Ridge and Transverse Correlation without Long-Range Longitudinal Correlation

A simple phenomenological relationship between the ridge distribution in Δη and the single-particle distribution in η can be established from the PHOBOS data on both distributions. The implication points to the possibility that it is not necessary to have long-range longitudinal correlation to expla...

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Main Authors: Charles B. Chiu, Rudolph C. Hwa
Format: Article
Language:English
Published: Wiley 2013-01-01
Series:Advances in High Energy Physics
Online Access:http://dx.doi.org/10.1155/2013/728365
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author Charles B. Chiu
Rudolph C. Hwa
author_facet Charles B. Chiu
Rudolph C. Hwa
author_sort Charles B. Chiu
collection DOAJ
description A simple phenomenological relationship between the ridge distribution in Δη and the single-particle distribution in η can be established from the PHOBOS data on both distributions. The implication points to the possibility that it is not necessary to have long-range longitudinal correlation to explain the data. An interpretation of the relationship is then developed, based on the recognition that longitudinal uncertainty of the initial configuration allows for non-Hubble-like expansion at early time. It is shown that the main features of the ridge structure can be explained in a model where transverse correlation stimulated by semihard partons is the principal mechanism. This work is related to the azimuthal anisotropy generated by minijets in Au-Au collisions at 0.2 TeV on the one hand and to the ridge structure seen in pp collisions at 7 TeV on the other hand.
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series Advances in High Energy Physics
spelling doaj-art-b9a6926adc214ca784a40922e2c044262025-02-03T05:59:50ZengWileyAdvances in High Energy Physics1687-73571687-73652013-01-01201310.1155/2013/728365728365Ridge and Transverse Correlation without Long-Range Longitudinal CorrelationCharles B. Chiu0Rudolph C. Hwa1Center for Particles and Fields and Department of Physics, University of Texas at Austin, Austin, TX 78712, USAInstitute of Theoretical Science and Department of Physics, University of Oregon, Eugene, OR 97403-5203, USAA simple phenomenological relationship between the ridge distribution in Δη and the single-particle distribution in η can be established from the PHOBOS data on both distributions. The implication points to the possibility that it is not necessary to have long-range longitudinal correlation to explain the data. An interpretation of the relationship is then developed, based on the recognition that longitudinal uncertainty of the initial configuration allows for non-Hubble-like expansion at early time. It is shown that the main features of the ridge structure can be explained in a model where transverse correlation stimulated by semihard partons is the principal mechanism. This work is related to the azimuthal anisotropy generated by minijets in Au-Au collisions at 0.2 TeV on the one hand and to the ridge structure seen in pp collisions at 7 TeV on the other hand.http://dx.doi.org/10.1155/2013/728365
spellingShingle Charles B. Chiu
Rudolph C. Hwa
Ridge and Transverse Correlation without Long-Range Longitudinal Correlation
Advances in High Energy Physics
title Ridge and Transverse Correlation without Long-Range Longitudinal Correlation
title_full Ridge and Transverse Correlation without Long-Range Longitudinal Correlation
title_fullStr Ridge and Transverse Correlation without Long-Range Longitudinal Correlation
title_full_unstemmed Ridge and Transverse Correlation without Long-Range Longitudinal Correlation
title_short Ridge and Transverse Correlation without Long-Range Longitudinal Correlation
title_sort ridge and transverse correlation without long range longitudinal correlation
url http://dx.doi.org/10.1155/2013/728365
work_keys_str_mv AT charlesbchiu ridgeandtransversecorrelationwithoutlongrangelongitudinalcorrelation
AT rudolphchwa ridgeandtransversecorrelationwithoutlongrangelongitudinalcorrelation