392 research outputs found

    Maxwell demons in phase space

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    Although there is not a complete "proof" of the second law of thermo- dynamics based on microscopic dynamics, two properties of Hamiltonian systems have been used to prove the impossibility of work extraction from a single thermal reservoir: Liouville's theorem and the adiabatic invariance of the volume enclosed by an energy shell. In this paper we analyze these two properties in the Szilard engine and other systems related with the Maxwell demon. In particular, we recall that the enclosed volume is no longer an adiabatic invariant in non ergodic systems and explore the consequences of this on the second law.Comment: 14 pages, to appear in EPJS

    Thermodynamic costs of information processing in sensory adaption

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    Biological sensory systems react to changes in their surroundings. They are characterized by fast response and slow adaptation to varying environmental cues. Insofar as sensory adaptive systems map environmental changes to changes of their internal degrees of freedom, they can be regarded as computational devices manipulating information. Landauer established that information is ultimately physical, and its manipulation subject to the entropic and energetic bounds of thermodynamics. Thus the fundamental costs of biological sensory adaptation can be elucidated by tracking how the information the system has about its environment is altered. These bounds are particularly relevant for small organisms, which unlike everyday computers operate at very low energies. In this paper, we establish a general framework for the thermodynamics of information processing in sensing. With it, we quantify how during sensory adaptation information about the past is erased, while information about the present is gathered. This process produces entropy larger than the amount of old information erased and has an energetic cost bounded by the amount of new information written to memory. We apply these principles to the E. coli's chemotaxis pathway during binary ligand concentration changes. In this regime, we quantify the amount of information stored by each methyl group and show that receptors consume energy in the range of the information-theoretic minimum. Our work provides a basis for further inquiries into more complex phenomena, such as gradient sensing and frequency response.Comment: 17 pages, 6 figure

    Évolution de la gĂ©omorphologie depuis la fin du XIXe siĂšcle

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    Jusque dans les annĂ©es 1940, ce sont des gĂ©ologues qui s’intĂ©ressent Ă  la physiographie, car la gĂ©omorphologie ne fait pas encore partie de la formation universitaire en gĂ©ographie au QuĂ©bec. Les premiers dĂ©partements de gĂ©ographie sont crĂ©Ă©s Ă  la fin des annĂ©es 1940 et les premiĂšres publications en gĂ©omorphologie apparaissent au milieu des annĂ©es 1950. Les gĂ©ographes sont davantage prĂ©occupĂ©s par la gĂ©omorphologie dynamique que par la physiographie. L’institutionnalisation de la gĂ©omorphologie commence au milieu des annĂ©es 1960 alors que les annĂ©es 1970 marquent le dĂ©but de l’apogĂ©e de la gĂ©omorphologie avec l’expansion du rĂ©seau de l’enseignement universitaire et la crĂ©ation de laboratoires, confirmant le passage d’une gĂ©omorphologie descriptive Ă  une gĂ©omorphologie quantitative. Les dĂ©cennies 1970 et 1980 sont caractĂ©risĂ©es par la prolifĂ©ration des recherches dans tous les domaines de la gĂ©omorphologie dynamique. C’est la pĂ©riode durant laquelle bon nombre de gĂ©omorphologues sont engagĂ©s par des organismes gouvernementaux ainsi que par des firmes d’ingĂ©nieurs et d’environnementalistes pour rĂ©aliser des inventaires rĂ©gionaux. L’utilisation d’ordinateurs personnels au milieu des annĂ©es 1980 et de SIG depuis le dĂ©but des annĂ©es 1990, combinĂ©s Ă  de meilleurs outils d’observation de la Terre, a favorisĂ© l’émergence d’une nouvelle gĂ©omorphologie axĂ©e sur la modĂ©lisation des processus. Toutefois, une ombre au tableau demeure : la rĂ©cente disparition de plusieurs programmes de formation en gĂ©ographie physique au niveau universitaire. L’avenir de la gĂ©omorphologie rĂ©side dans une optimisation des outils d’observation, de mesure et de prĂ©diction.Since the 1940s, physiography had been the sole interest of geologists, since geomorphology was not part of the geography curriculum at Quebec universities at that time. Geography departments were not set up until the late 1940s and geomorphology publications first appeared in the mid-1950s. Geographers were drawn more to dynamic geomorphology than to physiography. The institutionalization of geomorphology began in the mid-1960s, whereas the 1970s marked the “golden age” of geomorphology, when the university network was expanded, laboratories built, and descriptive geomorphology superseded by its quantitative counterpart. During the 1970s and 1980s, research in all fields of dynamic geomorphology proliferated. At the same time a large number of geomorphologists were hired by government agencies and engineering and environmental firms to carry out regional inventories. The use of PCs in the mid-1980s and GIS from the early 1990s, combined with the availability of more sophisticated Earth observation tools, led to the emergence of a new kind of geomorphology focused on process modelling management. However, the recent closure of several university physical geography programs in the Quebec university system has cast a shadow over the future of geomorphology, which now depends on the optimization of observation, measurement and prediction tools.Hasta los años 1940, son los geĂłlogos que se interesan a la fisiografĂ­a, puesto que en Quebec la GeomorfologĂ­a todavĂ­a no hace parte de la formaciĂłn universitaria en GeografĂ­a. Los primeros departamentos de GeografĂ­a fueron creados a fines de los años 1940 y las primeras publicaciones en GeomorfologĂ­a aparecieron a mediados de los años 1950. Los geĂłgrafos estĂĄn mĂĄs preocupados por la GeomorfologĂ­a dinĂĄmica que por la fisiografĂ­a. La institucionalizaciĂłn de la GeomorfologĂ­a comienza a mediados de los años 1960, mientras que los años 1970 marcan el comienzo de su apogeo debido a la expansiĂłn de la red de enseñanza universitaria y la creaciĂłn de laboratorios, confirmando el pasaje de una GeomorfologĂ­a descriptiva a una GeomorfologĂ­a cuantitativa. Los decenios 1970 y 1980 se caracterizan por la profusiĂłn de investigaciones en todos los campos de la GeomorfologĂ­a dinĂĄmica. Es en este periodo que numerosos geomorfĂłlogos son contratados por organismos gubernamentales y empresas de ingenieros y medio-ambientistas para realizar inventarios regionales. La utilizaciĂłn de computadoras personales, a mediados de los años 1980, y del SIG, desde comienzos de los años 1990, combinados con mejores Ăștiles de observaciĂłn de la Tierra, ha favorecido la emergencia de una nueva GeomorfologĂ­a orientada hacia la modelizaciĂłn de procedimientos. No obstante, queda un punto oscuro : la reciente desapariciĂłn de varios programas de formaciĂłn universitaria en GeografĂ­a FĂ­sica. El futuro de la GeomorfologĂ­a reside en el perfeccionamiento de sus Ăștiles de observaciĂłn, de medidas y de predicciĂłn

    The thermodynamic cost of measurements

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    The measurement of thermal fluctuations provides information about the microscopic state of a thermodynamic system and can be used in order to extract work from a single heat bath in a suitable cyclic process. We present a minimal framework for the modeling of a measurement device and we propose a protocol for the measurement of thermal fluctuations. In this framework, the measurement of thermal fluctuations naturally leads to the dissipation of work. We illustrate this framework on a simple two states system inspired by the Szilard's information engine

    Numerical simulation of model problems in plasticity based on field dislocation mechanics

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    The aim of this paper is to investigate the numerical implementation of the field dislocation mechanics (FDM) theory for the simulation of dislocation-mediated plasticity. First, the mesoscale FDM theory of Acharya and Roy (2006 J. Mech. Phys. Solids 54 1687-710) is recalled which permits to express the set of equations under the form of a static problem, corresponding to the determination of the local stress field for a given dislocation density distribution, complemented by an evolution problem, corresponding to the transport of the dislocation density. The static problem is solved using FFT-based techniques (Brenner et al 2014 Phil. Mag. 94 1764-87). The main contribution of the present study is an efficient numerical scheme based on high resolution Godunov-type solvers to solve the evolution problem. Model problems of dislocation-mediated plasticity are finally considered in a simplified layer case. First, uncoupled problems with uniform velocity are considered, which permits to reproduce annihilation of dislocations and expansion of dislocation loops. Then, the FDM theory is applied to several problems of dislocation microstructures subjected to a mechanical loading

    Aerodynamic measurement and analysis of the flow in an uncooled turbine stage

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    Thesis (M.S.)--Massachusetts Institute of Technology, Dept. of Aeronautics and Astronautics, 1998.Includes bibliographical references (p. 125-127).by Léo M. Grépin.M.S

    Finite self-similar p-groups with abelian first level stabilizers

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    We determine all finite p-groups that admit a faithful, self-similar action on the p-ary rooted tree such that the first level stabilizer is abelian. A group is in this class if and only if it is a split extension of an elementary abelian p-group by a cyclic group of order p. The proof is based on use of virtual endomorphisms. In this context the result says that if G is a finite p-group with abelian subgroup H of index p, then there exists a virtual endomorphism of G with trivial core and domain H if and only if G is a split extension of H and H is an elementary abelian p-group.Comment: one direction of theorem 2 extended to regular p-group

    Electric-field tuning of the valley splitting in silicon corner dots

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    We perform an excited state spectroscopy analysis of a silicon corner dot in a nanowire field-effect transistor to assess the electric field tunability of the valley splitting. First, we demonstrate a back-gate-controlled transition between a single quantum dot and a double quantum dot in parallel that allows tuning the device in to corner dot formation. We find a linear dependence of the valley splitting on back-gate voltage, from 880 ΌeV880~\mu \text{eV} to 610 ΌeV610~\mu \text{eV} with a slope of −45±3 ΌeV/V-45\pm 3~\mu \text{eV/V} (or equivalently a slope of −48±3 ΌeV/(MV/m)-48\pm 3~\mu \text{eV/(MV/m)} with respect to the effective field). The experimental results are backed up by tight-binding simulations that include the effect of surface roughness, remote charges in the gate stack and discrete dopants in the channel. Our results demonstrate a way to electrically tune the valley splitting in silicon-on-insulator-based quantum dots, a requirement to achieve all-electrical manipulation of silicon spin qubits.Comment: 5 pages, 3 figures. In this version: Discussion of model expanded; Fig. 3 updated; Refs. added (15, 22, 32, 34, 35, 36, 37
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