Fryderyk Wilczyński
Current Organizations / Institutes
The organizations/institutes from the scholar's latest article
Fryderyk Wilczyński has a total of 10 co-authors. Here are the top co-authors by number of shared publications:
- David W. Hughes
School of Mathematics, University of Leeds 1 , Leeds LS2 9JT, UK
5 shared publications - Fulvio Militello
UKAEA (United Kingdom Atomic Energy Authority)
2 shared publications - Wayne Arter
U.K. Atomic Energy Authority, Culham Science Centre, Abingdon, U.K.
2 shared publications - Christopher A. Jones
Newcastle University
1 shared publication Christopher J. Davies
University of Leeds
1 shared publication- Christopher J. Davies
University of Leeds
1 shared publication
Latest Publications
- Open Access
- 13 April 2026
- Published by Cambridge University Press (CUP) in Journal of Fluid Mechanics
- Vol. 1033
Rotating Rayleigh–Bénard convection with fixed-flux thermal boundary conditions
We derive the asymptotic solution for the onset of steady, linear, Boussinesq convection in a rapidly rotating system with stress-free, fixed-flux boundary conditions. While the fixed-temperature (FT) case is attainable analytically with relative ease, the fixed-flux (FF) configuration presents greater complexity. However, in the rapidly rotating limit, the leading-order interior solution remains unaffected by the choice of thermal boundary conditions. We exploit this property by employing an asymptotic approach to characterise the differences between the FT and FF systems. Specifically, this involves constructing a composite boundary layer structure comprising an Ekman layer of thickness $ {\textit{Ta}}^{-1/4}$ , where $ \textit{Ta}$ is the Taylor number ( $ \textit{Ta} \gg 1$ for rapid rotation), and a thermal boundary layer of thickness $ {\textit{Ta}}^{-1/6}$ , to accommodate the FF boundary condition. To capture both scales systematically, we introduce the small parameter ${\varepsilon } = {\textit{Ta}}^{-1/12}$ , representing the ratio between the two boundary layer thicknesses, and use it to guide the asymptotic expansion. The asymptotic corrections capturing the differences between the two systems are combined with the FT system to construct the corresponding solution for the FF system. We find an asymptotic correction of ${\mathcal{O}} ( {\textit{Ta}}^{-1/2} )$ to the critical Rayleigh number, corresponding wavenumber, vertical velocity and temperature, along with a correction of ${\mathcal{O}} ( {\textit{Ta}}^{-1/6} )$ to the vertical vorticity.- 13 April 2026
- Published by Cambridge University Press (CUP) in Journal of Fluid Mechanics
- Vol. 1033
Open AccessRotating Rayleigh–Bénard convection with fixed-flux thermal boundary conditions
We derive the asymptotic solution for the onset of steady, linear, Boussinesq convection in a rapidly rotating system with stress-free, fixed-flux boundary conditions. While the fixed-temperature (FT) case is attainable analytically with relative ease, the fixed-flux (FF) configuration presents greater complexity. However, in the rapidly rotating limit, the leading-order interior solution remains unaffected by the choice of thermal boundary conditions. We exploit this property by employing an asymptotic approach to characterise the differences between the FT and FF systems. Specifically, this involves constructing a composite boundary layer structure comprising an Ekman layer of thickness $ {\textit{Ta}}^{-1/4}$ , where $ \textit{Ta}$ is the Taylor number ( $ \textit{Ta} \gg 1$ for rapid rotation), and a thermal boundary layer of thickness $ {\textit{Ta}}^{-1/6}$ , to accommodate the FF boundary condition. To capture both scales systematically, we introduce the small parameter ${\varepsilon } = {\textit{Ta}}^{-1/12}$ , representing the ratio between the two boundary layer thicknesses, and use it to guide the asymptotic expansion. The asymptotic corrections capturing the differences between the two systems are combined with the FT system to construct the corresponding solution for the FF system. We find an asymptotic correction of ${\mathcal{O}} ( {\textit{Ta}}^{-1/2} )$ to the critical Rayleigh number, corresponding wavenumber, vertical velocity and temperature, along with a correction of ${\mathcal{O}} ( {\textit{Ta}}^{-1/6} )$ to the vertical vorticity. - Open Access
- 24 November 2023
- Published by Cambridge University Press (CUP) in Journal of Fluid Mechanics
- Vol. 976
A two-phase pure slurry model for planetary cores: one-dimensional solutions and implications for Earth's F-layer
We develop and analyse a continuum model of two-phase slurry dynamics for planetary cores. Mixed solid–liquid slurry regions may be ubiquitous in the upper cores of small terrestrial bodies and have also been invoked to explain anomalous seismic structure in the F-layer at the base of Earth's liquid iron core. These layers are expected to influence the dynamics and evolution of planetary cores, including their capacity to generate global magnetic fields; however, to date, models of two-phase regions in planetary cores have largely ignored the complex fluid dynamics that arises from interactions between phases. As an initial application of our model, and to focus on fundamental fluid dynamical processes, we consider a non-rotating and non-magnetic slurry comprised of a single chemical component with a temperature that is tied to the liquidus. We study one-dimensional solutions in a configuration set up to mimic Earth's F-layer, varying gravitational strength $R$ , the solid/liquid viscosity ratio $\lambda _{\mu }$ and the interaction parameter $K$ , which measures friction between the phases. We develop scalings describing behaviour in the limit $R \gg 1$ and $\lambda _{\mu } \gg 1$ , which are in excellent agreement with our numerical results. Application to Earth's core, where $R \sim 10^{28}$ and $\lambda _{\mu } \sim 10^{22}$ , suggests that a pure iron slurry F-layer would contain a mean solid fraction of at most 5 %.- 24 November 2023
- Published by Cambridge University Press (CUP) in Journal of Fluid Mechanics
- Vol. 976
Open AccessA two-phase pure slurry model for planetary cores: one-dimensional solutions and implications for Earth's F-layer
We develop and analyse a continuum model of two-phase slurry dynamics for planetary cores. Mixed solid–liquid slurry regions may be ubiquitous in the upper cores of small terrestrial bodies and have also been invoked to explain anomalous seismic structure in the F-layer at the base of Earth's liquid iron core. These layers are expected to influence the dynamics and evolution of planetary cores, including their capacity to generate global magnetic fields; however, to date, models of two-phase regions in planetary cores have largely ignored the complex fluid dynamics that arises from interactions between phases. As an initial application of our model, and to focus on fundamental fluid dynamical processes, we consider a non-rotating and non-magnetic slurry comprised of a single chemical component with a temperature that is tied to the liquidus. We study one-dimensional solutions in a configuration set up to mimic Earth's F-layer, varying gravitational strength $R$ , the solid/liquid viscosity ratio $\lambda _{\mu }$ and the interaction parameter $K$ , which measures friction between the phases. We develop scalings describing behaviour in the limit $R \gg 1$ and $\lambda _{\mu } \gg 1$ , which are in excellent agreement with our numerical results. Application to Earth's core, where $R \sim 10^{28}$ and $\lambda _{\mu } \sim 10^{22}$ , suggests that a pure iron slurry F-layer would contain a mean solid fraction of at most 5 %. - Open Access
- 27 May 2022
- Published by Cambridge University Press (CUP) in Journal of Fluid Mechanics
- Vol. 942
Magnetic buoyancy instability and the anelastic approximation: regime of validity and relationship with compressible and Boussinesq descriptions
Magnetic buoyancy instability, which is of astrophysical importance, results from the influence of magnetic pressure variations on the density of a fluid in a gravitational field. It is inherently a compressible phenomenon and is, as such, fully described by the equations of compressible magnetohydrodynamics (MHD). For analytical and computational reasons, it is often convenient to study compressible MHD within simpler, asymptotically consistent reduced systems; the two most widely used result from the Boussinesq and anelastic approximations. Within the standard Boussinesq approximation of MHD, leading to the equations of Boussinesq magnetoconvection, magnetic buoyancy is excluded. It can, however, be included by a rescaling of the basic-state variables and by making further assumptions about the perturbation length scales. Within the anelastic approximation, no special measures are taken to incorporate magnetic buoyancy. It is, however, a priori unclear as to whether this neglect is justified, particularly in the light of the Boussinesq results. Our aims here are thus twofold. The first is to formulate the relationship between descriptions of magnetic buoyancy in the compressible, anelastic and Boussinesq systems. In so doing, we show that, under both the anelastic and Boussinesq approximations, magnetic buoyancy can be included either through a combination of a weak field and strong gradient, or, conversely, a strong field and weak gradient. Each has its own asymptotically consistent reduction, with dedicated governing equations. Our second aim is to address, through a linear stability analysis, under which conditions the standard anelastic system provides a faithful representation of magnetic buoyancy instability. For completeness, we also formulate the energy principle of ideal MHD within the anelastic framework, and demonstrate the relation with its fully compressible counterpart.
- 27 May 2022
- Published by Cambridge University Press (CUP) in Journal of Fluid Mechanics
- Vol. 942
Open AccessMagnetic buoyancy instability and the anelastic approximation: regime of validity and relationship with compressible and Boussinesq descriptions
Magnetic buoyancy instability, which is of astrophysical importance, results from the influence of magnetic pressure variations on the density of a fluid in a gravitational field. It is inherently a compressible phenomenon and is, as such, fully described by the equations of compressible magnetohydrodynamics (MHD). For analytical and computational reasons, it is often convenient to study compressible MHD within simpler, asymptotically consistent reduced systems; the two most widely used result from the Boussinesq and anelastic approximations. Within the standard Boussinesq approximation of MHD, leading to the equations of Boussinesq magnetoconvection, magnetic buoyancy is excluded. It can, however, be included by a rescaling of the basic-state variables and by making further assumptions about the perturbation length scales. Within the anelastic approximation, no special measures are taken to incorporate magnetic buoyancy. It is, however, a priori unclear as to whether this neglect is justified, particularly in the light of the Boussinesq results. Our aims here are thus twofold. The first is to formulate the relationship between descriptions of magnetic buoyancy in the compressible, anelastic and Boussinesq systems. In so doing, we show that, under both the anelastic and Boussinesq approximations, magnetic buoyancy can be included either through a combination of a weak field and strong gradient, or, conversely, a strong field and weak gradient. Each has its own asymptotically consistent reduction, with dedicated governing equations. Our second aim is to address, through a linear stability analysis, under which conditions the standard anelastic system provides a faithful representation of magnetic buoyancy instability. For completeness, we also formulate the energy principle of ideal MHD within the anelastic framework, and demonstrate the relation with its fully compressible counterpart.
- 1 July 2020
- Published by AIP Publishing in Physics of Plasmas
- Vol. 27 (7) , 072508
Onset of interchange instability in a coupled core–SOL plasma
The dynamics at the edge of fusion confinement devices is driven by interchange instabilities and involves the motion of plasma across two regions—the “core region” and the scrape-off layer (SOL)—distinguished by whether field lines are, respectively, closed or connected to the wall. Motivated by this phenomenon, we present an extensive linear stability analysis of a two-layer plasma model encompassing the coupled interactions between the region with closed field lines and the SOL. We focus on the effect of varying the particle diffusivity and ion viscosity, revealing the significant variation in the spatial structure of the critical modes. In addition, we have investigated the dependence of the stability threshold on the ratio of the width of the region with closed field lines to that of the SOL; this dependence is strong when the ratio is sufficiently small, but becomes insignificant once the ratio is of order unity.
- 1 July 2020
- Published by AIP Publishing in Physics of Plasmas
- Vol. 27 (7) , 072508
Onset of interchange instability in a coupled core–SOL plasma
The dynamics at the edge of fusion confinement devices is driven by interchange instabilities and involves the motion of plasma across two regions—the “core region” and the scrape-off layer (SOL)—distinguished by whether field lines are, respectively, closed or connected to the wall. Motivated by this phenomenon, we present an extensive linear stability analysis of a two-layer plasma model encompassing the coupled interactions between the region with closed field lines and the SOL. We focus on the effect of varying the particle diffusivity and ion viscosity, revealing the significant variation in the spatial structure of the critical modes. In addition, we have investigated the dependence of the stability threshold on the ratio of the width of the region with closed field lines to that of the SOL; this dependence is strong when the ratio is sufficiently small, but becomes insignificant once the ratio is of order unity.
- 28 October 2019
- Published by American Physical Society (APS) in Physical Review Fluids
- Vol. 4 (10) , 103502
Stability of two-layer miscible convection
The dynamics at the edge of fusion confinement devices involves the motion of plasma across two regions—the core and the scrape-off layer—that may have very different properties. Motivated by this problem, and exploiting the analogy between the equations governing plasma interchange dynamics and those of classical Rayleigh-Bénard convection, we consider the linear stability of two-dimensional, two-layer miscible convection. We focus specifically on the influence of three particular parameters: the ratio of the viscosities in the two layers, the ratio of the thermal diffusivities, and the ratio of the depths of the two layers. The key result is that, depending on the parameters of the problem, the most unstable mode can take one of three quite distinct forms: whole layer solutions, in which the eigenfunctions of the stream function and temperature extend over both layers of fluid; localized solutions, with the velocity cells or the temperature perturbation (or both) confined to just one of the layers; and segregated solutions, in which the fluid motion and temperature perturbation are confined to different fluid layers.
- 28 October 2019
- Published by American Physical Society (APS) in Physical Review Fluids
- Vol. 4 (10) , 103502
Stability of two-layer miscible convection
The dynamics at the edge of fusion confinement devices involves the motion of plasma across two regions—the core and the scrape-off layer—that may have very different properties. Motivated by this problem, and exploiting the analogy between the equations governing plasma interchange dynamics and those of classical Rayleigh-Bénard convection, we consider the linear stability of two-dimensional, two-layer miscible convection. We focus specifically on the influence of three particular parameters: the ratio of the viscosities in the two layers, the ratio of the thermal diffusivities, and the ratio of the depths of the two layers. The key result is that, depending on the parameters of the problem, the most unstable mode can take one of three quite distinct forms: whole layer solutions, in which the eigenfunctions of the stream function and temperature extend over both layers of fluid; localized solutions, with the velocity cells or the temperature perturbation (or both) confined to just one of the layers; and segregated solutions, in which the fluid motion and temperature perturbation are confined to different fluid layers.
- 1 February 2019
- Published by AIP Publishing in Physics of Plasmas
- Vol. 26 (2) , 022510
Stability of scrape-off layer plasma: A modified Rayleigh–Bénard problem
We present an extensive linear stability analysis of a two-dimensional fluid model used to study the plasma dynamics in the scrape-off layer of tokamaks. The model equations are based on the Braginskii fluid equations under the assumptions of drift ordering and electrostatic plasma. The model also employs the commonly used slab geometry approximation, whereby the magnetic field is assumed constant and straight, with the effects of curvature reintroduced as effective gravitational terms. We study the linear instability in the system by solving a boundary value problem, thereby extending previous studies, which focused on a local analysis. Furthermore, we demonstrate that the governing plasma equations for the scrape-off layer can be viewed as describing a thermal convection problem with additional effects. The new features include a non-uniform basic state gradient, linear damping terms, and additional advective terms. We characterize the conditions at the onset of instability and perform an extensive parameter scan to describe how the stability threshold varies as a function of plasma parameters.
- 1 February 2019
- Published by AIP Publishing in Physics of Plasmas
- Vol. 26 (2) , 022510
Stability of scrape-off layer plasma: A modified Rayleigh–Bénard problem
We present an extensive linear stability analysis of a two-dimensional fluid model used to study the plasma dynamics in the scrape-off layer of tokamaks. The model equations are based on the Braginskii fluid equations under the assumptions of drift ordering and electrostatic plasma. The model also employs the commonly used slab geometry approximation, whereby the magnetic field is assumed constant and straight, with the effects of curvature reintroduced as effective gravitational terms. We study the linear instability in the system by solving a boundary value problem, thereby extending previous studies, which focused on a local analysis. Furthermore, we demonstrate that the governing plasma equations for the scrape-off layer can be viewed as describing a thermal convection problem with additional effects. The new features include a non-uniform basic state gradient, linear damping terms, and additional advective terms. We characterize the conditions at the onset of instability and perform an extensive parameter scan to describe how the stability threshold varies as a function of plasma parameters.