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On the value of hydrochemical data for the interpretation of flow and transport processes in karst systems
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| Created: | Sep 13, 2023 at 1:04 p.m. (UTC) | |
| Last updated: | Sep 14, 2023 at 8:35 a.m. (UTC) | |
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| Sharing Status: | Public |
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Abstract
This study presents the development of LuKARS 2.0 on an hourly scale. The model concept was modified in comparison to the original model from Bittner et al. (2018) by considering the interaction between matrix and conduit as well as possible surface water bypassing the spring. This allows a flexible conceptualization of binary karst systems characterized by a perennial spring and intermittent overflow. The aim of this study is to investigate the relevance of high-resolution hydrochemical data for the verification and selection of conceptual event-based karst models. The model was tested on the Baget karst system, France, whose recharge area shows the coexistence of karst and non-karst formations. The results of this study shows that despite different model parametrizations simulate the discharge at the spring with comparable accuracy, not all of them match the observed hydrochemical data.
Bittner, D., Narany, T. S., Kohl, B., Disse, M., and Chiogna, G. (2018). Modeling the hydrological impact of land use change in a dolomite-dominated karst system. Journal of Hydrology, 567, 267–279. https://doi.org/10.1016/j.jhydrol.2018.10.017
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Temporal
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Content
README.txt
Discharge_Precipitation.txt contains: - Hourly precipitation (mm) from the Antican station for the period 1/3/2022 - 30/4/2022 - Hourly discahrge (m3/s) observed at the Las Hountas spring for the period 1/3/2022 - 30/4/2022 Chemical_data.txt contains: - Electrical conductivity (μS/cm) for the period 30/3/2022 - 7/4/2022 at the Las Hountas spring (event-based temporal resolution) - Major solute concentrations (mg/L) for the period 30/3/2022 - 7/4/2022 at the Las Hountas spring (event-based temporal resolution)
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This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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