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Title:Young water fractions in spring discharge
Authors:ID Seelig, Simon (Author)
ID Thalheim, Felix (Author)
ID Seelig, Magdalena (Author)
ID Töchterle, Paul (Author)
ID Vremec, Matevž (Author)
ID Masten, Martin (Author)
ID Brielmann, Heike (Author)
ID Eybl, Jutta (Author)
ID Winkler, Gerfried (Author)
Files:URL https://www.sciencedirect.com/science/article/pii/S0022169426003185?via%3Dihub
 
.pdf 1-s2.0-S0022169426003185-mmc1.pdf (3,53 MB)
MD5: 6D0B4EAE439112C276838282C6FB2750
 
Language:English
Work type:Unknown
Typology:1.01 - Original Scientific Article
Organization:UAMEU - Alma Mater Europaea University
Abstract:Transit time distributions are fundamental to hydrologic research and practice, providing insights into how catch ments store, transport, and release water and solutes. Mean transit time estimates, however, often suffer from significant aggregation errors in heterogeneous and nonstationary catchments. The young water fraction (Fyw) provides a robust alternative that directly reflects the proportion of recent precipitation in discharge and enables consistent comparison between catchments. While numerous studies have focused on estimating Fyw in rivers, little is known about its magnitude and variability in springs. To address this knowledge gap, this study quanti f ies Fyw in spring discharge from a diverse set of 469 springs in Austria. Across the dataset, Fyw is generally low and approximately log-normally distributed (mean 0.06), with variability among springs largely controlled by aquifer structure: karst springs display the highest fractions and greatest variability, talus springs intermediate values, and fracture and alluvial springs low fractions with limited variability. Evaluating the sensitivity of Fyw to discharge reveals distinct responses to hydrologic forcing: karst springs are most sensitive, reflecting tempo rary shifts in relative flow path contributions, whereas fracture springs are least sensitive, reflecting conservative f low dynamics. Drawing on a dataset of 565 rivers compiled for comparison, springs exhibit substantially lower Fyw, likely reflecting their predominantly slow subsurface flow paths. By analyzing Fyw across a large number of springs, this study delivers the first systematic insight into young water contributions to spring discharge, informing conceptual models, water resource management strategies, and contamination risk assessments.
Keywords:young water fraction, stable isotopes, spring discharge, transit time, alpine hydrology, comparative hydrology
Publication date:01.05.2026
Year of publishing:2026
Number of pages:15 str.
Numbering:Vol. 670, [article no.] ǂ135221
PID:20.500.12556/ReVIS-13349 New window
COBISS.SI-ID:272580355 New window
UDC:556.36
ISSN on article:1879-2707
DOI:10.1016/j.jhydrol.2026.135221 New window
Note:Nasl. z nasl. zaslona; Opis vira z dne 23. 3. 2026;
Publication date in ReVIS:23.03.2026
Views:29
Downloads:0
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Record is a part of a journal

Title:Journal of hydrology
Shortened title:J. hydrol.
Publisher:Elsevier
ISSN:1879-2707
COBISS.SI-ID:23155461 New window

Licences

License:CC BY 4.0, Creative Commons Attribution 4.0 International
Link:http://creativecommons.org/licenses/by/4.0/
Description:This is the standard Creative Commons license that gives others maximum freedom to do what they want with the work as long as they credit the author.

Secondary language

Language:Slovenian
Keywords:frakcija mlade vode, stabilni izotopi, izvirni pretok, čas prehoda, alpska hidrologija, primerjalna hidrologija


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