
 extent:26
Fussnoten:Gesehen am 25.09.2021
Titel Quelle:Enthalten in: Water resources research
Ort Quelle:[New York] : Wiley, 1965
Jahr Quelle:2021
Band/Heft Quelle:57(2021), 7 vom: Juli, Artikel-ID e2020WR029058, Seite 1-26
ISSN Quelle:1944-7973
Abstract:Knowing the age distribution of water abstracted from public water supply wells helps to ensure customer trust in drinking water sources and underpin predictions of water quality evolution. We sampled the mixed water of 39 large public supply well fields for major ion chemistry, 3H, 3He, 18O, 2H, 14CDIC, 13CDIC and noble gases and determined the Noble Gas Temperature (NGT). We used a discrete travel time distribution model to quantify the age distributions using 3H, 4He, 14C apparent age and NGT as the 4 distinctive tracers. Helium-4 and NGT provided information on the older part of the age distributions and showed that the 14C apparent ages are often the result of mixing of waters ranging between 2,000 and 35,000 years old, instead of being discrete ages with a limited variance as previously assumed. The results reveal a large range of age distributions, comprising vulnerable well fields with >60% young water (<100 years) and well fields with >30% paleo groundwater (>25,000 years) and all forms of intermediate distributions. The age distributions match the hydrogeological setting; well fields with age distributions skewed towards older ages appear in the Roer Valley Graben structure, where fluvial and marine aquitards and sealed faults provide protection from recent recharge. Waters from this graben exhibit paleoclimate signals, with a clear relation between NGT (range 3.2-9.3 °C), 4He (up to 3.3 × 10−6 ccSTP/g) and δ18O (range −8.5‰ to −5.9‰VSMOW). Moreover, 3He/4He ratios of these graben waters suggest a certain influx of He from mantle origin.
DOI:doi:10.1029/2020WR029058
URL:Bitte beachten Sie: Dies ist ein Bibliographieeintrag. Ein Volltextzugriff für Mitglieder der Universität besteht hier nur, falls für die entsprechende Zeitschrift/den entsprechenden Sammelband ein Abonnement besteht oder es sich um einen OpenAccess-Titel handelt.

Volltext ; Verlag: https://doi.org/10.1029/2020WR029058
 Volltext: https://onlinelibrary.wiley.com/doi/abs/10.1029/2020WR029058
 DOI: https://doi.org/10.1029/2020WR029058
Datenträger:Online-Ressource
Sprache:eng
Sach-SW:3He/4He ratio
 4-helium
 age distribution
 carbon-14
 graben structure
 groundwater age
 noble gas temperature
 noble gases
 public supply wells
 travel time distribution
 tritium-helium
K10plus-PPN:1771802480
Verknüpfungen:→ Zeitschrift

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