Articles | Volume 26, issue 13
https://doi.org/10.5194/hess-26-3629-2022
https://doi.org/10.5194/hess-26-3629-2022
Research article
 | 
13 Jul 2022
Research article |  | 13 Jul 2022

Exploring river–aquifer interactions and hydrological system response using baseflow separation, impulse response modeling, and time series analysis in three temperate lowland catchments

Min Lu, Bart Rogiers, Koen Beerten, Matej Gedeon, and Marijke Huysmans

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Cited articles

Alaghmand, S., Beecham, S., Woods, J. A., Holland, K. L., Jolly, I. D., Hassanli, A., and Nouri, H.: Quantifying the impacts of artificial flooding as a salt interception measure on a river-floodplain interaction in a semi-arid saline floodplain, Environ. Model. Softw., 79, 167–183, https://doi.org/10.1016/j.envsoft.2016.02.006, 2016. 
Anibas, C., Fleckenstein, J. H., Volze, N., Buis, K., Verhoeven, R., Meire, P., and Batelaan, O.: Transient or steady-state? Using vertical temperature profiles to quantify groundwater-surface water exchange, Hydrol. Process., 23, 2165–2177, https://doi.org/10.1002/hyp.7289, 2009. 
Anibas, C., Buis, K., Verhoeven, R., Meire, P., and Batelaan, O.: A simple thermal mapping method for seasonal spatial patterns of groundwater–surface water interaction, J. Hydrol., 397, 93–104, https://doi.org/10.1016/j.jhydrol.2010.11.036, 2011. 
Anibas, C., Schneidewind, U., Vandersteen, G., Joris, I., Seuntjens, P., and Batelaan, O.: From streambed temperature measurements to spatial-temporal flux quantification: Using the LPML method to study groundwater-surface water interaction, Hydrol. Process., 30, 203–216, https://doi.org/10.1002/hyp.10588, 2015. 
Anibas, C., Tolche, A. D., Ghysels, G., Nossent, J., Schneidewind, U., Huysmans, M., and Batelaan, O.: Delineation of spatial-temporal patterns of groundwater/surface-water interaction along a river reach (Aa river, belgium) with transient thermal modeling, Hydrogeol. J., 26, 819–835, https://doi.org/10.1007/s10040-017-1695-9, 2017. 
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Short summary
Lowland rivers and shallow aquifers are closely coupled. We study their interactions here using a combination of impulse response modeling and hydrological data analysis. The results show that the lowland catchments are groundwater dominated and that the hydrological system from precipitation impulse to groundwater inflow response is a very fast response regime. This study also provides an alternative method to estimate groundwater inflow to rivers from the perspective of groundwater level.
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