Federica Antico

Federica Antico
  • PhD in Civil Hydraulic Engineering
  • PhD Student at University of Lisbon

About

9
Publications
1,017
Reads
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27
Citations
Current institution
University of Lisbon
Current position
  • PhD Student
Additional affiliations
March 2014 - present
University of Lisbon
Position
  • PhD Student

Publications

Publications (9)
Article
Full-text available
We address the issue of characterizing experimentally entrainment and disentrainment of sediment particles of cohesionless granular beds in turbulent open channel flows. Employing Particle Image Velocimetry, we identify episodes of entrainment and of disentrainment of bed particles by analysing the raw PIV images. We define a reference velocity for...
Article
Full-text available
The purpose of the present paper is to provide further insights on the definition of the parameters of the log-law in open-channel flows with rough mobile granular beds. Emphasis is placed in the study of flows over cohesionless granular beds composed of monosized spherical particles in simple lattice arrangements. Potentially influencing factors s...
Article
Full-text available
Channel bed morphology depends on bedload fluxes which are difficult to determine even in controlled laboratory conditions. Particle counting can provide time resolved bedload fluxes. Determination of particle rates by means of digital image processing is computationally expensive and the requirement for optical access is not always met. Weighing m...
Article
Sediment overfeeding may induce important changes in the structure of the near-bed region of gravel-bed river flows, mainly in what concerns exchange of momentum and mass between the flow within the riverbed roughness elements and the flow in the upper regions. Although the turbulent structure of flows over gravel- bed rivers is object of several p...
Article
Full-text available
Sediment overfeeding may induce important changes in the structure of the near-bed region of gravel-bed river flows, mainly in what concerns exchange of momentum and mass between the flow within the riverbed roughness elements and the flow in the upper regions. Although the turbulent structure of flows over gravel- bed rivers is object of several p...

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