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Chung-Wen Kao Chung-Yuan Christian University
Kaon multiplicities of Semi-inclusive DIS and the fragmentation functions Chung-Wen Kao Chung-Yuan Christian University QNP 2018 Tsukuba, Japan
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Collaboration and Reference
In Collaboration with Nam Seung-il (PKU, Korea) Dong-Jing Yang, Fu-Jiun Jiang (NTNU, Taiwan) Wen-Chen Chang (AS, Taiwan) This talk is based on the following works: (1) Nam Seung-il, CWK, Phys. Rev .D85, (2012) (2) Nam Seung-il, CWK, : Phys.Rev.D85, (2012) (3) Dong Jing Yang, Fu-Jiun Jaing, CWK, Nam Seung-il: Phys. Rev D87, (2013) (4) Dong Jing Yang, Fu-Jiun Jaing, CWK, Nam Seung-il: arXiv (5) Dong Jing Yang, Fu-Jiun Jaing, Wen-Chen Chang, CWK, Nam Seung-il: Phys. Lett. B 755(2016) 393
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How to extract Fragmentation functions?
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SIDIS using deuteron target
Charge Conjugation of fragmentation functions Why deuteron ?
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SIDIS off deuteron target
p: proton, n: neutron
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SIDIS using deuteron target
Assume PDFs are charge symmetric:
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SIDIS using deuteron target
DQ>>DS
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HERMES Data of Pion multiplicity
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Kaon Multiplicity
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HERMES Kaon Data A. Airapetian et al. (HERMES Collaboration), Phys. Rev. D , (2014).
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Pion and kaon multiplicities
For pion and kaon multiplicities of SIDIS off the deuteron target: Combine the HERMES data of kaon and DSS07 Fragmentation functions, the strange quark PDF was extracted. Phys. Rev. D 89, (2014)
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Phys.Lett. B755 (2016)
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Constrains on A and B Since S(x)>0, Q(x)>0, then S(x)/Q(x) is positive! At fixed x and Q2 : Note that the values of and are independent of x!
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Choices of FFs
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HKNS (LO) HKNS (NLO) DSS (LO) DSS (NLO) 5.NJL-Jet Model 6.Nonlocal Chiral Quark Model 7.AKK08 8.SMKA 9.DSEHS
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HKNS (LO) HKNS (NLO) DSS (LO) DSS (NLO) 5.NJL-Jet Model 6.Nonlocal Chiral Quark Model 7.AKK08
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NLO fitting of SIDIS
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A game need two players….
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COMPASS and HERMES The data pointes are taken at
different Q2 values compared with HERMES data. Phys.Lett. B767 (2017)
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COMPASS and HERMES HERMES COMPASS
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COMPASS and HERMES
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DSS 2017 fragmentation functions
Phys.Rev. D95 (2017) no.9, , already have 27 citations.
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DSS 2017 fragmentation functions
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DSS 2017 fragmentation functions
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DSS 2017 fragmentation functions
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DSS 2017 fragmentation functions
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DSS 2017 fragmentation functions
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Our Puzzle over DSS17 If DSS17 can describe both of HERMES and COMPASS kaon multiplicities well, then the two sets of data surely are compatible. However, the simple plot shows otherwise. So what’s going on? Maybe the difference of two sets of data is indeed due to the different Q2?
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Test of DSS17 at HERMES and COMPASS kinematics
Using DSS17 Apply DSS17 with MMHT and NNPDF at (x, Q2) of HERMES data points and COMPASS, we find the theoretical results of both should be close. The effect of Q2 evolution is not enough to explain the difference between two data sets.
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Kaon multiplicity Using DSS17
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Check HERMES data K+
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Check HERMES data K- Error! It should be 𝛼=0.38 𝛼=0.07 𝛼=0.02 𝛼=0.00
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Log to Log & Linear to Linear:
Fit well?
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MK+(x, Q2) and MK-(x, Q2) Red point: usual integral method
Blue cross: integrate z by HERMES method Black point: HERMES For positive and negative kaon, The PDFXFF values are higher than The experimental values.
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Charged Kaon Multiplicity
Similar check on COMPASS kinematics is needed.
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Three regions Phys.Lett. B766 (2017) 245-253 by
M.Boglione, J.Collins, L.Gamberg, J.O.Gonzalez-Hernandez, T.C.Rogers, N.Sato, LO cross section: PDF X FF
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Is it the reason of the serious inconsistency between
pion and kaon multiplicities? How to prove or falsify it?
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Summary and outlook Is DSS17 good as they claimed?
Can one extract the strange PDFs from the current SIDIS data? Is there tension between COMPASS and HERMES data of SIDIS? Is there tension between the pion and kaon multiplicities? Is the contribution of the central region able to explain the difference between HERMES and COMPASS data?
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Two data sets of SIDIS cause many confusions, but two cups of ice cream are just perfect!
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