在震后2300～2450s的时间内,于震中距30°～50°之间发现了以前从未报道过的1Hz散射波。这些散射波可能是在上地幔和地壳发生的PKPbc到PKPbc的反方位角散射而产生的,为绘制地幔非均匀性的小尺度变化(10km)提供了一个新的手段。...在震后2300～2450s的时间内,于震中距30°～50°之间发现了以前从未报道过的1Hz散射波。这些散射波可能是在上地幔和地壳发生的PKPbc到PKPbc的反方位角散射而产生的,为绘制地幔非均匀性的小尺度变化(10km)提供了一个新的手段。大孔径地震台阵(LASA)记录的阵列波束清晰地展示了散射波能量从噪声中逐步显露,在大约80s后达到最大振幅,并在150s后恢复到噪声水平。横向与径向慢度(ρt,ρr)的叠加显示在大约(2,-2)和(-2,-2)s/°存在两个峰值,表明这些波是沿着主弧路径(180°～360°)到达,而且明显是反方位角。基于上述观测资料,我们提出一种地幔和地表的PKPbc到PKPbc的散射机制,因为(1)这与散射波到时和散射波特有的慢度特征相吻合,(2)它的散射路径与之前观测到的深部地幔PK·KP散射路径类似(Chang and Cleary,1981)。观测到的上地幔散射波和PK·KP波均符合散射波的广义集合,我们称其为P′·d·P′,可以在地幔的任意深度d散射。展开更多
The product of the ∧0/b （-B/0） differential production cross-section and the branching fraction of the decay ∧0/b→ J/ψ pK-（-B/0→ J/ψ-K＊（892）0）is measured as a function of the beauty hadron transverse mome...The product of the ∧0/b （-B/0） differential production cross-section and the branching fraction of the decay ∧0/b→ J/ψ pK-（-B/0→ J/ψ-K＊（892）0）is measured as a function of the beauty hadron transverse momentum, PT, and rapidity, y. The kinematic region of the measurements is pT〈20 GeV/c and 2.0 〈g〈4.5.The measurements use a data sample corresponding to an integrated luminosity of 3fb-1 collected by the LHCb detector in pp collisions at centre-of-mass energies √s=7 TeV in 2011 and √s=8 TeV in 2012. Based on previous LHCb results of the fragmentation fraction ratio,f∧0/b/fd,the branching fraction of the decay ∧0/b→ J/ψ pK-is measured to be B（∧0/b→ J/ψ pK-）=（3.17±0.04±0.07±0.34＋0.45/-0.28）×10-4,where the first uncertainty is statistical, the second is systematic, the third is due to the uncertainty on the branching fraction of the decay -B/0 →J/ψ-K＊（892）0,and the fourth is due to the knowledge of f∧0/b/fd.The sum of the asymmetries in the production and decay between ∧0/b and ∧0/bis also measured as a function of PT and y.The previously published branching fraction of ∧0/b→ J/ψ pπ-,relative to that of ∧0/b→ J/ψ pK-,is updated. The branching fractions of ∧0/b→P＋c（→ J/ψp）K-are determined.展开更多
文摘在震后2300～2450s的时间内,于震中距30°～50°之间发现了以前从未报道过的1Hz散射波。这些散射波可能是在上地幔和地壳发生的PKPbc到PKPbc的反方位角散射而产生的,为绘制地幔非均匀性的小尺度变化(10km)提供了一个新的手段。大孔径地震台阵(LASA)记录的阵列波束清晰地展示了散射波能量从噪声中逐步显露,在大约80s后达到最大振幅,并在150s后恢复到噪声水平。横向与径向慢度(ρt,ρr)的叠加显示在大约(2,-2)和(-2,-2)s/°存在两个峰值,表明这些波是沿着主弧路径(180°～360°)到达,而且明显是反方位角。基于上述观测资料,我们提出一种地幔和地表的PKPbc到PKPbc的散射机制,因为(1)这与散射波到时和散射波特有的慢度特征相吻合,(2)它的散射路径与之前观测到的深部地幔PK·KP散射路径类似(Chang and Cleary,1981)。观测到的上地幔散射波和PK·KP波均符合散射波的广义集合,我们称其为P′·d·P′,可以在地幔的任意深度d散射。
基金Supported by CERN and national agencies:CAPES,CNPq,FAPERJ and FINEP(Brazil)NSFC(China)+17 种基金CNRS/IN2P3(France)BMBF,DFG,HGF and MPG(Germany)INFN(Italy)FOM and NWO(The Netherlands)MNi SW and NCN(Poland)MEN/IFA(Romania)Min ES and FANO(Russia)Min ECo(Spain)SNSF and SER(Switzerland)NASU(Ukraine)STFC(United Kingdom)NSF(USA)supported by IN2P3(France),KIT and BMBF(Germany),INFN(Italy),NWOSURF(The Netherlands),PIC(Spain),Grid PP(United Kingdom)support from EPLANET,Marie Sk lodowska-Curie ActionsERC(European Union),Conseil général de Haute-Savoie,Labex ENIGMASS and OCEVU,RégionAuvergne(France),RFBR(Russia),Xunta GalGENCAT(Spain),Royal Society and Royal Commission for the Exhibition of 1851(United Kingdom)
文摘The product of the ∧0/b （-B/0） differential production cross-section and the branching fraction of the decay ∧0/b→ J/ψ pK-（-B/0→ J/ψ-K＊（892）0）is measured as a function of the beauty hadron transverse momentum, PT, and rapidity, y. The kinematic region of the measurements is pT〈20 GeV/c and 2.0 〈g〈4.5.The measurements use a data sample corresponding to an integrated luminosity of 3fb-1 collected by the LHCb detector in pp collisions at centre-of-mass energies √s=7 TeV in 2011 and √s=8 TeV in 2012. Based on previous LHCb results of the fragmentation fraction ratio,f∧0/b/fd,the branching fraction of the decay ∧0/b→ J/ψ pK-is measured to be B（∧0/b→ J/ψ pK-）=（3.17±0.04±0.07±0.34＋0.45/-0.28）×10-4,where the first uncertainty is statistical, the second is systematic, the third is due to the uncertainty on the branching fraction of the decay -B/0 →J/ψ-K＊（892）0,and the fourth is due to the knowledge of f∧0/b/fd.The sum of the asymmetries in the production and decay between ∧0/b and ∧0/bis also measured as a function of PT and y.The previously published branching fraction of ∧0/b→ J/ψ pπ-,relative to that of ∧0/b→ J/ψ pK-,is updated. The branching fractions of ∧0/b→P＋c（→ J/ψp）K-are determined.
