The HydroEcoSedimentary tool: An integrated approach to characterise interstitial hydro‐sedimentary and associated ecological processes

Casas‐Mulet, Roser ORCIDiD
Pander, Joachim ORCIDiD
Prietzel, Maximilian
Geist, Juergen ORCIDiD

DOI: https://doi.org/10.1002/rra.3819
Persistent URL: http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9832
Casas‐Mulet, Roser; Pander, Joachim; Prietzel, Maximilian; Geist, Juergen, 2021: The HydroEcoSedimentary tool: An integrated approach to characterise interstitial hydro‐sedimentary and associated ecological processes. In: River Research and Applications, 37, 7, 988-1002, DOI: https://doi.org/10.1002/rra.3819. 
 
Pander, Joachim; 1 Aquatic Systems Biology Unit TUM School of Life Sciences, Technical University of Munich Freising Germany
Prietzel, Maximilian; 1 Aquatic Systems Biology Unit TUM School of Life Sciences, Technical University of Munich Freising Germany
Geist, Juergen; 1 Aquatic Systems Biology Unit TUM School of Life Sciences, Technical University of Munich Freising Germany

Abstract

Increased deposition of fine sediments in rivers and streams affects a range of key ecosystem processes across the sediment–water interface, and it is a critical aspect of river habitat degradation and restoration. Understanding the mechanisms leading to fine sediment accumulation along and across streambeds and their effect on ecological processes is essential for comprehending human impacts on river ecosystems and informing river restoration. Here, we introduce the HydroEcoSedimentary tool (HEST) as an integrated approach to assess hydro‐sedimentary and ecologically relevant processes together. The HEST integrates the estimation of sedimentary processes in the interstitial zone, as well as hydraulic, geochemical and ecological assessments, with a focus on brown trout early life stages. Compared to other methods, the HEST expands the possibilities to monitor and quantify fine sediment deposition in streambeds by differentiating between vertical, lateral and longitudinal infiltration pathways, and distinguishing between the depth (upper vs. lower layers) at which interstitial processes occur within the sediment column. By testing the method in two rivers with different degrees of morphological degradation, we detail the possible measurements and uses of the HEST, demonstrate its feasibility and discuss its reliability.