Results 241 to 250 of about 100,610 (311)
Fossil wood cells recorded 300 million years of Europe's tectonic history. [PDF]
Trümper S +10 more
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Monitoring bioremediation of an impacted coastal lagoon through nature-based solutions: a case study of the Maricá Lagoon (RJ, Brazil). [PDF]
de Carvalho Aguiar VM +8 more
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Diversity and structure of riparian forests in an industrial and urban hub of the Amazon. [PDF]
de Matos Rodrigues JI +4 more
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High-resolution dataset (2017-2023) of physical-geographical predictors for machine learning modelling of fluvial flooding: the Gidra river case, Slovakia. [PDF]
Vojtek M +7 more
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Incorporating river morphodynamics in the characterization of key ecological system units for conservation in the western Amazon. [PDF]
Dominguez-Ruben L +6 more
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Some Aspects on Fluvial Sediments and Fluvial Morphology
Geografiska Annaler: Series A, Physical Geography, 1968This article is the second in a series of articles (cf. Sundborg 1967) dealing with fluvial sediments and fluvial morphology and accounting for results of field research, experimental investigation...
Pontus Ljunggren, Äke Sundborg
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From fluvial dynamics to eco-fluvial dynamics
International Journal of Sediment Research, 2019Abstract Sediment plays a very important role in the functioning of river ecosystems. It is the basic substance for the survival of benthic animals and aquatic plants. On the other hand, the growth of biofilms and bio-disturbance of benthos affect the sediment transport characteristics. With the increasing attention to protect aquatic ecosystems, the
Guojian He +3 more
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1972
Abstract The width (w) depth (d), meander wavelength (l), gradient (s), shape (w/d), and sinuosity (P) of stable alluvial river channels are dependent on the volume of water moving through the channel (Qw) and the type of sediment load conveyed through the channel (Qs).
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Abstract The width (w) depth (d), meander wavelength (l), gradient (s), shape (w/d), and sinuosity (P) of stable alluvial river channels are dependent on the volume of water moving through the channel (Qw) and the type of sediment load conveyed through the channel (Qs).
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