Krzysztof Mizerski

Dr. Krzysztof Mizerski

Zakład Magnetyzmu (Geoelektromagnetyzm), Instytut Geofizyki Polskiej Akademii Nauk, ul. Ksiecia Janusza 64, 01-452 Warszawa, Poland
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Research Focus & Metrics

Academic Career Length

20Years (2007-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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28 August 2013 in Journal of Fluid Mechanics
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EWEligiusz Wajnryb
Eligiusz Wajnryb
Krzysztof MizerskiKrzysztof Mizerski
Krzysztof Mizerski
PŻPaweł J. Żuk
Paweł J. Żuk
Piotr SzymczakPiotr Szymczak
Piotr Szymczak
The Rotne–Prager–Yamakawa approximation is one of the most commonly used methods of including hydrodynamic interactions in modelling of colloidal suspensions and polymer solutions. The two main merits of this approximation are that it includes all long-range terms (i.e. decaying as ${R}^{- 3} $ or slower in interparticle distances) and that the diffusion matrix is positive definite, which is essential for Brownian dynamics modelling. Here, we extend the Rotne–Prager–Yamakawa approach to include both translational and rotational degrees of freedom, and derive the regularizing corrections to account for overlapping particles. Additionally, we show how the Rotne–Prager–Yamakawa approximation can be generalized for other geometries and boundary conditions.

11 February 2014 in Journal of Fluid Mechanics
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PŻPaweł J. Żuk
Paweł J. Żuk
EWE. Wajnryb
E. Wajnryb
Krzysztof MizerskiKrzysztof Mizerski
Krzysztof Mizerski
Piotr SzymczakPiotr Szymczak
Piotr Szymczak
The Rotne–Prager–Yamakawa (RPY) approximation is a commonly used approach to model the hydrodynamic interactions between small spherical particles suspended in a viscous fluid at a low Reynolds number. However, when the particles overlap, the RPY tensors lose their positive definiteness, which leads to numerical problems in the Brownian dynamics simulations as well as errors in calculations of the hydrodynamic properties of rigid macromolecules using bead modelling. These problems can be avoided by using regularizing corrections to the RPY tensors; so far, however, these corrections have only been derived for equal-sized particles. Here we show how to generalize the RPY approach to the case of overlapping spherical particles of different radii and present the complete set of mobility matrices for such a system. In contrast to previous ad hoc approaches, our method relies on the direct integration of force densities over the sphere surfaces and thus automatically provides the correct limiting behaviour of the mobilities for the touching spheres and for a complete overlap, with one sphere immersed in the other one. This approach can then be used to calculate hydrodynamic properties of complex macromolecules using bead models with overlapping, different-sized beads, which we illustrate with an example.

27 July 2009 in Journal of Fluid Mechanics
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Krzysztof MizerskiKrzysztof Mizerski
Krzysztof Mizerski
KBK. Bajer
K. Bajer
We address the question of stability of the Euler flow with elliptical streamlines in a rotating frame, interacting with uniform external magnetic field perpendicular to the plane of the flow. Our motivation for this study is of astrophysical nature, since many astrophysical objects, such as stars, planets and accretion discs, are tidally deformed through gravitational interaction with other bodies. Therefore, the ellipticity of the flow models the tidal deformations in the simplest way. The joint effect of the magnetic field and the Coriolis force is studied here numerically and analytically in the limit of small elliptical (tidal) deformations (ζ ≪ 1), using the analytical technique developed by Lebovitz & Zweibel (Astrophys. J., vol. 609, 2004, pp. 301–312). We find that the effect of background rotation and external magnetic field is quite complex. Both factors are responsible for new destabilizing resonances as the vortex departs from axial symmetry (ζ ≪ 1); however, just like in the non-rotating case, there are three principal resonances causing instability in the leading order. The presence of the magnetic field is very likely to destabilize the system with respect to perturbations propagating in the direction of the magnetic field if the basic vorticity and the background rotation have opposite signs (i.e. for anticyclonic background rotation). We present the dependence of the growth rates of the modes on various parameters describing the system, such as the strength of the magnetic field (h), the inverse of the Rossby number (ℛv), the ellipticity of the basic flow (ϵ) and the direction of propagation of modes (ϑ). Our analytical predictions agree well with the numerical calculations.

22 November 2017 in Fluid Dynamics Research
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HMH K Moffatt
H K Moffatt
Krzysztof MizerskiKrzysztof Mizerski
Krzysztof Mizerski
The relaxation of a helical magnetic field B ( x , t ) in a high-conductivity plasma contained in the annulus between two perfectly conducting coaxial cylinders is considered. The plasma is of low density and its pressure is negligible compared with the magnetic pressure; the flow of the plasma is driven by the Lorentz force and energy is dissipated primarily by the viscosity of the medium. The axial and toroidal fluxes of magnetic field are conserved in the perfect-conductivity limit, as is the mass per unit axial length. The magnetic field relaxes during a rapid initial stage to a force-free state, and then decays slowly, due to the effect of weak resistivity η , while constrained to remain approximately force-free. Interest centres on whether the relaxed field may attain a Taylor state; but under the assumed conditions with axial and toroidal flux conserved inside every cylindrical Lagrangian surface, this is not possible. The effect of an additional α -effect associated with instabilities and turbulence in the plasma is therefore investigated in exploratory manner. An assumed pseudo-scalar form of α proportional to q η ( j · B ) is adopted, where j = ∇ × B and q is an ( 1 ) dimensionless parameter. It is shown that, when q is less than a critical value q c , the evolution remains smooth and similar to that for q = 0; but if q > q c , negative-diffusivity effects act on the axial component of B , generating high-frequency rapidly damped oscillations and an associated transitory appearance of reversed axial field. However, the field shows no sign of relaxing to a Taylor state for which the scalar quantity γ = j · B / B 2 would have to be constant.

28 December 2017 in Geophysical & Astrophysical Fluid Dynamics
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Krzysztof MizerskiKrzysztof Mizerski
Krzysztof Mizerski
HMH. K. Moffatt
H. K. Moffatt
Random waves in a uniformly rotating plasma in the presence of a locally uniform seed magnetic field and subject to weak kinematic viscosity ν and resistivity η are considered. These “Lehnert” waves may have either positive or negative helicity, and it is supposed that waves of a single sign of helicity are preferentially excited by a symmetry-breaking mechanism. A mean electromotive force proportional to ν-η is derived, demonstrating the conflicting effects of the two diffusive processes. Attention is then focussed on the situation η=0, relevant to conditions in the universe before and during galaxy formation. An α-effect, axisymmetric about the rotation vector, is derived, decaying on a time-scale proportional to ν-1; this amplifies a large-scale seed magnetic field to a level independent of ν, this field being subsequently steady and having the character of a “fossil field”. Subsequent evolution of this fossil field is briefly discussed.

8 November 2021 in Journal of Fluid Mechanics
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CJChris A. Jones
Chris A. Jones
Krzysztof MizerskiKrzysztof Mizerski
Krzysztof Mizerski
MKMouloud Kessar
Mouloud Kessar
Anelastic convection at high Rayleigh number in a plane parallel layer with no slip boundaries is considered. Energy and entropy balance equations are derived, and they are used to develop scaling laws for the heat transport and the Reynolds number. The appearance of an entropy structure consisting of a well-mixed uniform interior, bounded by thin layers with entropy jumps across them, makes it possible to derive explicit forms for these scaling laws. These are given in terms of the Rayleigh number, the Prandtl number and the bottom to top temperature ratio, which also measures how much the density varies across the layer. The top and bottom boundary layers are examined and they are found to be very different, unlike in the Boussinesq case. Elucidating the structure of these boundary layers plays a crucial part in determining the scaling laws. Physical arguments governing these boundary layers are presented, concentrating on the case in which the boundary layers are so thin that temperature and density vary little across them, even though there may be substantial temperature and density variations across the whole layer. Different scaling laws are found, depending on whether the viscous dissipation is primarily in the boundary layers or in the bulk. The cases of both high and low Prandtl number are considered. Numerical simulations of no-slip anelastic convection up to a Rayleigh number of $10^7$ have been performed and our theoretical predictions are compared with the numerical results.