Integrating transpiration and xylem water stable isotopes in a process-based model to determine transpiration and discharge age distributions
- 1Environmental Research and Innovation Department, Luxembourg Institute of Science and Technology, Belvaux, Luxembourg (maelle.fresne@list.lu)
- 2The University of the West of England, Bristol, UK
- 3Faculty of Science, Technology and Medicine, University of Luxembourg, Belval, Luxembourg
- 4Department of Agriculture, Food, Environment and Forestry, University of Florence, Florence, Italy
- 5Department of Water Management, Faculty of Civil Engineering and Geosciences, Delft University of Technology, Netherlands
- 6Department of Forest Resources and Environmental Conservation, Virginia Tech, Blacksburg, VA, USA
- 7Earth and Life Institute, UC Louvain, Belgium
- 8Department of Geography, University of Bonn, Germany
Transpiration is an important component of the catchment water balance, and tree water uptake can significantly influence discharge dynamic and travel times. Tree usually use water of a different age than the water that generates discharge. Most hydrological models that track water age rely on discharge and stream water isotopes data for calibration. This calibrated age-tracking model enables to simulate time-variant discharge travel times. However, transpiration and related water isotopes data are rarely integrated. We currently lack understanding on the age distribution of transpiration and how discharge travel times relate to this age distribution. In this context, the objectives of this work are to 1) analyse spatio-temporal patterns of xylem water isotopes, 2) determine transpiration age distribution and investigate its temporal dynamic over two growing seasons and 3) evaluate how discharge travel times respond to changes in the transpiration age distribution. We determined the spatial controls on xylem water isotopes (δ18O and δ2H) and simulated travel times in discharge and transpiration in a forested catchment in Luxembourg. We used a lumped, process-based catchment model for water fluxes and tracer transport based on storage-age selection functions. Using discharge, transpiration, stream and xylem water δ2H measurements, the model was calibrated over a period of three years (October 2017-September 2020) by means of a Monte Carlo optimization and a multi-objectives approach. Preliminary results indicate that tree species and diameter are the main drivers of xylem water isotopes variation. Vegetation controls are especially dominant during a drier growing season while landscape variables (hillslope position, topographical position index, flow accumulation) appear to also control xylem water δ2H in wetter conditions. Investigations of transpiration and discharge age distributions will help to better understand how tree water uptake influences discharge travel times over the growing seasons. The spatial analysis of xylem water isotopes further provides a foundation for investigating the spatial variability of the transpiration age distribution. This study will also profit in assessing the value of transpiration and associated isotopes data for discharge travel times simulations and improving our current model representations of hydrological processes in forested catchments.
How to cite: Fresne, M., Chun, K. P., Fabiani, G., Hrachowitz, M., McGuire, K., Moussa, A., Schoppach, R., and Klaus, J.: Integrating transpiration and xylem water stable isotopes in a process-based model to determine transpiration and discharge age distributions, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-3046, https://doi.org/10.5194/egusphere-egu22-3046, 2022.
