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${{\mathit N}{(1710)}}$ ELASTIC POLE RESIDUE

PHASE $\theta $

INSPIRE   PDGID:

B014IMR

VALUE ($^\circ{}$) DOCUMENT ID TECN  COMMENT $\bf{ 120\text{ to }270\text{ }(\approx190) }$ OUR ESTIMATE $-114$ $\pm29$ ROENCHEN 2022 DPWA Multichannel $130$ $\pm35$ SOKHOYAN 2015 A DPWA Multichannel $-104$ $\pm7$ $\pm3$ 1 SVARC 2014 L+P ${{\mathit \pi}}$ ${{\mathit N}}$ $\rightarrow$ ${{\mathit \pi}}{{\mathit N}}$ $175$ $\pm35$ CUTKOSKY 1980 IPWA ${{\mathit \pi}}$ ${{\mathit N}}$ $\rightarrow$ ${{\mathit \pi}}{{\mathit N}}$ • • We do not use the following data for averages, fits, limits, etc. • • $55$ ROENCHEN 2015 A DPWA Multichannel $120$ $\pm45$ GUTZ 2014 DPWA Multichannel $9$ SHKLYAR 2013 DPWA Multichannel $120$ $\pm70$ ANISOVICH 2012 A DPWA Multichannel $20$ 2 BATINIC 2010 DPWA ${{\mathit \pi}}$ ${{\mathit N}}$ $\rightarrow$ ${{\mathit N}}{{\mathit \pi}}$, ${{\mathit N}}{{\mathit \eta}}$ $-167$ CUTKOSKY 1990 IPWA ${{\mathit \pi}}$ ${{\mathit N}}$ $\rightarrow$ ${{\mathit \pi}}{{\mathit N}}$ 1  Fit to the amplitudes of HOEHLER 1979. 2  BATINIC 2010 finds evidence for a second ${\mathit P}_{\mathrm 11}$ state with all parameters except for the phase of the pole residue very similar to the parameters we give here.

References

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