Search results for "R0"

showing 10 items of 62 documents

"Table 5" of "Production properties of D0, D+, D*+ and D(s)+ in 230-GeV/c pi- and K- Cu interactions"

1992

Total cross sections assuming A**1 dependence.

PI- CU --> D*(2010)+ XPI- CU --> D/S- XStrange productionPI- CU --> D*(2010)- XPI- CU --> D/S+ XIntegrated Cross SectionPI- CU --> D+ XCross SectionSIGPI- CU --> DBAR0 XInclusiveCharm productionPI- CU --> D- XPI- CU --> D0 X2.300E+022.300E+02
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"Table 2" of "Charmed pair correlations in pi- Cu interactions at 230-GeV/c."

1993

No description provided.

PI- NUCLEUS --> D+ DBAR0 XPI- NUCLEUS --> D DBAR XStrange productionPI- CU --> D0 DBAR0 XPI- CU --> D+ D- XPI- CU --> D DBAR XPI- NUCLEUS --> DBAR LAMBDA/C+ XYRAPPI- NUCLEUS --> D/S+ DBAR XInclusivePI- CU --> D+ DBAR0 XPI- CU --> D/S+ DBAR XCharm productionPI- CU --> LAMBDA/C+ DBAR XPI- NUCLEUS --> D0 DBAR0 XPI- NUCLEUS --> D+ D- X
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"Table 1" of "Charmed pair correlations in pi- Cu interactions at 230-GeV/c."

1993

FOR ONLY 20 EVENTS IN WICH BOTH DECAYS ARE FULLY RECONSTRUCTED ( 26 D0 , 8 D+ , 5 D/S+ , 1 LAMBDA/C+ CHARMED PARTICLES ).

PI- NUCLEUS --> D+ DBAR0 XStrange productionPI- CU --> D0 DBAR0 XPI- NUCLEUS --> DBAR LAMBDA/C+ XPTMYRAPPI- NUCLEUS --> D/S+ DBAR XInclusivePI- CU --> D+ DBAR0 XPI- CU --> D/S+ DBAR XCharm productionPI- CU --> LAMBDA/C+ DBAR XPI- NUCLEUS --> D0 DBAR0 X
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Least gradient functions in metric random walk spaces

2019

In this paper we study least gradient functions in metric random walk spaces, which include as particular cases the least gradient functions on locally finite weighted connected graphs and nonlocal least gradient functions on $\mathbb{R}^N$. Assuming that a Poincar\'e inequality is satisfied, we study the Euler-Lagrange equation associated with the least gradient problem. We also prove the Poincar\'e inequality in a few settings.

Pure mathematicsControl and Optimization05C81 35R02 26A45 05C21 45C99010102 general mathematicsPoincaré inequalityRandom walk01 natural sciences010101 applied mathematicsComputational Mathematicssymbols.namesakeMathematics - Analysis of PDEsControl and Systems EngineeringMetric (mathematics)FOS: Mathematicssymbols0101 mathematicsAnalysis of PDEs (math.AP)MathematicsESAIM: Control, Optimisation and Calculus of Variations
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Reconstruction of Hamiltonians from given time evolutions

2010

In this paper we propose a systematic method to solve the inverse dynamical problem for a quantum system governed by the von Neumann equation: to find a class of Hamiltonians reproducing a prescribed time evolution of a pure or mixed state of the system. Our approach exploits the equivalence between an action of the group of evolution operators over the state space and an adjoint action of the unitary group over Hermitian matrices. The method is illustrated by two examples involving a pure and a mixed state.

Quantum PhysicsGroup (mathematics)Time evolutionFOS: Physical sciencesState (functional analysis)Group Theory (math.GR)Condensed Matter PhysicsHermitian matrixAtomic and Molecular Physics and OpticsAction (physics)Invers problems time dependent hamiltonian22E70 81R05 93B15Unitary groupQuantum systemFOS: MathematicsState spaceApplied mathematicsQuantum Physics (quant-ph)Mathematics - Group TheoryMathematical PhysicsMathematics
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(Table 1) Sea surface temperature reconstruction for eastern equatorial Pacific surface sediment samples

2012

Significant uncertainties persist in the reconstruction of past sea surface temperatures in the eastern equatorial Pacific, especially regarding the amplitude of the glacial cooling and the details of the post-glacial warming. Here we present the first regional calibration of alkenone unsaturation in surface sediments versus mean annual sea surface temperatures (maSST). Based on 81 new and 48 previously published data points, it is shown that open ocean samples conform to established global regressions of Uk'37 versus maSST and that there is no systematic bias from seasonality in the production or export of alkenones, or from surface ocean nutrient concentrations or salinity. The flattening…

Reference sourceRC23RR9702ASea surface temperatureannual meaninterpolatedV21Roger A RevellePiston corer (BGR type)ME0005Aunsaturation index UK 37VemaKNR182 91988RC18Marion Dufresne (1995)Hakuho MaruKH-03-1MultiCorerTemperaturePiston corer BGR typeAMPHITRITEsediment rockRoger A. RevelleKH 03 1Earth System ResearchLeg138Robert ConradCoreWecomaCalculated from UK 37 Prahl et alPiston corerMoana WaveLongitude of eventHakuho-MaruAlkenone unsaturation index UK'37Thomas WashingtonW7706differenceKNR176-2KNR195-5Leg201DEPTH sediment/rockVNTR01SO147PLDS 3Sea surface temperature annual meanPLDS-3Giant piston corerMW8708MelvilleMD126Marion Dufresne 1995KnorrRC11RC13Event labelJoides ResolutionYALOC69Calculated from UK'37 (Prahl et al. 1988)V19ArgoSonneKNR176 2KNR195 5DEPTHYaquinaKNR182-9Gravity corerTemperature differenceBox corerAlkenoneComposite CoreSCANReference/source
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Riesz transform and vertical oscillation in the Heisenberg group

2023

We study the $L^{2}$-boundedness of the $3$-dimensional (Heisenberg) Riesz transform on intrinsic Lipschitz graphs in the first Heisenberg group $\mathbb{H}$. Inspired by the notion of vertical perimeter, recently defined and studied by Lafforgue, Naor, and Young, we first introduce new scale and translation invariant coefficients $\operatorname{osc}_{\Omega}(B(q,r))$. These coefficients quantify the vertical oscillation of a domain $\Omega \subset \mathbb{H}$ around a point $q \in \partial \Omega$, at scale $r > 0$. We then proceed to show that if $\Omega$ is a domain bounded by an intrinsic Lipschitz graph $\Gamma$, and $$\int_{0}^{\infty} \operatorname{osc}_{\Omega}(B(q,r)) \, \frac{dr}{…

Riesz transformNumerical Analysisintrinsic Lipschitz graphsApplied MathematicsHeisenberg groupFunctional Analysis (math.FA)Mathematics - Functional Analysis42B20 (Primary) 31C05 35R03 32U30 28A78 (Secondary)Mathematics - Classical Analysis and ODEsClassical Analysis and ODEs (math.CA)FOS: MathematicsMathematics::Metric Geometrysingular integralsAnalysis
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Seifert manifolds admitting partially hyperbolic diffeomorphisms

2017

We characterize which 3-dimensional Seifert manifolds admit transitive partially hyperbolic diffeomorphisms. In particular, a circle bundle over a higher-genus surface admits a transitive partially hyperbolic diffeomorphism if and only if it admits an Anosov flow.

Surface (mathematics)Pure mathematicsMathematics::Dynamical SystemsCircle bundle[MATH.MATH-DS]Mathematics [math]/Dynamical Systems [math.DS]Dynamical Systems (math.DS)01 natural sciences[MATH.MATH-GN]Mathematics [math]/General Topology [math.GN]0103 physical sciencesFOS: MathematicsMSC: Primary: 37D30 37C15; Secondary: 57R30 55R05.Mathematics - Dynamical Systems0101 mathematicsMathematics::Symplectic GeometrySeifert spacesMathematics - General TopologyMathematicsTransitive relationAlgebra and Number TheoryApplied Mathematics010102 general mathematicsGeneral Topology (math.GN)Mathematics::Geometric TopologyFlow (mathematics)Partially hyperbolic diffeomorphisms010307 mathematical physicsDiffeomorphismAnalysis
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Ré-adaptation et création dans le mythe de Frankenstein (Mary Shelley, James Whale, Kenneth Branagh)

2010

International audience; Le roman de Mary Shelley (1818), les films de James Whale (dès 1931) ou encore de Terence Fisher (dans les années 50 et 60), sont aussi célèbres qu'étudiés, cas d'école pour qui s'intéresse au fantastique, à l'Âge d'or Hollywoodien et à la question de l'adaptation. Tout ou presque a peut-être déjà été écrit sur les avatars du monstre et de son créateur à l'écran : les écarts de James Whale et la création d'un nouveau mythe ; les exubérances de la Hammer ; enfin, le retour au texte dans le film de Kenneth Branagh (1994). Comment expliquer cette profusion d'adaptations du roman de Shelley ? Pourquoi le public accepta-t-il autant de trahisons du roman ? Plusieurs raison…

[SHS.LITT] Humanities and Social Sciences/Literature[SHS.LITT]Humanities and Social Sciences/LiteratureAPFAPER004030cinémaadaptation[ SHS.LITT ] Humanities and Social Sciences/LiteratureFrankensteinréadaptationlittérature et cinémaFilm Radio Television
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Algebraic models of the real affine plane

2017

We introduce a new invariant, the real (logarithmic)-Kodaira dimension, that allows to distinguish smooth real algebraic surfaces up to birational diffeomorphism. As an application, we construct infinite families of smooth rational real algebraic surfaces with trivial homology groups, whose real loci are diffeomorphic to $\mathbb{R}^2$, but which are pairwise not birationally diffeomorphic. There are thus infinitely many non-trivial models of the real affine plane, contrary to the compact case.

birational diffeomorphismaffine complexificationMathematics::Algebraic Geometry14R05 14R25 14E05 14P25 14J26.affine surface[MATH.MATH-AG] Mathematics [math]/Algebraic Geometry [math.AG]rational fibrationReal algebraic model[MATH.MATH-AG]Mathematics [math]/Algebraic Geometry [math.AG]Mathematics::Symplectic Geometry[ MATH.MATH-AG ] Mathematics [math]/Algebraic Geometry [math.AG]
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