Results 11 to 20 of about 143 (79)

Patterns and Processes of Groundwater Invasion by Copepods in the Interior Low Plateaus of the United States

open access: yesActa Carsologica, 2007
The copepod crustacean fauna collected from subterranean habitats, including caves, wells, and the hyporheos of streams in and near the Interior Low Plateaus of the United States is dominated by Cyclopoida, with 39 species, followed by Harpacticoida with
Julian J. Lewis, Janet W. Reid
doaj   +3 more sources

The hyporheic zone and its functions: revision and research status in Neotropical regions

open access: yesBrazilian Journal of Biology
The hyporheic zone (HZ), as the connecting ecotone between surface- and groundwater, is functionally part of both fluvial and groundwater ecosystems. Its hydrological, chemical, biological and metabolic features are specific of this zone, not belonging ...
R Mugnai, G Messana, T Di Lorenzo
doaj   +2 more sources

Responses of resources and consumers to experimental flow pulses in a temporary Mediterranean stream [PDF]

open access: yes, 2021
Determining the resistance and resilience of resources and benthic invertebrates connected to instream refuges and species re-colonization in post-flood periods may help to elucidate mechanisms behind community recovery.
Verdonschot, Piet F.M.   +5 more
core   +5 more sources

Invertebrate Responses to Restoration across Benthic and Hyporheic Stream Compartments [PDF]

open access: yes, 2021
River restoration is a multi-billion-dollar business, yet it is unclear whether benthic community health, which is routinely monitored, can be used as a proxy for the health of the hyporheos.
Robertson, AL   +11 more
core   +1 more source

Metabolism Modeling in Rivers With Unsteady Flow Conditions and Transient Storage Zones

open access: yesJournal of Geophysical Research: Biogeosciences, Volume 128, Issue 3, March 2023., 2023
Abstract Whole‐stream metabolism characterizes energy and carbon transformations, thus providing an estimate of the food base and CO2 emission sources from streams and rivers. Metabolism models are generally implemented with a steady flow assumption that does not hold true for many systems with sub‐daily flow variation, such as river sections ...
Devanshi Pathak, Benoît O. L. Demars
wiley   +1 more source

Quantifying the ecological effects of water abstraction in Alpine streams through flume simulations

open access: yesEcohydrology, Volume 15, Issue 6, September 2022., 2022
Abstract Water abstraction by small hydropower plants is a growing human pressure on Alpine stream ecosystems. Using a set of seminatural streamside flumes, we investigated the response of benthic invertebrate communities to a 50% experimental reduction of the natural discharge.
Francesca Vallefuoco   +3 more
wiley   +1 more source

The hyporheic zone as an invertebrate refuge during a fine sediment disturbance event

open access: yesEcohydrology, Volume 15, Issue 6, September 2022., 2022
Abstract Subsurface sediments offer an important refuge that support the survival and persistence of river invertebrates during adverse surface conditions. Access to refuges for invertebrates varies with differing hydrological and substrate characteristics, especially the proportion of fine sediment.
Victoria S. Milner   +3 more
wiley   +1 more source

Organizational Principles of Hyporheic Exchange Flow and Biogeochemical Cycling in River Networks Across Scales

open access: yesWater Resources Research, Volume 58, Issue 3, March 2022., 2022
Abstract Hyporheic zones increase freshwater ecosystem resilience to hydrological extremes and global environmental change. However, current conceptualizations of hyporheic exchange, residence time distributions, and the associated biogeochemical cycling in streambed sediments do not always accurately explain the hydrological and biogeochemical ...
Stefan Krause   +19 more
wiley   +1 more source

Temperature time series in the stream and adjacent hyporheos.

open access: yes, 2023
Upper-left quadrant: B station. Upper-right quadrant: C station. Lower-left quadrant: E station. Lower-right quadrant: I station. Blue line: stream temperature. Brown lines: hyporheos temperature at increasing depths, from 10cm-deep (pale brown) to 20cm-,
Nicolas Flipo (14626802)   +5 more
core   +1 more source

Lag time (in h) between surface water and hyporheos maximum temperature at different depths.

open access: yes, 2023
Lag time (in h) between surface water and hyporheos maximum temperature at different depths.
Nicolas Flipo (14626802)   +5 more
core   +1 more source

Home - About - Disclaimer - Privacy