Analysis of ATLAS pp elastic measurements at $\sqrt{s}$=13 TeV and comparison with TOTEM measurements
E. Ferreira, T. Kodama, A. K. Kohara
TL;DR
The paper analyzes pp elastic scattering at $\sqrt{s}=13$ TeV by ATLAS and TOTEM within the KFK framework, showing that differences in $d\sigma/dt$ and $\sigma_{\rm tot}$ are largely attributable to a common normalization related by the optical theorem. By disentangling the real and imaginary parts of the amplitude with independent slopes and locating zeros (including Martin's zero) in both parts, the study explains why the ATLAS and TOTEM results are qualitatively similar and yields a model-dependent $\rho^{ATLAS}=0.091\pm0.004$. It demonstrates that an effective normalization factor of about $0.88$ aligns the differential cross sections across the measured $|t|$ ranges, and highlights the importance of the $T_R$ and $T_I$ separation for interpreting forward quantities and the dip–bump structure. The work underscores that $\rho$ and related slope parameters are sensitive to the underlying amplitude model, and that genuine incompatibilities between experiments are unlikely once a coherent phenomenological description is employed.
Abstract
A comparative description is made of the measurements at LHC of pp elastic scattering at 13 TeV by the ATLAS and TOTEM Collaborations. In the total and differential cross sections we show that the differences are justified through single numerical factor. It seems that there is no fundamental physical difference, but only a difference of normalization between the two experiments. We study the real and imaginary amplitudes disentangled with the KFK (Kohara-Ferreira-Kodama) model and show that the properties are similar in qualitative aspects for both experiments. The real and imaginary parts have different slopes at the origin and present zeros, with distributions that are common to several models, with three zeros in the real part and one zero in the imaginary amplitude. A zero in the real part, known as Martin's zero, influences the determination of the $ρ$ parameter.
