12,447 research outputs found

    Dilaton-Axion hair for slowly rotating Kerr black holes

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    Campbell et al. demonstrated the existence of axion ``hair'' for Kerr black holes due to the non-trivial Lorentz Chern-Simons term and calculated it explicitly for the case of slow rotation. Here we consider the dilaton coupling to the axion field strength, consistent with low energy string theory and calculate the dilaton ``hair'' arising from this specific axion source.Comment: 13 pages + 1 fi

    The Cytology of Caltha L.

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    A Comparison of the Hyde and Durham Air-borne Pollen Collecting Shelters

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    Determination of electromagnetic medium from the Fresnel surface

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    We study Maxwell's equations on a 4-manifold where the electromagnetic medium is described by an antisymmetric (22)2\choose 2-tensor Îș\kappa. In this setting, the Tamm-Rubilar tensor density determines a polynomial surface of fourth order in each cotangent space. This surface is called the Fresnel surface and acts as a generalisation of the light-cone determined by a Lorentz metric; the Fresnel surface parameterises electromagnetic wave-speed as a function of direction. Favaro and Bergamin have recently proven that if Îș\kappa has only a principal part and if the Fresnel surface of Îș\kappa coincides with the light cone for a Lorentz metric gg, then Îș\kappa is proportional to the Hodge star operator of gg. That is, under additional assumptions, the Fresnel surface of Îș\kappa determines the conformal class of Îș\kappa. The purpose of this paper is twofold. First, we provide a new proof of this result using Gr\"obner bases. Second, we describe a number of cases where the Fresnel surface does not determine the conformal class of the original (22)2\choose 2-tensor Îș\kappa. For example, if Îș\kappa is invertible we show that Îș\kappa and Îș−1\kappa^{-1} have the same Fresnel surfaces.Comment: 23 pages, 1 figur

    Variation of Loess Thickness and Clay Content in Southern Iowa

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    This report summarizes two aspects of the Wisconsin loess in southern Iowa and presents some information on the sandy-silt immediately underlying the loess and overlying the till in southcentral Iowa. The data has originated from project work done over the last five year on the loess and glacial till of Iowa (Project 283-S) in .an attempt to solve the problem of stabilization of loess and till for roads. This paper incorporates data procured to date on the loess of southwest, southern and east-central Iowa and present studies in progress in south-central Iowa. (See references 1, 2, 3 and 4.

    Evolutionary Approaches to Optimization Problems in Chimera Topologies

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    Chimera graphs define the topology of one of the first commercially available quantum computers. A variety of optimization problems have been mapped to this topology to evaluate the behavior of quantum enhanced optimization heuristics in relation to other optimizers, being able to efficiently solve problems classically to use them as benchmarks for quantum machines. In this paper we investigate for the first time the use of Evolutionary Algorithms (EAs) on Ising spin glass instances defined on the Chimera topology. Three genetic algorithms (GAs) and three estimation of distribution algorithms (EDAs) are evaluated over 10001000 hard instances of the Ising spin glass constructed from Sidon sets. We focus on determining whether the information about the topology of the graph can be used to improve the results of EAs and on identifying the characteristics of the Ising instances that influence the success rate of GAs and EDAs.Comment: 8 pages, 5 figures, 3 table

    Reconstructing the phytoplankton community of the Cariaco Basin during the Younger Dryas cold event using chlorin steryl esters

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    Author Posting. © American Geophysical Union, 2004. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 19 (2004): PA01006, doi:10.1029/2003PA000907.A record of the downcore distribution of chlorin steryl esters (CSEs) through the Younger Dryas was produced from Cariaco Basin sediments in order to assess the potential use of CSEs as recorders of the structure of phytoplankton communities through time. Using an improved high-performance liquid chromatography method for the separation of CSEs, we find significant changes in the distribution of CSEs during the Younger Dryas in the Cariaco Basin. During the Younger Dryas, enhanced upwelling in the Cariaco Basin caused an increase in the diatom population and therefore an increase in the relative abundance of CSEs derived from diatoms. In contrast, the dinoflagellate population, and therefore CSEs derived from dinoflagellates, decreased in response to the climate change during the Younger Dryas. These community shifts agree well with the shifts observed in the present day on a seasonal basis that result from the north-south migration of the Intertropical Convergence Zone over the Cariaco Basin. We also identify changes in the abundance of several CSEs that seem to reflect rapid warming and cooling events. This study suggests that CSEs are useful proxies for reconstructing phytoplankton communities and paleoenvironments.This work was supported by the Chemical Oceanography Division of the National Science Foundation and a WHOI Watson Fellowship (to KAD)

    Further Studies of Loess in Iowa: Thickness, Clay Content, and Engineering Classification

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    This paper is a continuation of the work previously reported by Dahl, Handy and Davidson (1), and summarizes currently available information on properties of the Wisconsin loess. New areas of investigation are in northwest and eastern Iowa. Depth measurements and samples in the bluffs region were obtained mostly from the traverses of Hutton (2) and Davidson, et al. (3). Riggs (4) continued these traverses and the northwest-southeast traverses of Lyon, et al. (5), and established a grid-like sample pattern in southwest Iowa. Dahl (6) and Hansen (7) extended the grid eastward to the Mississippi River. Data on northwest Iowa was obtained from the east-west traverses initiated by Davidson (8)
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