AbstractThe 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 truly neither to surface- nor to groundwater. Exchanges of water, nutrients, and organic matter occur in response to variations in discharge and bed topography and porosity. Dynamic gradients exist at all scales and vary temporally. Across all scales, the functional significance of the HZ relates to its activity and connection with the surface stream. The HZ is a relatively rich environment and almost all invertebrate groups have colonized this habitat. This fauna, so-called hyporheos...
Rivers are important ecosystems under continuous anthropogenic stresses. The hyporheic zone is a ubi...
The hyporheic zone is an important ecotone where hydrological, biogeochemical and ecological process...
The hyporheic zone and its interactions with coarse surface sediments is increasingly reported by aq...
Distinct boundaries, where biological and physicochemical environments change abruptly, occur in nat...
[Departement_IRSTEA]Eaux [TR1_IRSTEA]BELCA [TR2_IRSTEA]QUASARE [TR2_IRSTEA]ARCEAUInternational audie...
Abstract In the Neotropical Region, information concerning hyporheic communities is virtually non-ex...
International audienceThe interface between groundwater and surface water within riverine/riparian e...
Rivers are important ecosystems under continuous anthropogenic stresses. The hyporheic zone is a ubi...
Flow of water is essential to provide food (organic matter - OM), nutrients (e.g. N and P) and elect...
Abstract In the Neotropical Region, information concerning hyporheic communities is virtually non-ex...
Environmental conditions in the interstices beneath streams and rivers with porous beds are unlike t...
Physical, chemical, or biological exchanges that occur between the groundwater system and surface wa...
The hyporheic zone of streams not only connects groundwater and surface water, but is essential for ...
A principal ecological role proposed for the hyporheic zone is as a refugium that promotes benthic i...
Rivers are important ecosystems under continuous anthropogenic stresses. The hyporheic zone is a ubi...
The hyporheic zone is an important ecotone where hydrological, biogeochemical and ecological process...
The hyporheic zone and its interactions with coarse surface sediments is increasingly reported by aq...
Distinct boundaries, where biological and physicochemical environments change abruptly, occur in nat...
[Departement_IRSTEA]Eaux [TR1_IRSTEA]BELCA [TR2_IRSTEA]QUASARE [TR2_IRSTEA]ARCEAUInternational audie...
Abstract In the Neotropical Region, information concerning hyporheic communities is virtually non-ex...
International audienceThe interface between groundwater and surface water within riverine/riparian e...
Rivers are important ecosystems under continuous anthropogenic stresses. The hyporheic zone is a ubi...
Flow of water is essential to provide food (organic matter - OM), nutrients (e.g. N and P) and elect...
Abstract In the Neotropical Region, information concerning hyporheic communities is virtually non-ex...
Environmental conditions in the interstices beneath streams and rivers with porous beds are unlike t...
Physical, chemical, or biological exchanges that occur between the groundwater system and surface wa...
The hyporheic zone of streams not only connects groundwater and surface water, but is essential for ...
A principal ecological role proposed for the hyporheic zone is as a refugium that promotes benthic i...
Rivers are important ecosystems under continuous anthropogenic stresses. The hyporheic zone is a ubi...
The hyporheic zone is an important ecotone where hydrological, biogeochemical and ecological process...
The hyporheic zone and its interactions with coarse surface sediments is increasingly reported by aq...