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A study of turbulent flow in large-scale porous media at high Reynolds numbers. Part II: flow physics
KTH, Skolan för arkitektur och samhällsbyggnad (ABE), Byggvetenskap. (Hydraulic Engineering)
KTH, Skolan för arkitektur och samhällsbyggnad (ABE), Byggvetenskap, Vattendragsteknik.ORCID-id: 0000-0002-2342-2068
2016 (engelsk)Inngår i: Journal of Hydraulic Research, ISSN 0022-1686, E-ISSN 1814-2079, Vol. 54, nr 6, s. 678-691Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

The evaluation of hydraulic performance of coarse porous media at high Reynolds numbers is of significant importance for dam safety assessment. To address this task, the present study uses a numerical approach based on a rigorous theoretical framework. The novelty of the study lies in the application of a fully calibrated and validated numerical three-dimensional model and a set of modified equations for momentum transfer and the associated coefficients for flow in porous media. A Lagrangian particle tracking model was used to estimate the lengths of the flow channels that developed in the porous media. Gamma distributions were fitted to the normalized channel lengths, and the scale and shape parameters of the gamma distribution were found to be Reynolds number dependent. These shape parameters can be estimated from the suggested polynomial equations. The proposed normalized length parameter can be used to evaluate permeability, energy dissipation, induced forces, and diffusion. It was found that shear forces exerted on the coarse particles depend on the inertial forces of the flow and can be estimated using the proposed equation for the developed turbulent flows in porous media.

sted, utgiver, år, opplag, sider
Taylor & Francis Group, 2016. Vol. 54, nr 6, s. 678-691
Emneord [en]
Numerical experimentation, particle tracking, porous-media flow, shear turbulence, wall-bounded flows
HSV kategori
Forskningsprogram
Byggvetenskap
Identifikatorer
URN: urn:nbn:se:kth:diva-193719DOI: 10.1080/00221686.2016.1211185ISI: 000386438300006Scopus ID: 2-s2.0-84984669595OAI: oai:DiVA.org:kth-193719DiVA, id: diva2:1033920
Merknad

QC 20161011

Tilgjengelig fra: 2016-10-10 Laget: 2016-10-10 Sist oppdatert: 2020-01-02bibliografisk kontrollert
Inngår i avhandling
1. Internal Erosion Phenomena in Embankment Dams: Throughflow and internal erosion mechanisms
Åpne denne publikasjonen i ny fane eller vindu >>Internal Erosion Phenomena in Embankment Dams: Throughflow and internal erosion mechanisms
2016 (engelsk)Doktoravhandling, med artikler (Annet vitenskapelig)
Abstract [en]

 In this study, two major internal erosion initiation processes, suffusion and concentrated leak mechanisms, which lead to both defect formation in a dam’s body and its foundation and high throughflow in dams subjected to internal erosion were studied. This understanding has the potential to facilitate numerical modelling and expedite dam safety assessment studies. 

The throughflow properties of coarse rockfill material were studied by; analysing filed pump test data, performing extensive laboratory experiments with a large-scale apparatus and numerically simulating the three-dimensional flow through coarse rock materials, replicating the material used in the laboratory experiments.

Results from the tests demonstrate that the parameters of the nonlinear momentum equation of the flow depend on the Reynolds number for pore Reynolds numbers lower than 60000. 

Numerical studies were also carried out to conduct numerical experiments. By applying a Lagrangian particle tracking method, a model for estimating the lengths of the flow channels in the porous media was developed.  The shear forces exerted on the coarse particles in the porous media were found to be significantly dependent on the inertial forces of the flow.

Suffusion and concentrated leak mechanisms were also studied by means of laboratory experiments to develop a theoretical framework for continuum-based numerical modelling. An erosion apparatus was designed and constructed with the capability of applying hydraulic and mechanical loading. Results were then used to develop constitutive laws of the soil erosion as a function of the applied hydromechanical load for both suffusion and concentrated leak mechanisms. Both the initiation and mass removal rate of were found to be dependent on the soil in-situ stresses.

A three-dimensional electrical-resistivity-based tomography method was also adopted for the internal erosion apparatus and was found to be successful in visualising the porosity evolution due to suffusion.

sted, utgiver, år, opplag, sider
Stockholm: KTH Royal Institute of Technology, 2016. s. 74
Serie
TRITA-HYD ; 2016:4
Serie
ISSN, ISSN 1650-8602
Emneord
Internal erosion modelling in porous material; Constitutive law of erosion for closure of continuum-mechanics-based balance equations for numerical modelling; High Reynolds-number turbulent flow; Flow laws; Coarse rockfill material throughflow; Computational Fluid Dynamics.
HSV kategori
Forskningsprogram
Byggvetenskap
Identifikatorer
urn:nbn:se:kth:diva-193627 (URN)978-91-7729-130-5 (ISBN)
Disputas
2016-11-04, Kollegiesalen, Brinellvägen 8, Stockholm, 09:00 (engelsk)
Opponent
Veileder
Merknad

QC 20161006

Tilgjengelig fra: 2016-10-06 Laget: 2016-10-06 Sist oppdatert: 2020-01-02bibliografisk kontrollert

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