1,848 research outputs found

    Analytical approach to directed sandpile models on the Apollonian network

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    We investigate a set of directed sandpile models on the Apollonian network, which are inspired on the work by Dhar and Ramaswamy (PRL \textbf{63}, 1659 (1989)) for Euclidian lattices. They are characterized by a single parameter qq, that restricts the number of neighbors receiving grains from a toppling node. Due to the geometry of the network, two and three point correlation functions are amenable to exact treatment, leading to analytical results for the avalanche distributions in the limit of an infinite system, for q=1,2q=1,2. The exact recurrence expressions for the correlation functions are numerically iterated to obtain results for finite size systems, when larger values of qq are considered. Finally, a detailed description of the local flux properties is provided by a multifractal scaling analysis.Comment: 7 pages in two-column format, 10 illustrations, 5 figure

    Transverse instability of dunes

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    The simplest type of dune is the transverse one, which propagates with invariant profile orthogonally to a fixed wind direction. Here we show numerically and with a linear stability analysis that transverse dunes are unstable with respect to along-axis perturbations in their profile and decay on the bedrock into barchan dunes. Any forcing modulation amplifies exponentially with growth rate determined by the dune turnover time. We estimate the distance covered by a transverse dune before fully decaying into barchans and identify the patterns produced by different types of perturbation.Comment: 4 pages, 3 figures; To appear in Physical Review Letter

    Numerical modeling of the wind flow over a transverse dune

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    Transverse dunes, which form under unidirectional winds and have fixed profile in the direction perpendicular to the wind, occur on all celestial objects of our solar system where dunes have been detected. Here we perform a numerical study of the average turbulent wind flow over a transverse dune by means of computational fluid dynamics simulations. We find that the length of the zone of recirculating flow at the dune lee --- the {\em{separation bubble}} --- displays a surprisingly strong dependence on the wind shear velocity, u∗u_{\ast}: it is nearly independent of u∗u_{\ast} for shear velocities within the range between 0.2 0.2\,ms and $0.8\,$ms but increases linearly with u∗u_{\ast} for larger shear velocities. Our calculations show that transport in the direction opposite to dune migration within the separation bubble can be sustained if u∗u_{\ast} is larger than approximately 0.39 0.39\,ms, whereas a larger value of $u_{\ast}$ (about $0.49\,$ms) is required to initiate this reverse transport.Comment: 11 pages, 8 figure

    Spreading gossip in social networks

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    We study a simple model of information propagation in social networks, where two quantities are introduced: the spread factor, which measures the average maximal fraction of neighbors of a given node that interchange information among each other, and the spreading time needed for the information to reach such fraction of nodes. When the information refers to a particular node at which both quantities are measured, the model can be taken as a model for gossip propagation. In this context, we apply the model to real empirical networks of social acquaintances and compare the underlying spreading dynamics with different types of scale-free and small-world networks. We find that the number of friendship connections strongly influences the probability of being gossiped. Finally, we discuss how the spread factor is able to be applied to other situations.Comment: 10 pages, 16 figures, Revtex; Virt.J. of Biol. Phys., Oct.1 200

    Optimal box-covering algorithm for fractal dimension of complex networks

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    The self-similarity of complex networks is typically investigated through computational algorithms the primary task of which is to cover the structure with a minimal number of boxes. Here we introduce a box-covering algorithm that not only outperforms previous ones, but also finds optimal solutions. For the two benchmark cases tested, namely, the E. Coli and the WWW networks, our results show that the improvement can be rather substantial, reaching up to 15% in the case of the WWW network.Comment: 5 pages, 6 figure

    Computational tool for the analysis and simulation of cold room performance in perishable products industry

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    Perishable products such as meat, fruit and dairy products are some of the major food products preferred by consumers due to their nutritional and organoleptic characteristics. The conservation of their properties through time is usually ensured by storing them in rooms with controlled air temperature and humidity. The refrigeration systems that accomplish these environmental conditions are the main responsible by the electrical energy consumption in food sector industries. With the aim to promote an improvement of its energy performance, a computational tool for the analysis and simulation of cold rooms performance was developed. It allows the analysis of the behaviour of relevant parameters, such as: raw material quantity, cold rooms volume, refrigeration systems power, among others. The preliminary results of the practical application of this tool show its usefulness on the decision making for energy efficiency measures to reduce the specific energy consumption in perishable products industry.info:eu-repo/semantics/publishedVersio

    Aeolian transport layer

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    We investigate the airborne transport of particles on a granular surface by the saltation mechanism through numerical simulation of particle motion coupled with turbulent flow. We determine the saturated flux qsq_{s} and show that its behavior is consistent with a classical empirical relation obtained from wind tunnel measurements. Our results also allow to propose a new relation valid for small fluxes, namely, qs=a(u∗−ut)αq_{s}=a(u_{*}-u_{t})^{\alpha}, where u∗u_{*} and utu_{t} are the shear and threshold velocities of the wind, respectively, and the scaling exponent is α≈2\alpha \approx 2. We obtain an expression for the velocity profile of the wind distorted by the particle motion and present a dynamical scaling relation. We also find a novel expression for the dependence of the height of the saltation layer as function of the wind velocity.Comment: 4 pages, 4 figure
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