Novel observation techniques (e.g., smart tracers) for characterizing coupled hydrological and biogeochemical processes are improving understanding of stream network transport and transformation dynamics. In turn, these observations are thought to enable increasingly sophisticated representations within transient storage models (TSMs). However, TSM parameter estimation is prone to issues with insensitivity and equifinality, which grow as parameters are added to model formulations. Currently, it is unclear whether (or not) observations from different tracers may lead to greater process inference and reduced parameter uncertainty in the context of TSM. Herein, we aim to unravel the role of in‐stream processes alongside metabolically active (M...
Water storage dynamics modulate fluxes within catchments, control the rainfall-runoff response and r...
Models must effectively represent velocities and celerities if they are to address the old water par...
Solute transport in rivers is controlled by surface hydrodynamics and by mass exchanges with distinc...
International audienceNovel observation techniques (e.g., smart tracers) for characterizing coupled ...
International audienceImproved understanding of stream solute transport requires meaningful comparis...
Little is known about the impact of surface transient storage (STS) zones on reach‐scale transport a...
Transient storage of stream water and associated solutes is expected to vary along stream networks i...
Author Posting. © American Geophysical Union, 2011. This article is posted here by permission of Am...
Ecological functions are coupled to the physical transport of water and solutes in streams. Transpor...
Using “smart” tracers such as Resazurin (Raz) allows assessment of sediment-water interactions and a...
Abstract. The fate of contaminants in streams and rivers is affected by exchange and biogeochemical ...
Stream hydraulics control flux into and out of slow-moving water transient storage (WTS) zones and, ...
The stream tracer experiment, including field tracer application and subsequent analysis of solute t...
Transient storage processes in streams are well recognized as being spatially variable; however, thi...
ABSTRACT: A stream tracer study was conducted in a 320-m reach of Indian Creek in Philadelphia. The ...
Water storage dynamics modulate fluxes within catchments, control the rainfall-runoff response and r...
Models must effectively represent velocities and celerities if they are to address the old water par...
Solute transport in rivers is controlled by surface hydrodynamics and by mass exchanges with distinc...
International audienceNovel observation techniques (e.g., smart tracers) for characterizing coupled ...
International audienceImproved understanding of stream solute transport requires meaningful comparis...
Little is known about the impact of surface transient storage (STS) zones on reach‐scale transport a...
Transient storage of stream water and associated solutes is expected to vary along stream networks i...
Author Posting. © American Geophysical Union, 2011. This article is posted here by permission of Am...
Ecological functions are coupled to the physical transport of water and solutes in streams. Transpor...
Using “smart” tracers such as Resazurin (Raz) allows assessment of sediment-water interactions and a...
Abstract. The fate of contaminants in streams and rivers is affected by exchange and biogeochemical ...
Stream hydraulics control flux into and out of slow-moving water transient storage (WTS) zones and, ...
The stream tracer experiment, including field tracer application and subsequent analysis of solute t...
Transient storage processes in streams are well recognized as being spatially variable; however, thi...
ABSTRACT: A stream tracer study was conducted in a 320-m reach of Indian Creek in Philadelphia. The ...
Water storage dynamics modulate fluxes within catchments, control the rainfall-runoff response and r...
Models must effectively represent velocities and celerities if they are to address the old water par...
Solute transport in rivers is controlled by surface hydrodynamics and by mass exchanges with distinc...