We analyze PHENIX near-side ridge data for central Au+Au collisions at √ sNN = 200 GeV with the momentum kick model, in which a near-side jet emerges near the surface, kicks medium partons, loses energy, and fragments into the trigger particle and fragmentation products. The kicked medium partons subsequently materialize as the observed ridge particles, which carry direct information on the early parton momentum distribution and the magnitude of the momentum kick. We find that the PHENIX ridge data can be described well by the momentum kick model and the extracted early partons momentum distribution has a thermal-like transverse distribution and a rapidity plateau structure. We also find that the parton-parton scattering between the jet parton and the medium parton involves the exchange of a non-perturbative pomeron, for jet partons in momentum range considered in the near-side ridge measurements. PACS numbers: 25.75.Gz 25.75.Dw
I. INTRODUCTIONRecently, the STAR Collaboration [1,2,3,4,5,6,7,8,9,10,11,12,13] observed a ∆φ-∆η correlation of particles associated with a high-p t near-side hadron trigger particle in central Au+Au collisions at √ s N N = 200 GeV, where ∆φ and ∆η are the azimuthal angle and pseudorapidity differences measured relative to the trigger particle, respectively. Particles associated with the near-side jet can be decomposed into a "jet component" at (∆φ, ∆η)∼(0,0), and a "ridge component" at ∆φ∼0 with a ridge structure in ∆η. A similar correlation with a high-p t trigger has also been observed by the PHENIX Collaboration [14,15,16] and the PHOBOS Collaboration [17]. Recent reviews of the ridge phenomenon have also been presented [18,19,20].In this manuscript, we shall limit our attention to the ridge phenomenon involving a high p t jet on the near-side. We shall not consider ridge-type ∆φ-∆η correlations that have also been observed between two low-p t hadrons [21], as they do not involve the occurrence of a high-p t jet on the near-side. ] have been proposed to discuss the ridge phenomenon. The model of Ref. [27] assumes that the ridge particles arise from the extra particles deposited by the forward and backward beam jets at the source point associated with the two transverse jets. The correlation of the jet source transverse position and the transverse medium flow then leads to an azimuthal distribution with a width in ∆φ [27,28]. The width in ∆φ obtained from such a model is wide in comparison with experimental data [27]. The Correlated Emission Model [29,30,31,32] assumes that ridge particles arise from soft thermal gluons radiated along the jet direction, with an enhancement due to the radial flow. The models of Refs. [27] and [29] deal with the azimuthal correlations in the central rapidity region, and the pseudorapidity correlation has not yet been considered. The back-splash model assumes that the ridge on the near-side arises from the hydrodynamical back-splash of the away-side jet flow [33]; hydrodynamical calculations for such a model has not yet been made. The Glasma model examine...