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Water supply in times of climate change—Tracer tests to identify the catchment area of an Alpine karst spring, Tyrol, Austria

Schäffer, R. ; Sass, I. ; Heldmann, C.-D. (2020)
Water supply in times of climate change—Tracer tests to identify the catchment area of an Alpine karst spring, Tyrol, Austria.
In: Arctic, Antarctic, and Alpine Research, 52 (1)
doi: 10.1080/15230430.2020.1723853
Artikel, Bibliographie

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Kurzbeschreibung (Abstract)

Climate change and glacial retreat are changing the runoff behavior of Alpine springs and streams. For example, in the extremely dry and hot summer of 2018, many springs used for drinking water supply lost up to 50 percent of their average discharge; a few springs have even run dry. In order to ensure drinking water supply in the future, springs featuring large and constantly sufficient discharge rates will have to be identified and tapped. A case study was undertaken at the Tuxbachquelle because catchment area and temporal variation of physicochemical and hydrochemical properties were previously unknown. Tracer tests with uranine proved a hydraulic connection between this karst spring and a stream a few kilometers uphill. At low runoff, uranine needed about 4½ hours from the sink to the spring, whereas at high runoff more than four days was required. It became evident that discharge, electrical conductivity, temperature, and turbidity of the Tuxbachquelle respond within a few hours to precipitation events. The water quality and an examination of the water balance resulted in a significantly larger catchment area. It is assumed that widely karstified calcite marble subterraneously drains a considerable part of the Tuxertal (Tux Valley), including some active rock glaciers.

Typ des Eintrags: Artikel
Erschienen: 2020
Autor(en): Schäffer, R. ; Sass, I. ; Heldmann, C.-D.
Art des Eintrags: Bibliographie
Titel: Water supply in times of climate change—Tracer tests to identify the catchment area of an Alpine karst spring, Tyrol, Austria
Sprache: Englisch
Publikationsjahr: März 2020
Verlag: Taylor & Francis
Titel der Zeitschrift, Zeitung oder Schriftenreihe: Arctic, Antarctic, and Alpine Research
Jahrgang/Volume einer Zeitschrift: 52
(Heft-)Nummer: 1
DOI: 10.1080/15230430.2020.1723853
URL / URN: https://www.tandfonline.com/doi/full/10.1080/15230430.2020.1...
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Kurzbeschreibung (Abstract):

Climate change and glacial retreat are changing the runoff behavior of Alpine springs and streams. For example, in the extremely dry and hot summer of 2018, many springs used for drinking water supply lost up to 50 percent of their average discharge; a few springs have even run dry. In order to ensure drinking water supply in the future, springs featuring large and constantly sufficient discharge rates will have to be identified and tapped. A case study was undertaken at the Tuxbachquelle because catchment area and temporal variation of physicochemical and hydrochemical properties were previously unknown. Tracer tests with uranine proved a hydraulic connection between this karst spring and a stream a few kilometers uphill. At low runoff, uranine needed about 4½ hours from the sink to the spring, whereas at high runoff more than four days was required. It became evident that discharge, electrical conductivity, temperature, and turbidity of the Tuxbachquelle respond within a few hours to precipitation events. The water quality and an examination of the water balance resulted in a significantly larger catchment area. It is assumed that widely karstified calcite marble subterraneously drains a considerable part of the Tuxertal (Tux Valley), including some active rock glaciers.

Freie Schlagworte: Uranine; karst; discharge/runoff; rock glaciers; Hochstegen Formation
Fachbereich(e)/-gebiet(e): 11 Fachbereich Material- und Geowissenschaften
11 Fachbereich Material- und Geowissenschaften > Geowissenschaften
11 Fachbereich Material- und Geowissenschaften > Geowissenschaften > Fachgebiet Angewandte Geothermie
Hinterlegungsdatum: 12 Mär 2020 06:39
Letzte Änderung: 03 Jul 2024 02:43
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