Zone photique

thumb|right|250px|Diagramme des couches de la zone pélagique. La zone photique, aussi nommée zone euphotique, zone épipélagique ou couche photique, est la zone aquatique d’un lac ou d’un océan exposée à une lumière suffisante pour que la photosynthèse s'y produise. La profondeur de la zone photique peut être grandement affectée par la turbidité et la latitude. Elle s’étend jusqu’à une profondeur à laquelle l’intensité lumineuse résiduelle correspond à 1 % de celle en surface (également appelée « profondeur euphotique »). Sa taille dépend de l’étendue de l’atténuation lumineuse dans les colonnes d’eau. Typiquement, la profondeur euphotique varie de plusieurs mètres dans les estuaires turbidiques jusqu’à environ en haute mer. En milieu marin, la zone photique correspond à la partie supérieure de la zone pélagique. La zone photique est la seule zone aquatique où la productivité marine primaire (algues, phanérogames) existe, à l’exception de la productivité abyssale (turbine hydrotherma

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Competition between cooling and shortwave radiation in shaping near-surface convection in pelagic waters of Lake Geneva

Hugo Cruz

When lake surface waters above the temperature of maximum density 4◦C cools, the verysurface fluid parcels become denser than their neighbours below. The latter process leads to a gravitationally unstable density distribution which may trigger ‘free convection’, i.e. the upper denser waters look for their equilibrium position somewhere down in the water column. This phenomenon usually occurs at night time, when the atmosphere is colder than surface waters. However, during daytime, it may happen that the lake surface cools—releasing heat to the atmosphere—while shortwave radiation penetrates through upper waters. In this scenario, the near surface waters of the photic zone can host an unstable layer due to the net surface cooling, whereas waters beneath it experience radiative heating and gravitational stabilization. Here, we investigate the competition between shortwave radiation and surface cooling when wind is low or negligible. Thus, depending on the relative intensity of surface cooling and shortwave radiation, the upper water column undergoes different gravitationally unstable density distributions and potentially convective regions. The objective of this Master Project is to investigate, describe, and characterise such convective regimes. To do so, the heat equation controlling temperature evolution of the upper water column subject to surface cooling and penetrative radiative heating is investigated. In parallel with in-situ observations, mathematical and numerical modelling allow to understand the phenomenon taking place. The results allow to infer how the relative importance of surface cooling and penetrating shortwave radiation may affect vertical heat and mass transfer within the lake and between the lake and the atmosphere.

2021

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Density effects on nanoparticle transport in the hyporheic zone

David Andrew Barry, Qihao Jiang

A carbon solution composed of nanoparticles was used in experiments designed to explore nanoparticle transport characteristics within the hyporheic zone of a riverbed. Experiments and numerical simulations demonstrated that nanoparticle transport in the hyporheic zone is affected by hydraulic head gradients due to river flow-bedform interactions as well as density gradients associated with the nano-carbon solution. Differences with similar flow/transport situations were examined, and it was found that particulate-enhanced density can change hyporheic transport appreciably. In addition to density, particle settling enhances downward movement of the nano-carbon plume in the riverbed. While nanoparticle transport in the upper hyporheic zone is largely controlled by advection due to flow driven by head gradients at the bed surface, density gradients and particle settling influence the transport process significantly in the lower hyporheic zone. During the transport process, nanoparticles become deposited due to attachment to sand particles and filtration by small pores in the bed. Compared with transport where density variations are minimal, the particulate-induced density gradient induces downward transport of nanoparticles and entrained liquids, leading to deposition/accumulation at the base of the bed.

2018

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Density-dependent solute transport in a layered hyporheic zone

David Andrew Barry, Mohsen Cheraghi, Qihao Jiang, Jing Xu

Hyporheic exchange is affected by bedform geometry, which induces complex flow paths within the bedform. Additional factors that influence flow and solute transport in the hyporheic zone are layered profile sediments and density-driven flow. This study explored the combined effects of these factors on hyporheic exchange through laboratory experiments and numerical simulations involving infiltrating solute displacing less-dense resident water in a layered bedform with a low permeability layer (LPL). The bedform consisted of three horizontal layers, in which the hydraulic conductivity of the middle layer (LPL) was less than that of the top (TL) and bottom layers (BL). The results demonstrated that a previously unexplored combination of mechanisms (density effects and layered bedform) produces irregular spatial patterns of solute transport in the hyporheic zone. For instance, the width of solute plume within the bottom layers becomes narrowed compared with tracer transport. With increasing density contrast between infiltrating solute and resident water, the solute plume becomes much narrower, forming fingers. Numerical modeling further shows that the hydraulic conductivity contrast (HCC) and relative thickness (RT) of the hyporheic zone layers also affect the spatial solute transport patterns. As the hydraulic conductivity contrast or relative thickness increases, the plume becomes much narrower. Horizontal ambient flow (HAF) dominated in the bottom layers, and lateral solute spreading and mixing intensified with a higher hydraulic conductivity contrast and relative thickness. Furthermore, the vertical solute plume was detached by the horizontal ambient flow in the bottom layers with a discontinuous low permeability layer, forming a discontinuous zone of vertical solute transport.

ELSEVIER SCI LTD2020

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ENV-426: Fluvial biogeosciences

Stream and river ecosystems are increasingly deteriorated owing to global change and climate change. Students will understand basic physical, chemical and biological processes in streams and rivers, and how they relate to ecosystem health and integrity .

ENV-406: Biomineralization: from nature to application

Understanding process and role of biomineralization (minerals formed by living organisms) in context of Earth's evolution,global chemical cycles, climatic changes and remediation.

ENV-220: Fundamentals in ecology

The students will learn the fundamentals in ecology with the goal to perceive the environment beyond its physical and chemical characteristics. Starting from basic concepts, they will acquire mechanistic understanding of biodiversity, ecosystem functioning and global change.

Phytoplancton

Le phytoplancton (du grec φυτόν, phyton, pour « plante » et πλαγκτός, planktos, errante) est le plancton autotrophe vis-à-vis du carbone, obtenant son énergie par la photosynthèse (comme les plantes)

Bacillariophyta

Les Bacillariophyta, ou Diatomées, sont un embranchement d'eucaryotes unicellulaires (de deux micromètres à un millimètre) présents dans tous les milieux aquatiques et majoritaires dans certains bio

Océan

vignette|Animation montrant les découpages possibles en 5, 4, 3 ou 1 seul océan(s). vignette|Le grand océan planétaire, mis en valeur par la projection de Fuller. Un océan est souvent défini, en géogr