Comparison of the Dynamics of the Flowing Drainage Network and Water Chemistry for Four Headwater Catchments DOI Creative Commons
Izabela Bujak, Jana von Freyberg, Andrea Rinaldo

et al.

Ecohydrology, Journal Year: 2024, Volume and Issue: unknown

Published: Dec. 30, 2024

ABSTRACT The re‐emergence of water in dry stream reaches affects streamwater chemistry due to the flushing sediment and nutrients from previously channels increased connectivity between hillslopes streams. Although these processes have been studied at reach scale, field data on network dynamics hydrochemistry catchment scale are rare. We temporal changes flowing drainage (FDN) for two 5‐ha catchments Swiss pre‐Alps 25‐ 32‐ha Plateau. At each site, one was relatively flat had an extensive augmented by artificial ditches, while other steep a shorter where flow maintained springs. FDN differed substantially geomorphologically different region, despite their proximity, comparable size, soil bedrock characteristics. Hydrochemistry were more dynamic flatter with but shallow ditches. For catchments, nitrate mobilisation notable ‘first flush’ solutes observed during most rainfall events. remained stable steeper fed perennial These results highlight spatial variations responses precipitation events insights that can be gained joint observations hydrochemical dynamics.

Language: Английский

How Alluvial Storage Controls Spatiotemporal Water Balance Partitioning in Intermittent and Ephemeral Stream Systems DOI Creative Commons
E. Zarate, Martin S. Andersen, Gabriel C. Rau

et al.

Water Resources Research, Journal Year: 2025, Volume and Issue: 61(4)

Published: April 1, 2025

Abstract The hydrological dynamics of intermittent rivers and ephemeral streams (IRES) impacts the availability water to riparian ecosystems, height downstream runoff peaks, replenishment groundwater systems. Despite its significance, influence superficial geology on IRES flow processes remains an area limited understanding. Here we first present a comprehensive data set encompassing streamflow levels from stream situated in New South Wales, Australia. We then use targeted geophysical investigations show how configurations control responses. analysis reveals that periods stable stage consistently occur after episodic surges streamflow, followed by recession channel desiccation. duration phases exhibits upstream‐to‐downstream pattern, reaching maximum 44 ± 3 days upstream abruptly declining further downstream. There is remarkable consistency these periods, irrespective size preceding peaks. propose two primary controls this behavior: (a) variability permeability contrasts between alluvium surrounding geological deposits, (b) longitudinal fluctuations volume recent alluvial reservoir. interplay generates “goldilocks zone,” which optimizes potential for recharge landscapes. These may reflect continuum other dryland catchments with widespread implications classification based occurrence duration.

Language: Английский

Citations

0

STICr: An open-source package and workflow for Stream Temperature, Intermittency, and Conductivity (STIC) data DOI Creative Commons
Samuel C. Zipper, C. T. Wheeler, Delaney Peterson

et al.

Environmental Modelling & Software, Journal Year: 2025, Volume and Issue: unknown, P. 106484 - 106484

Published: April 1, 2025

Language: Английский

Citations

0

Diel dissolved organic matter patterns reflect spatiotemporally varying sources and transformations along an intermittent stream DOI
Rebecca L. Hale, Sarah E. Godsey,

Jenna M. Dohman

et al.

Limnology and Oceanography, Journal Year: 2024, Volume and Issue: unknown

Published: Nov. 18, 2024

Abstract Stream dissolved organic matter (DOM) is a globally important carbon flux and locally control on stream ecosystems, therefore understanding controls DOM fluxes dynamics crucial at both local global scales. However, attributing process challenging because hydrological biological are integrated may vary over time throughout networks. Our objective was to assess the patterns corresponding of diel cycles through seasonal flow recession by using reach‐scale in situ sensors non‐perennial network. We identified five characteristic variations with differing phase amplitude. During snowmelt flows, were consistent among sites reflected flowpath shifts photodegradation. Evapotranspiration‐driven stage oscillations emerged two upstream sites, shaping indirectly, creating conditions for instream processing. At spring‐fed site, minimal variation observed summer whereas an intermittent reach, daily drying rewetting created biogeochemical hot moments. This research demonstrates that space, even close proximity, generating asynchronous fDOM during low illuminating processes flowpaths.

Language: Английский

Citations

1

Comparison of the Dynamics of the Flowing Drainage Network and Water Chemistry for Four Headwater Catchments DOI Creative Commons
Izabela Bujak, Jana von Freyberg, Andrea Rinaldo

et al.

Ecohydrology, Journal Year: 2024, Volume and Issue: unknown

Published: Dec. 30, 2024

ABSTRACT The re‐emergence of water in dry stream reaches affects streamwater chemistry due to the flushing sediment and nutrients from previously channels increased connectivity between hillslopes streams. Although these processes have been studied at reach scale, field data on network dynamics hydrochemistry catchment scale are rare. We temporal changes flowing drainage (FDN) for two 5‐ha catchments Swiss pre‐Alps 25‐ 32‐ha Plateau. At each site, one was relatively flat had an extensive augmented by artificial ditches, while other steep a shorter where flow maintained springs. FDN differed substantially geomorphologically different region, despite their proximity, comparable size, soil bedrock characteristics. Hydrochemistry were more dynamic flatter with but shallow ditches. For catchments, nitrate mobilisation notable ‘first flush’ solutes observed during most rainfall events. remained stable steeper fed perennial These results highlight spatial variations responses precipitation events insights that can be gained joint observations hydrochemical dynamics.

Language: Английский

Citations

0