estuarine systems
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2021 ◽  
pp. 1-11
Author(s):  
Cássia de Carvalho ◽  
Leandro Rabello Monteiro ◽  
Karina A. Keunecke ◽  
Helena P. Lavrado ◽  
Ana Paula M. Di Beneditto

Author(s):  
Oluwatosin A. Onabule ◽  
Steve B. Mitchell ◽  
Fay Couceiro ◽  
John B. Williams

Water ◽  
2021 ◽  
Vol 13 (21) ◽  
pp. 3008
Author(s):  
Argyrios S. Sapounidis ◽  
Emmanuil T. Koutrakis

Maintaining and improving the aquatic ecosystems in the community is the aim of the Water Framework Directive (WFD) 2000/60/EC. The WFD requires the water quality to be classified into five categories. Lagoons are dynamic ecosystems. The fish communities inhabiting them are highly affected by the environmental conditions prevailing both in the freshwater systems and in the marine environment. The current paper presented the first effort to develop a fish-based index (Lagoon Fish-based Index—LFI) for the assessment of the Mediterranean shallow lagoons, as almost all indices produced to date refer to freshwater or estuarine systems. For the development and calibration of the index, data were collected from nine lagoons situated in three estuarine systems in the East Macedonia and Thrace regions. The development of the LFI was based on the principles of the Indices of Biological Integrity (IBIs) that were primary used for the assessment of aquatic ecosystems in the USA. A total number of 25 metrics were selected as potential metrics for the LFI. These metrics describe attributes such as the abundance and composition of the fish fauna, the feeding strategies of the species, and the presence of sentinel species. Finally, eight metrics were included in the LFI.


Water ◽  
2021 ◽  
Vol 13 (21) ◽  
pp. 2977
Author(s):  
Stephan Korblah Lawson ◽  
Hitoshi Tanaka ◽  
Keiko Udo ◽  
Nguyen Trong Hiep ◽  
Nguyen Xuan Tinh

It is well known that estuarine systems are significantly affected by hydrodynamic conditions such as river discharge, storm surges, waves and tidal conditions. In addition to this, human interferences through developmental projects have the capability of disrupting the natural morphological processes occurring at estuaries. In West Africa, the goal to improve standards of living through large-scale dam construction, offshore ports and coastal erosion countermeasures has triggered alarming changes in the morphodynamics of estuarine systems. The estuaries at the Volta River mouth (Ghana) and “Bouche du Roi” inlet (Benin), located along the Bight of Benin coast, West Africa, were selected as two case study sites to examine their long-term morphodynamics and sandspit evolution. In this study, we primarily analyzed estuarine morphology using remotely sensed images acquired from 1984 to 2020. We further estimated the longshore sediment transport for this region using results from the image analysis and the depth of active sediment motion. Our results reveal that the longshore sediment transport rates for this region are in the magnitude of 105–106 m3/year. Comparative analysis with other estuaries and sandy coasts suggests that the longshore sediment transport along this coast has one of the largest rates estimated in the world.


2021 ◽  
Author(s):  
Claire Chassagne ◽  
Zeinab Safar ◽  
Zhirui Deng ◽  
Qing He ◽  
Andy Manning

Modelling the flocculation of particles in a natural environment like an estuary is a challenging task owing to the complex particle-particle and particle-hydrodynamic interactions involved. In this chapter a summary is given of recent laboratory and in-situ studies regarding flocculation. A flocculation model is presented and the way to implement it in an existing sediment transport model is discussed. The model ought to be parametrized, which can be done by performing laboratory experiments which are reviewed. It is found, both from laboratory and in-situ studies, that flocculation between mineral sediment and organic matter is the dominant form of flocculation in estuarine systems. Mineral sediment in the water column is < 20 μm in size and its settling velocity is in the range [0–0.5] mm/s. Flocs can then be categorized in two types: flocs of size [20–200] μm and flocs of size > 200 μm. The origin of these two types is discussed. The two types of flocs are found at different positions in the water column and both have settling velocities in the range [0.5–10] mm/s.


Chemosphere ◽  
2021 ◽  
Vol 278 ◽  
pp. 130338
Author(s):  
Prantick Patra ◽  
Chellandi Mohandass ◽  
Parthasarathi Chakraborty ◽  
Seyieleno C. Seleyi

Author(s):  
Angéline Lefran ◽  
Tania Hernández Fariñas ◽  
Francis Gohin ◽  
Pascal Claquin

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