102,613 research outputs found

    Dr M T Batchelor, Physics

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    L to R: Dr B I Henry and Dr M T Batchelor, Physics awarded first prize from British Institute of Physics in 1990, Beauty of Physics exhibitio

    Kraichnan-Leith-Batchelor similarity theory and two-dimensional inverse cascades

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    We study the scaling properties and Kraichnan-Leith-Batchelor (KLB) theory of forced inverse cascades in generalized two-dimensional (2D) fluids (α\alpha-turbulence models) simulated at resolution 819228192^2. We consider α=1\alpha=1 (surface quasigeostrophic flow), α=2\alpha=2 (2D vorticity dynamics) and α=3\alpha=3. The forcing scale is well-resolved, a direct cascade is present and there is no large-scale dissipation. Coherent vortices spanning a range of sizes, most larger than the forcing scale, are present for both α=1\alpha=1 and α=2\alpha=2. The active scalar field for α=3\alpha=3 contains comparatively few and small vortices. The energy spectral slopes in the inverse cascade are steeper than the KLB prediction (7α)/3-(7-\alpha)/3 in all three systems. Since we stop the simulations well before the cascades have reached the domain scale, vortex formation and spectral steepening are not due to condensation effects; nor are they caused by large-scale dissipation, which is absent. One- and two-point pdfs, hyperflatness factors and structure functions indicate that the inverse cascades are intermittent and non-Gaussian over much of the inertial range for α=1\alpha=1 and α=2\alpha=2, while the α=3\alpha=3 inverse cascade is much closer to Gaussian and non-intermittent. For α=3\alpha=3 the steep spectrum is close to that associated with enstrophy equipartition. Continuous wavelet analysis shows approximate KLB scaling E(k)k2\mathcal{E}(k) \propto k^{-2} (α=1\alpha=1) and E(k)k5/3\mathcal{E}(k) \propto k^{-5/3} (α=2\alpha=2) in the interstitial regions between the coherent vortices. Our results demonstrate that coherent vortex formation (α=1\alpha=1 and α=2\alpha=2) and non-realizability (α=3\alpha=3) cause 2D inverse cascades to deviate from the KLB predictions, but that the flow between the vortices exhibits KLB scaling and non-intermittent statistics for α=1\alpha=1 and α=2\alpha=2. The results will appear in \cite{BurgessEA2015}, which has been accepted to the \emph{Journal of Fluid Mechanics}

    The quantum inverse scattering method with anyonic grading

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    We formulate the quantum inverse scattering method for the case of anyonic grading. This provides a general framework for constructing integrable models describing interacting hard-core anyons. Through this method we reconstruct the known integrable model of hard core anyons associated with the XXX model, and as a new application we construct the anyonic t − J model. The energy spectrum for each model is derived by means of a generalization of the algebraic Bethe ansatz. The grading parameters implementing the anyonic signature give rise to sector-dependent phase factors in the Bethe ansatz equations

    The works of Mr. Congreve : in two volumes; to which is prefixed The Life of the author.

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    v.1. The life of the author. The old batchelor. The double dealer. Love for love. -- v.2. The mourning bride. The way of the world. The judgment of Paris. Semele. Poems on several occasions.Mode of access: Internet

    Steady Prandtl-Batchelor flows past a circular cylinder

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    The high Reynolds number flow past a circular cylinder with a trailing wake region is considered when the wake region is bounded and contains uniform vorticity. The formulation allows only for a single vortex pair trapped behind the cylinder, but calculates solutions over a range of values of vorticity. The separation point and length of the region are determined as outputs. It was found that using this numerical method there is an upper bound on the vorticity for which solutions can be calculated for a given arclength of the cavity. In some cases with shorter cavities, the limiting solutions coincide with the formation of a stagnation point in the outer flow at both separation from the cylinder and reattachment at the end of the cavity

    A. T. Prior

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    "A.T. (Tom) Prior 12 Squadron R.A.A.F. Darwin & Batchelor Dec 1941 - 1943."A.T. (Tom) Prior. 12 Squadron, Royal Australian Air Force. Darwin & Batchelor. December 1941 - 1943.Date:199

    Turbulent super-diffusion as a ballistic cascade

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    Since the pioneering work of Richardson in 1926, later refined by Batchelor and Obukhov in 1950, it is predicted that the rate of separation of pairs of fluid elements in turbulent flows with initial separation at inertial scales, grows ballistically first (Batchelor regime), before undergoing a transition towards a super-diffusive regime where the mean-square separation grows as t3t^3 (Richardson regime). Richardson empirically interpreted this super-diffusive regime in terms of a non-Fickian process with a scale dependent diffusion coefficient (the celebrated Richardson's ``4/3rd'' law). However, the actual physical mechanism at the origin of such a scale dependent diffusion coefficient remains unclear. The present work proposes a simple physical phenomenology for the Richardson super-diffusivity in turbulence based on a scale dependent \emph{ballistic} scenario rather than a scale dependent \emph{diffusive} scenario. It is shown that this phenomenology elucidates several aspects of turbulent dispersion: (i) it gives a simple physical explanation of the origin of the super diffusive t3t^3 Richardson regime as an iterative cascade of scale-dependent ballistic separations, (ii) it simply relates the Richardson constant to the Kolmogorov constant (and eventually to a ballistic persistence parameter), (iii) it gives a simple physical interpretation of the non-Fickian scale-dependent diffusivity coefficient as originally proposed by Richardson and (iv) a further extension of the phenomenology, taking into account higher order corrections to the local ballisitic motion, gives a robust interpretation of the assymetry between forward and backward dispersion, with an explicit connection to the energy flux accross scales

    Batchelor Road CH 8.4 km to CH 10.9 km geotechnical investigation

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    This factual report presents the results of a geotechnical investigation of sites along the Batchelor Road between chainages 8.4km and 10.9km. This report details the scope of work carried out and provides results of field and laboratory testing.Made available by the Northern Territory Library via the Publications (Legal Deposit) Act 2004 (NT).Introduction -- Scope of works -- Results -- Limitations -- Appendix A-

    Letter, [Author unclear] to Paulina T. Merritt

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    Handwritten letter to Paulina Merritt from an unknown author, October 1, 1876.
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