Abstract
A significant intermittency signal is observed in 630 GeV pp collisions measured in the UA1 central detector. It occurs with similar magnitude in different variables: pseudorapidity, rapidity and azimuthal angle. The signal increases with decreasing charged particle multiplicity in the event. Its strength in a sample of low p⊥ tracks and its multiplicity dependence are not reproduced by commonly used Monte Carlo models of high energy interactions.
Original language | English (US) |
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Pages (from-to) | 1-21 |
Number of pages | 21 |
Journal | Nuclear Physics, Section B |
Volume | 345 |
Issue number | 1 |
DOIs | |
State | Published - Nov 26 1990 |