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    On the distribution and swim pressure of run-and-tumble particles in confinement

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    The spatial and orientational distribution in a dilute active suspension of non-Brownian run-and-tumble spherical swimmers confined between two planar hard walls is calculated theoretically. Using a kinetic model based on coupled bulk/surface probability density functions, we demonstrate the existence of a concentration wall boundary layer with thickness scaling with the run length, the absence of polarization throughout the channel, and the presence of sharp discontinuities in the bulk orientation distribution in the neighborhood of orientations parallel to the wall in the near-wall region. Our model is also applied to calculate the swim pressure in the system, which approaches the previously proposed ideal-gas behavior in wide channels but is found to decrease in narrow channels as a result of confinement. Monte-Carlo simulations are also performed for validation and show excellent quantitative agreement with our theoretical predictions

    EstratigrafĂ­a de Sr y evoluciĂłn sedimentaria de los depĂłsitos marinos del Mioceno temprano en el antepaĂ­s del norte de la Cuenca Austral (o Magallanes), Argentina

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    Early Miocene shallow marine deposits in the region of Lago Posadas-Meseta Belgrano (Argentina) represent part of the “Patagoniense” transgression, an Atlantic marine incursion that flooded large part of Patagonia, including the Austral (foreland) Basin (southern Patagonia). These deposits, referred as El Chacay (Argentina) or Guadal (Chile) formations, and the transition to the overlying Santa Cruz Formation were divided into six facies: subtidal sandbars, shallow marine sandy deposits, muddy shelf deposits, estuarine complex deposits, fluvial channels and fluvial floodplains. These are arranged in a general transgressive-regressive cycle, subdivided into two stratigraphic sequences, separated by a major erosional surface. 87Sr/86Sr ages from shell carbonate in eight oysters yielded an age range of 20.3 to 18.1 Ma for these “Patagoniense” deposits. Correlation with other dated “Patagoniense” sections in southern Patagonia, like those at Lago Argentino or Comodoro Rivadavia, indicates that they belong to a single transgression that flooded several Patagonian basins approximately at the same time. Eustasy, flexural subsidence created by tectonic loading in the adjacent fold-and-thrust belt, and basin floor paleo-topography controlled the duration of the depositional event and the sedimentation style of these shallow marine deposits.Los depĂłsitos marino-someros del Mioceno temprano de la regiĂłn del Lago Posadas-Meseta Belgano representan parte de la transgresiĂłn “Patagoniense”, una incursiĂłn marina atlĂĄntica que invadiĂł gran parte de la Patagonia, incluyendo la Cuenca de antepaĂ­s Austral (Patagonia austral). Estos depĂłsitos, referidos como formaciones El Chacay (Argentina) y Guadal (Chile), y su transiciĂłn a la suprayacente FormaciĂłn Santa Cruz, fueron divididos en seis facies: barras submareales, depĂłsitos arenosos marino-someros, depĂłsitos fangosos de plataforma, complejo estuarino, canales fluviales y planicie de inundaciĂłn. Estas facies muestran un arreglo general transgresivo-regresivo, el que puede ser subdividido en dos secuencias estratigrĂĄficas separadas por una superficie erosiva. Resultados de ocho edades 87Sr/86Sr de carbonato tomado de valvas de ostras dieron un rango entre 20,3 Ma y 18,1 Ma para estos depĂłsitos Patagonienses. La correlaciĂłn con sucesiones equivalentes de edad conocida en la Patagonia Austral, como las del Lago Argentino o Comodoro Rivadavia, indican que estas pertenecen a una misma transgresiĂłn que inundĂł gran parte de la Patagonia aproximadamente al mismo tiempo. La eustacia, la subsidencia flexural creada por carga tectĂłnica en la faja corrida y plegada adyacente, y la paleotopografĂ­a del fondo de la cuenca, controlaron la duraciĂłn del evento depositacional y el estilo de sedimentaciĂłn estos depĂłsitos marino-someros.Fil: Cuitiño, JosĂ© Ignacio. Consejo Nacional de Investigaciones CientĂ­ficas y TĂ©cnicas. Centro Nacional PatagĂłnico; ArgentinaFil: Ventura Santos, Roberto. Universidade de BrasĂ­lia; BrasilFil: Alonso Muruaga, Pablo Joaquin. Consejo Nacional de Investigaciones CientĂ­ficas y TĂ©cnicas. Oficina de CoordinaciĂłn Administrativa Ciudad Universitaria. Instituto de Geociencias BĂĄsicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias BĂĄsicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Scasso, Roberto Adrian. Consejo Nacional de Investigaciones CientĂ­ficas y TĂ©cnicas. Oficina de CoordinaciĂłn Administrativa Ciudad Universitaria. Instituto de Geociencias BĂĄsicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias BĂĄsicas, Aplicadas y Ambientales de Buenos Aires; Argentin

    Option-Implied Preferences Adjustments and Risk-Neutral Density Forecasts

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    The main objective of this paper is to analyse the value of information contained in prices of options on the IBEX 35 index at the Spanish Stock Exchange Market. The forward looking information is extracted using implied risk-neutral density functions estimated by a mixture of two-lognormals and three alternative risk-adjustments: the classic power and exponential utility functions and a habit-based specification that allows for a counter-cyclical variation of risk aversion. Our results show that at four-week horizon we can reject the hypothesis that between October 1996 and March 2000 the risk-neutral densities provide accurate predictions of the distributions of future realisations of the IBEX 35 index at a four-week horizon. When forecasting through risk-adjusted densities the performance of this period is statistically improved and we no longer reject that hypothesis. All risk-adjusted densities generate similar forecasting statistics. Then, at least for a horizon of four-weeks, the actual risk adjustment does not seem to be the issue. By contrast, at the one-week horizon risk-adjusted densities do not improve the forecasting ability of the risk-neutral counterparts.forecasting performance, risk adjustment, option implied densities

    Testing the Forecasting Performance of Ibex 35 Option-implied Risk-neutral Densities

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    Published also as: Documento de Trabajo Banco de España 0504/2005.risk-neutral densities, forecasting performance
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