Silicon intercalation into the graphene-SiC interface

In this work we use LEEM, XPEEM and XPS to study how the excess Si at the graphene-vacuum interface reorders itself at high temperatures. We show that silicon deposited at room temperature onto multilayer graphene films grown on the SiC(000[`1]) rapidly diffuses to the graphene-SiC interface when heated to temperatures above 1020. In a sequence of depositions, we have been able to intercalate ~ 6 ML of Si into the graphene-SiC interface.Comment: 6 pages, 8 figures, submitted to PR

Contribution française à l'upgrade de LHCb

La contribution française à l'upgrade de LHCb est d etaillée dans ce document et s'inscrit dans le prolongement du Framework TDR soumis au LHCC le 25 mai 2012. La France a contribué à la conception et à la réalisation de la mécanique et de l'électronique de lecture des calorimètres. Elle est l'acteur principal du système de déclenchement de premier niveau et l'initiatrice du projet DIRAC, progiciel de traitement et d'analyse de données dans un environnement distribué. Les physiciens et ingénieurs français ont de nombreuses responsabilités de premier plan et sont très fortement impliqués dans l'analyse des données. Les groupes français souhaitent poursuivre leur forte participation a l'expérience en contribuant a son upgrade, notamment l'électronique de lecture des calorimètres et du trajectographe en fibres scintillantes ainsi qu'au data processing

Contribution française à l'upgrade de LHCb

La contribution française à l'upgrade de LHCb est d etaillée dans ce document et s'inscrit dans le prolongement du Framework TDR soumis au LHCC le 25 mai 2012. La France a contribué à la conception et à la réalisation de la mécanique et de l'électronique de lecture des calorimètres. Elle est l'acteur principal du système de déclenchement de premier niveau et l'initiatrice du projet DIRAC, progiciel de traitement et d'analyse de données dans un environnement distribué. Les physiciens et ingénieurs français ont de nombreuses responsabilités de premier plan et sont très fortement impliqués dans l'analyse des données. Les groupes français souhaitent poursuivre leur forte participation a l'expérience en contribuant a son upgrade, notamment l'électronique de lecture des calorimètres et du trajectographe en fibres scintillantes ainsi qu'au data processing

Measurement of the mass difference and relative production rate of the Ωb− and Ξb− baryons

The mass difference between the Ω − b and Ξ − b baryons is measured using proton-proton collision data collected by the LHCb experiment, corresponding to an integrated luminosity of 9     fb − 1 , and is found to be m ( Ω − b ) − m ( Ξ − b ) = 248.54 ± 0.51 ( stat ) ± 0.38 ( syst )     MeV / c 2 . The mass of the Ω − b baryon is measured to be m ( Ω − b ) = 6045.9 ± 0.5 ( stat ) ± 0.6 ( syst )     MeV / c 2 . This is the most precise determination of the Ω − b mass to date. In addition, the production rate of Ω − b baryons relative to that of Ξ − b baryons is measured for the first time in p p collisions, using an LHCb dataset collected at a center-of-mass energy of 13 TeV and corresponding to an integrated luminosity of 6     fb − 1 . Reconstructing beauty baryons in the kinematic region 2 < η < 6 and p T < 20     GeV / c with their decays to a J / ψ meson and a hyperon, the ratio f Ω − b f Ξ − b × B ( Ω − b → J / ψ Ω − ) B ( Ξ − b → J / ψ Ξ − ) = 0.120 ± 0.008 ( stat ) ± 0.008 ( syst ) , is obtained, where f Ω − b and f Ξ − b are the fragmentation fractions of b quarks into Ω − b and Ξ − b baryons, respectively, and B represents the branching fractions of their respective decays

On the Growth of Averaged Weyl Sums for Rigid Rotations

Let ! 2 n and f 2 L 2 (S 1 ). We study the asymptotic behaviour of the Weyl sums S(m;!)f(x) = P m\Gamma1 k=0 f(x + k!) and their averages S(m;!)f(x) = 1 m P m j=1 S(j; !)f(x), in the L 2 -norm. In particular, for a suitable class of Liouville rotation numbers ! 2 n , we are able to construct examples of functions f 2 H s (S 1 ), s ? 0, such that, for all ffl ? 0, jj S(m;!)f jj 2 C ffl m 1 1+s \Gammaffl as m ! 1. In addition, for all f 2 H s (S 1 ), lim inf m \Gamma 1 1+s (log m) \Gamma1=2 k S(m;!)f k 2 ! 1, for all ! 2 n . 1 Introduction and statement of the results We study the asymptotic behaviour of the following skew products on the cylinder: (x 0 ; v 0 ) 2 S 1 \Theta j T S 1 ! (x 1 = x 0 + !; v 1 = v 0 + f(x 0 )): (1.1) E-mail: [email protected] y E-mail: [email protected] and [email protected] Here ! 2 n and f : S 1 ! ; S 1 = =. After m iterations of the map we have xm = x 0 + m!; v m = v 0 + S(m; !)f(x 0 ); wh..

A uniform, quality controlled Surface Ocean CO2 Atlas (SOCAT)

A well documented, publicly available, global data set of surface ocean carbon dioxide (CO2) parameters has been called for by international groups for nearly two decades. The Surface Ocean CO2 Atlas (SOCAT) project was initiated by the international marine carbon science community in 2007 with the aim of providing a comprehensive, publicly available, regularly updated, global data set of marine surface CO2, which had been subject to quality control (QC). Many additional CO2 data, not yet made public via the Carbon Dioxide Information Analysis Center (CDIAC), were retrieved from data originators, public websites and other data centres. All data were put in a uniform format following a strict protocol. Quality control was carried out according to clearly defined criteria. Regional specialists performed the quality control, using state-of-the-art web-based tools, specially developed for accomplishing this global team effort. SOCAT version 1.5 was made public in September 2011 and holds 6.3 million quality controlled surface CO2 data points from the global oceans and coastal seas, spanning four decades (1968–2007). Three types of data products are available: individual cruise files, a merged complete data set and gridded products. With the rapid expansion of marine CO2 data collection and the importance of quantifying net global oceanic CO2 uptake and its changes, sustained data synthesis and data access are priorities