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References - Bogoliubov Laboratory of Theoretical Physics - JINR

References - Bogoliubov Laboratory of Theoretical Physics - JINR

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ackground fraction, and asymmetry in the background, are estimated from sidebands<br />

around the mass peak. Background fractions vary from 16% in the π 0 pT range <strong>of</strong> 2-3<br />

GeV, to 6% in the 9-12 GeV range at √ s = 200 GeV.<br />

In 2006, PHENIX recorded 0.08<br />

pb −1 <strong>of</strong> pp collisions at √ s = 62.4<br />

GeV. This run was intended primarily<br />

to improve upon ISR results on inclusive<br />

pion cross-sections. At these low center<br />

<strong>of</strong> mass energies, next-to-leading order<br />

(NLO) perturbative QCD (pQCD) predictions<br />

<strong>of</strong> inclusive pion cross-sections<br />

tend to under-predict the observed<br />

yields. Including threshold resummation<br />

at next-to-leading-logarithm (NLL)<br />

accuracy improves the agreement with<br />

fixed target [5] and collider data [6]. The<br />

PHENIX measurement <strong>of</strong> the inclusive<br />

π 0 cross-section confirmed the necessity<br />

<strong>of</strong> such corrections [7]. In addition,<br />

the measurement <strong>of</strong> ALL(pp → π 0 X)at<br />

√ s =62.4 GeV [7], made with one week<br />

Figure 2: ALL for π 0 at √ s =62.4 GeV as a function<br />

<strong>of</strong> pT , showing statistical uncertainties. (14% uncertainty<br />

in polarization not shown.) Four GRSV NLO<br />

pQCD (solid curves) and NLL pQCD (dashed curves)<br />

are shown for comparison. See text for details.<br />

<strong>of</strong> data, excluded the GRSV scenarios Δg(x) =±g(x) [8] (see Fig. 2). The NLL predictions<br />

for Aπ0 LL are smaller than for NLO pQCD. The asymmetry measurement also<br />

extended our sensitivity to Δg(x) tohigherx in comparison to the measurements at<br />

√ s = 200 GeV.<br />

From the 2005 and 2006 runs at √ s = 200 GeV, PHENIX published results on ALL<br />

<strong>of</strong> π 0 [9] (see Fig. 3). These asymmetries are consistent with zero, and clearly lie below<br />

the GRSV standard model (which reflected the best fit to polarized deep inelastic scattering<br />

(DIS) data), thus favoring a smaller Δg(x), and smaller integral Δg. Anestimate<br />

<strong>of</strong> the integral <strong>of</strong> Δg(x) can be made from these data in the framework <strong>of</strong> the GRSV<br />

model. We use the notation Δg [a,b] to denote the integral <strong>of</strong> Δg(x) froma

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