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Moments of Nucleon's Parton Distribution for the Sea and Valence Quarks from Lattice QCD

M. Deka, T. Streuer, T. Doi, S. J. Dong, T. Draper, K. F. Liu, N. Mathur, A. W. Thomas

TL;DR

The paper computes the first two moments of nucleon parton distributions, including sea-quark (disconnected) contributions, on a quenched $16^3 imes24$ lattice with Wilson fermions. It develops a stochastic complex $Z_2$-noise framework with unbiased subtraction to access all-to-all propagators and employs symmetry-based noise reduction, multiple nucleon sources, and careful renormalization to obtain $0.027 \\pm 0.006$ for $ig\<xig e_{s+ar{s}}$ at $\,\mu=2$ GeV and a ratio $ig\<xig e_{s+ar{s}} / ig\<x e_{u+ar{u}}$ (DI) of $0.88 \\pm 0.07$. The DI signals for light and strange quarks are strong for the first moment, while the second moments are statistically consistent with zero; CI results align with prior lattice studies. A notable finding is that the DI strange-to-light momentum ratio is larger than phenomenological fits, suggesting distinct connected and disconnected sea contributions and motivating future dynamical (2+1 flavor) lattice analyses to clarify the sea-quark structure and Gottfried-sum-type effects. Overall, the work demonstrates a feasible lattice-QCD route to sea-quark moments and highlights the need for dynamical fermions to reduce systematic uncertainties.

Abstract

We extend the study of lowest moments, $<x>$ and $<x^2>$, of the parton distribution function of the nucleon to include those of the sea quarks; this entails a disconnected insertion calculation in lattice QCD. This is carried out on a $16^3 \times 24$ quenched lattice with Wilson fermion. The quark loops are calculated with $Z_2$ noise vectors and unbiased subtractions, and multiple nucleon sources are employed to reduce the statistical errors. We obtain 5$σ$ signals for $<x>$ for the $u,d,$ and $s$ quarks, but $<x^2>$ is consistent with zero within errors. We provide results for both the connected and disconnected insertions. The perturbatively renormalized $<x>$ for the strange quark at $μ= 2$ GeV is $<x>_{s+\bar{s}} = 0.027 \pm 0.006$ which is consistent with the experimental result. The ratio of $<x>$ for $s$ vs. $u/d$ in the disconnected insertion with quark loops is calculated to be $0.88 \pm 0.07$. This is about twice as large as the phenomenologically fitted $\displaystyle\frac{< x>_{s+\bar{s}}}{< x>_{\bar{u}}+< x>_{\bar{d}}}$ from experiments where $\bar{u}$ and $\bar{d}$ include both the connected and disconnected insertion parts. We discuss the source and implication of this difference.

Moments of Nucleon's Parton Distribution for the Sea and Valence Quarks from Lattice QCD

TL;DR

The paper computes the first two moments of nucleon parton distributions, including sea-quark (disconnected) contributions, on a quenched lattice with Wilson fermions. It develops a stochastic complex -noise framework with unbiased subtraction to access all-to-all propagators and employs symmetry-based noise reduction, multiple nucleon sources, and careful renormalization to obtain for at GeV and a ratio (DI) of . The DI signals for light and strange quarks are strong for the first moment, while the second moments are statistically consistent with zero; CI results align with prior lattice studies. A notable finding is that the DI strange-to-light momentum ratio is larger than phenomenological fits, suggesting distinct connected and disconnected sea contributions and motivating future dynamical (2+1 flavor) lattice analyses to clarify the sea-quark structure and Gottfried-sum-type effects. Overall, the work demonstrates a feasible lattice-QCD route to sea-quark moments and highlights the need for dynamical fermions to reduce systematic uncertainties.

Abstract

We extend the study of lowest moments, and , of the parton distribution function of the nucleon to include those of the sea quarks; this entails a disconnected insertion calculation in lattice QCD. This is carried out on a quenched lattice with Wilson fermion. The quark loops are calculated with noise vectors and unbiased subtractions, and multiple nucleon sources are employed to reduce the statistical errors. We obtain 5 signals for for the and quarks, but is consistent with zero within errors. We provide results for both the connected and disconnected insertions. The perturbatively renormalized for the strange quark at GeV is which is consistent with the experimental result. The ratio of for vs. in the disconnected insertion with quark loops is calculated to be . This is about twice as large as the phenomenologically fitted from experiments where and include both the connected and disconnected insertion parts. We discuss the source and implication of this difference.

Paper Structure

This paper contains 35 sections, 88 equations, 19 figures, 12 tables.

Figures (19)

  • Figure 1: Quark line diagrams of the three-point function in the Euclidean path integral formalism. (a) Connected insertion and (b) disconnected insertion.
  • Figure 2: Plaquette terms (a) for the operator ${\cal O}_{\mu\mu}$ when $\kappa^3 D^3$ term is considered and (b) for ${\cal O}_{4ii}$ when $\kappa^2 D^2$ term is considered.
  • Figure 3: Errors of the noise estimation plotted against the number of configurations for different sets of noise vectors for the loop part of the current, ${\cal O}_{4i}$ at $\kappa_s = 0.154$ nd insertion time, $t_1 = 14$ (a) without subtraction and (b) with four subtraction terms.
  • Figure 4: Errors of the noise estimation plotted against the number of noise vectors for different sets of configurations for the loop part of the current ${\cal O}_{4i}$ at $\kappa_s = 0.154$ and insertion time, $t_1 = 14$ (a) without subtraction and (b) with four subtraction terms.
  • Figure 5: The ratio (D.I.) of the three-point to two-point functions at $\kappa_v=\kappa_s=0.154$ for the ${\cal O}_{4i}$ operator is plotted against the nucleon sink time ($t_2$) by using four different methods: (a) summation of insertion time from 5 to 20, (b) summation of insertion time from source to sink time, (c) method used in R. Lewis et al.wilcox3, and (d) summation of insertion time from (source time $+$ 1) to (sink time + 1).
  • ...and 14 more figures