6,347 research outputs found

    Weak Decays of Doubly Heavy Baryons: the 1/21/21/2\to 1/2 case

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    Very recently, the LHCb collaboration has observed in the final state Λc+Kπ+π+\Lambda_c^+ K^-\pi^+\pi^+ a resonant structure that is identified as the doubly-charmed baryon Ξcc++\Xi_{cc}^{++}. Inspired by this observation, we investigate the weak decays of doubly heavy baryons Ξcc++\Xi_{cc}^{++}, Ξcc+\Xi_{cc}^{+}, Ωcc+\Omega_{cc}^{+}, Ξbc()+\Xi_{bc}^{(\prime)+}, Ξbc()0\Xi_{bc}^{(\prime)0}, Ωbc()0\Omega_{bc}^{(\prime)0}, Ξbb0\Xi_{bb}^{0}, Ξbb\Xi_{bb}^{-} and Ωbb\Omega_{bb}^{-} and focus on the decays into spin 1/21/2 baryons in this paper. At the quark level these decay processes are induced by the cd/sc\to d/s or bu/cb\to u/c transitions, and the two spectator quarks can be viewed as a scalar or axial vector diquark. We first derive the hadronic form factors for these transitions in the light-front approach and then apply them to predict the partial widths for the semi-leptonic and non-leptonic decays of doubly heavy baryons. We find that a number of decay channels are sizable and can be examined in future measurements at experimental facilities like LHC, Belle II and CEPC.Comment: 40 pages, 4 figures, to appear in EPJ

    Multipartite entanglement purification with quantum nondemolition detectors

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    We present a scheme for multipartite entanglement purification of quantum systems in a Greenberger-Horne-Zeilinger state with quantum nondemolition detectors (QNDs). This scheme does not require the controlled-not gates which cannot be implemented perfectly with linear optical elements at present, but QNDs based on cross-Kerr nonlinearities. It works with two steps, i.e., the bit-flipping error correction and the phase-flipping error correction. These two steps can be iterated perfectly with parity checks and simple single-photon measurements. This scheme does not require the parties to possess sophisticated single photon detectors. These features maybe make this scheme more efficient and feasible than others in practical applications.Comment: 8 pages, 5 figure

    Edge states in self-complementary checkerboard photonic crystals: Zak phase, surface impedance and experimental verification

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    Edge states of photonic crystals have attracted much attention for the potential applications such as high transmission waveguide bends, spin dependent splitters and one-way photonic circuits. Here, we theoretically discuss and experimentally observe the deterministic edge states in checkerboard photonic crystals. Due to the self-complementarity of checkerboard photonic crystals, a common band gap is structurally protected between two photonic crystals with different unit cells. Deterministic edge states are found inside the common band gap by exploiting the Zak phase analysis and surface impedance calculation. These edge states are also confirmed by a microwave experiment.Comment: 13 pages, 4 figure

    Magmatic record of India-Asia collision

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    This work was financially co-supported by Chinese Academy of Sciences (XDB03010301) and other Chinese funding agencies (Project 973: 2011CB403102 and 2015CB452604; NSFC projects: 41225006, 41273044, and 41472061).New geochronological and geochemical data on magmatic activity from the India-Asia collision zone enables recognition of a distinct magmatic flare-up event that we ascribe to slab breakoff. This tie-point in the collisional record can be used to back-date to the time of initial impingement of the Indian continent with the Asian margin. Continental arc magmatism in southern Tibet during 80-40 Ma migrated from south to north and then back to south with significant mantle input at 70-43 Ma. A pronounced flare up in magmatic intensity (including ignimbrite and mafic rock) at ca. 52-51 Ma corresponds to a sudden decrease in the India-Asia convergence rate. Geological and geochemical data are consistent with mantle input controlled by slab rollback from ca. 70 Ma and slab breakoff at ca. 53 Ma. We propose that the slowdown of the Indian plate at ca. 51 Ma is largely the consequence of slab breakoff of the subducting Neo-Tethyan oceanic lithosphere, rather than the onset of the India-Asia collision as traditionally interpreted, implying that the initial India-Asia collision commenced earlier, likely at ca. 55 Ma.Peer reviewe
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