Watercourse


Sediment discharge

Updated on 26/10/2022
Définition
Sens commun
Mass of solids passing through a given cross section of a watercourse per time unit. The sediment discharge includes dissolved matters, suspended solids and riverbed materials. These materials are moved in the riverbed according to different transport laws: thrust, suspension, saltation. Sediment discharge and liquid flow are the two main variables of river dynamics.
Source
According to OFB

Morphogenetic flow

Updated on 26/10/2022
Définition
Sens technique
Full filling up of the riverbed. The bankfull discharge is responsible for the formation and dynamics of flow facies and morphological alterations of the watercourse. It is the liquid flow for which the transported sediment discharge is maximal. We thus speak of morphogenetic flow. For many streams the bankfull discharge is a 1 to 3 year
Source
According to OFB

Liquid flow

Updated on 26/10/2022
Définition
Sens technique
Volume of water passing through a cross section of a watercourse per time unit. The flow rates of watercourses are expressed in m3/s with at least three significant figures (e.g. 1.92 m3/s, 19.2 m3/s, 192 m3/s) or for small streams in l/s. The national HYDRO database stores measurements of water levels coming from 3,500 measuring stations (including 2,400 that are currently in service) and used to calculate instantaneous, daily and monthly flow rates in a large number of French streams. Liquid flow and sediment discharge are the two main variables of river dynamics.
Source
According to OFB

Watercourse

Updated on 13/07/2018
Définition
Sens commun
Legally characterized by the permanence of its bed, the natural character of the stream or its normal water flow (e.g. a channel offering the river, in the collective interest, an additional outlet or replacing the natural bed) and an adequate supply, not limited to discharges or stormwater (the existence of a spring is required).
Source
According to Rhone-Mediterranean and Corsica Water Agency

Riparian corridor

Updated on 13/07/2018
Définition
Sens technique

Strip of natural vegetation located along a river, and which differs from the surrounding matrix, including the river bank, the floodplain and part of the alluvial terraces. The presence of a stream or wood is not enough to make corridors. It is their conduction function that defines them. At the regional level, the riparian corridor appears to be a relatively uniform area (line of trees). At the local level, sedimentary and hydrological constraints provide variability of conditions resulting in a mosaic of habitats. The corridor is a transition zone between the water system and terrestrial system. Thus,…

Source
According to the Ministry of Ecology

Ecological continuity

Updated on 26/10/2022
Définition
Sens commun

For a river, to ensure the free movement of species (in particular fishes) and the smooth flow of sediments.

Source
according to Loire-Bretagne Water Agency and IOWater
Sens technique

Is defined by the free circulation of biological species and good flow of natural river sediment transport. The concept of ecological continuity did not take sediment transport into account until the Water Act of 2006.

Source
according to OFB

Sediment transport

Updated on 13/07/2018
Définition
Sens commun
Phenomenon related to the movement of materials on the bottom of a watercourse. Often used as a synonym for "bedload discharge".
Source
According to Marcel Roche (hydrologist)

Oxbow lake

Updated on 26/10/2022
Définition
Sens commun
Part of an old meander or braid of a river. Oxbow lakes are more or less disconnected from the main channel due to the latter's displacement over time and to sedimentation mechanisms. Depending on their age, season and weather context, oxbow lakes can be with water or dry. These very rich evolutionary environments are favourable for breeding fish and some amphibians.
Source
According to OFB