1989
DOI: 10.1051/kmae:1989003
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Typologie des faciès d'écoulement ou unités morphodynamiques des cours d'eau à haute énergie

Abstract: RESUMETo sector a stream, classify It and choose the study reaches which could give o reliable picture of it, It is necessary to have a good knowledge of the morphological feotures (faciès) types llkely to be encountered.The Identification of thèse units wlll t>e done In the fleld using some simple crlterlo such as water depth, stream veloclty, sédiment size, cross section shape, longitudinal profile and plan vIew.ThIs wlll be carried out during low flow stage In order to observe the more varled flow condition… Show more

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Cited by 49 publications
(34 citation statements)
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“…The sampled river bed (10 m wide and 2000 m long), extended from the river mouth to 50 m above sea level. It is characterized by small cascades, rapids, cobble-riffles, pools and large runs (according to the classification of Malavoi, 1989). This alternation of hydromorphological facies creates differences in stream velocity and constitutes a mosaic of habitats available for macrofauna.…”
Section: Study Sitementioning
confidence: 99%
“…The sampled river bed (10 m wide and 2000 m long), extended from the river mouth to 50 m above sea level. It is characterized by small cascades, rapids, cobble-riffles, pools and large runs (according to the classification of Malavoi, 1989). This alternation of hydromorphological facies creates differences in stream velocity and constitutes a mosaic of habitats available for macrofauna.…”
Section: Study Sitementioning
confidence: 99%
“…We characterised four types of morphological units and measured their fre quency in each of the sectors studied: shallow riffles, deep riffles, pools and shelters according to Malavoi (1989) (Table 1). Shelters are considered as natural hides available to fish along the banks or in the bed of the river.…”
Section: Study Areamentioning
confidence: 99%
“…Chaque station a été divisée en faciès d'écoulement (MALAVOI, 1989). Sur chacun de ces faciès, des transects de hauteur d'eau (sondage au cm près) et de vitesse du courant (mesurée au cm/s près, à l'aide d'un courantomètre Marsh McBirney 201 D) ont été effectués, et la granulométrie a été estimée au point contact selon l'échelle de CAILLEUX (1954).…”
Section: Mesures D'habitatunclassified