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Erik Martens

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Curriculum Vitae and Research
Academic background
Publications
  1. Exact Results for the Kuramoto Model with a Bimodal Frequency Distribution
    Phys. Rev. E, Vol. 79, No.2 (2009), arXiv:0809.2129
    E. A. Martens, E. Barreto, S. H. Strogatz, E. Ott, P. So and T. Antonsen

  2. Cooperative Behavior in Networks of Coupled Oscillators
    Ph.D. thesis, Cornell University (2009)

  3. Solvable Model of a Spiral Wave Chimeras
    Phys. Rev. Lett., Vol. 104, 044101 (2010), arXiv:0910.5389
    E. A. Martens, C. R. Laing and S. H. Strogatz

  4. Bistable Chimerae on a Triangular Network of Oscillator Populations
    (to be submitted)
    E. A. Martens

  5. Chimerae in a Network of Three Oscillator Populations with Varying Network Topology
    (to be submitted)
    E. A. Martens

  6. A Model for Polygonal Hydraulic Jumps: I. Static Solutions
    (in preparation)
    With T. Bohr, S. Watanabe, J. Rønby, K.S. Hansen, D. Jørgensen, B. Toldbod and J. Larsen
Talks & Poster Presentations
  1. Statistical Physics / Theory of Chaos Group (Arkady Pikovsky), University of Potsdam, Germany, January 2010:
    Invited talk: Chimera States in 2D Nonlocally Coupled Oscillator Systems

  2. FOR 608 Nonlineary Dynamics, University of Bayreuth, Germany, October 2009:
    Talk: Coexistence of Synchronized and Desynchronized States in Nonlocally Coupled Oscillator Systems

  3. Dynamics Days Europe, Gottingen, August 2009:
    Talk: Coexistence of Synchronized and Desynchronized States in Coupled Oscillators

  4. SIAM Conference on Applications of Dynamical Systems, Snowbird, May 17 2009:
    Talk: Kuramoto Model with Bimodal Distribution (minisymposium)

  5. Fluid Dynamics Group (Paul Steen), Chemical Engineering, Cornell University, Ithaca, November 2008
    Invited Talk: Pattern Formation in Fluids

  6. Complex Motions in Fluids, Summer School at Krogerup Højskole, Denmark
    Talk: The Hydraulic Jump and Its Polygonal Regime

  7. Gordon Conference, Nonlinear Science 2005:
    Poster: Pattern Formation in Fluids: Polygonal Hydraulic Jumps
Scientific Interests
Current Research
Studies In networks of coupled oscillators often assume that every unit is coupled globally (with equal strength), or then, only locally (only via their nearest neighbors). But what happens in the intermediate, nonlocal case? This question can be addressed by introducing a coupling strength that attenuates depending on the distance of the oscillators in a network, e.g.,
sideview
We consider phase oscillator systems of the Kuramoto type, i.e.,
sideview
The entities are here defined as follows:
sideview
If we have a finite set of populations corresponding to spatial locations on a ring, we find so-called chimera states:

sideview

The x-axis represents the spatial coordinate (or population), and the y-axis corresponds to the phase of individual oscillators. Populations are represented by the 'slots' delineated by red vertical lines, inhabited by a number of oscillators. One can clearly distinguish that the oscillators form two groups, one of which is phase-locked (left and right), and the other one is oscillating in an incoherent fashion (center). Surprisingly, this state of coexisting synchronized and desynchronized oscillators is stable! It can be shown to be born through a saddle-node bifurcation. For many of these systems we also see that such a state may undergo a further transition characterized by a supercritical Hopf. These states are referred to as breathing chimeras due to their periodic reappearance.

Questions:

sideview
Impinging jet on flat surface. The flow separation occurs after the jump, and is indicated by the smaller of the two circles; the larger one indicates the roller vortex structure as it may appear for Type II jumps.

A stationary hydraulic jump forms when a liquid jet with circular cross section impinges on a flat surface and a steady open surface flow is established. Liquid jet impingement is not only of particular interest for the cooling of technical devices, but also of fundamental physical interest. The flow changes from supercritical to subcritical at a critical radius where typically a circular jump is formed and flow separation occurs. It is observed that the jump undergoes a transition from this circular structure (Type I) to more complex structures (Type II) featuring a roller similar to a stationary breaking wave. As flow parameters are changed, the symmetry may be broken spontaneously and polygons form (reported in Ellegaard et al., Nature 392, 767 (1998)).
jump transition
Transition from so-called Type I jump with separation vortex to Type II jump with roller structure at the surface.

Matching of polygonal hydraulic jump shapes

A phenomenological ODE model of the Type II jump was developed and analysed (with T.Bohr, S.Watanabe and RUC). The forces that act on the roller such as viscosity, hydrostatic pressure and surface tension, are incorporated. We find that the model reproduces circular as well as polygonal structures, of both convex and concave shapes, in agreement with measured phase diagrams. Coexisting solutions for constant flow parameters are also found which indicate the possibility of hysteretical effects as observed in experiments.

Below, four examples of polygonal jumps are displayed and compared with shapes that are obtained as a result of the theoretical model that I have been working on during my Master's thesis. The pictures taken from experiments (C. Ellegaard et al.) are shown on the left; they are taken from below the impact plate and thus correspond to the projection of the vertical jet axis onto the horizontal plane.

Experimentally observed jumps
(Ellegaard et al., Nonlinearity 12 (1999), 1-12)

Shapes produced by mathematical model
(E.Martens)

2-cornered polygon (lens shaped)
2-cornered polygon (lens shaped)
Jump with two corners

3-cornered polygon
3-cornered polygon
Three-sided jump

5-cornered polygon
5-cornered polygon
5-cornered polygon

8-cornered polygon
8-cornered polygon
Octogon



hexagon
bowtie
Hexagon in water. It is hard to stabilize noncircular structures in low viscosity fluids, but this hexagonal structure was observed in water in a pretty stable mode (E.Martens, TSL M&AE Cornell University). Bowties and clover structures were first observed in John Bush's group at MIT (Viscous Hydraulic Jumps (Physics of Fluids (2004), 16 - 9). This picture of a bowtie was taken at my own lab (TSL, Mech. & Aer. Eng., Cornell University) using green anti freeze.

Questions:
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