首页> 外文OA文献 >Measurement of single transverse spin asymmetry via single hadrons and di-hadron correlations in the 200GeV p + p collision in the PHENIX experiment at RHIC
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Measurement of single transverse spin asymmetry via single hadrons and di-hadron correlations in the 200GeV p + p collision in the PHENIX experiment at RHIC

机译:在RHIC进行的PHENIX实验中,通过200GeV p + p碰撞中的单个强子和双强子相关性测量单个横向自旋不对称性

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摘要

The spin structure of the proton has been revealed to be extremely complex. The proton spin is composed of the spins and the orbital angular momenta of quarks and gluons in the proton. The first results from polarized deep inelastic scattering (pDIS) experiments in the late 1980s and early 1990s revealed that quarks do not carry a significant fraction of the proton\u27s spin. The recent global analysis on gluon spin including RHIC results showed that gluons have a very small contribution on the spin of proton. Therefore, it is extremely important for physicists understanding the contribution from the orbital angular momenta of quarks and gluons. However, it is very difficult for the current experiments measuring the orbital angular momentum directly and accurately. The Sivers-type single transverse spin asymmetry provides us a window to study the orbital angular momentum.In this thesis, results for the single transverse spin asymmetry of forward charged hadrons in polarized proton collisions measured with the PHENIX detector are presented.A predicted sizable asymmetry has been observed which is consistent with the results from other experiments. A correlation between neutral pions and charged hadrons measured in the central region of the PHENIX detector has been used to extract the single transverse spin asymmetry due to the Sivers effect. The Sivers effect describes the relation of the proton\u27s spin and its intrinsic transverse momentum. The latter one has been thought to originate from the orbital angular momentum of proton.
机译:质子的自旋结构已被证明极其复杂。质子自旋由质子中的自旋以及夸克和胶子的轨道角动量组成。极化深非弹性散射(pDIS)实验在1980年代末和1990年代初的第一项结果表明,夸克没有携带质子自旋的很大一部分。最近对胶子自旋的全球分析包括RHIC结果表明,胶子对质子自旋的贡献很小。因此,对于物理学家来说,了解夸克和胶子的轨道角动量的贡献非常重要。但是,当前的实验很难直接,准确地测量轨道角动量。 Sivers型单横向自旋不对称性为我们研究轨道角动量提供了一个窗口。本文提出了利用PHENIX探测器测量的极化质子碰撞中的正电荷强子的单横向自旋不对称性的结果。已经观察到与其他实验的结果一致。由于Sivers效应,在PHENIX探测器中心区域测得的中性介子与带电强子之间的相关性已被用于提取单个横向自旋不对称性。 Sivers效应描述了质子自旋与其固有的横向动量之间的关系。后者被认为起源于质子的轨道角动量。

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    Wei, Feng;

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  • 年度 2010
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  • 原文格式 PDF
  • 正文语种 en
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