Kinetic processes and stable isotopes in cave dripwaters as indicators of winter severity

Ersek, Vasile, Onac, Bogdan and Persoiu, Aurel (2018) Kinetic processes and stable isotopes in cave dripwaters as indicators of winter severity. Hydrological Processes, 32 (18). pp. 2856-2862. ISSN 0885-6087

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Official URL: https://doi.org/10.1002/hyp.13231

Abstract

We examine how the stable isotope composition of meteoric water is transmitted through soil and epikarst to dripwaters in a cave in western Romania. δ2H and δ18O in precipitation at this site are influenced by temperature and moisture source conditions (Atlantic and Mediterranean), with lower δ18O in winter and higher in summer. The stable isotope composition of cave dripwaters mimics this seasonal pattern of low and high δ18O, but the onset and end of freezing conditions in the winter season are marked by sharp transitions in the isotopic signature of cave dripwaters of approximately 1‰. We interpret these shifts as the result of kinetic isotopic fractionation during the transition phase from water to ice at the onset of freezing conditions, and the input of meltwater to the cave at the beginning of the spring season. This process is captured in dripwaters and therefore speleothems from Urșilor Cave which grew under such dripping points, may have the potential to record past changes in the severity of winters. Similar isotopic changes in dripwaters driven by freeze-thaw processes can affect other caves in areas with winter snowcover, and cave monitoring during such changes is essential in linking the isotopic variability in dripwaters and speleothems to surface climate.

Item Type: Article
Uncontrolled Keywords: cave, dripwaters, stable isotopes, karst, winter climate, precipitation
Subjects: F800 Physical and Terrestrial Geographical and Environmental Sciences
Department: Faculties > Engineering and Environment > Geography and Environmental Sciences
Depositing User: Paul Burns
Date Deposited: 25 Jun 2018 10:49
Last Modified: 05 Sep 2018 18:45
URI: http://nrl.northumbria.ac.uk/id/eprint/34668

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