Inverse problem or Spectral unfolding
Key assumptions: (see also: astro-ph/0506588 ) All observed spectra dF/dû in the high energy Extensive Air Shower (EAS) physics have been obtained via the convolutions of the energy spectra dℑ/dEA of primary nuclei (A ≡ H, He, ... at least up to Ni) over the atmosphere with the expected spectra ∂WA(EA, u)/∂u of EAS vector parameter u={Ne , Nμ , s, θ, ...} at the observation level taking into account the corresponding response function of a given experiment, ∂ℜA(u, EA, x, y, θ)/∂û, which itself is the probability to detect and reconstruct a shower with vector parameter û
instead of true vector parameter u.
For a horizontal observation level and the shower core coordinates x, y, θ, φ, the mentioned convolution looks like:
dF/dû = ∑A∫dℑ/dEA⋅KA(EA,û)dEA
,
(1)
where
KA(EA,û) = ∫∫(∂WA/∂u)⋅(∂ℜA/∂û)dudD
is the kernel function defined in the multivariate shower detection space with
dudD=du⋅2πcosθdxdydcosθ space element.
In general, the shower spectra WA(EA,u) from (1) depend on the interaction model (see also [S.V.Ter-Antonyan and L.S.Haroyan, hep-ex/0003006 (2000), or S.V.Ter-Antonyan & P.L.Biermann, astro-ph/0106091 (2001)].
The multidimensional integral (1) is better to calculate by the Monte-Carlo simulation since the shower spectra WA(u) and corresponding response functions ℜA(u,û) one can estimate more or less precisely only by the simulations.
The integral equation (1) is not a Fredholm equation (or a set of equations) of the first kind due to a set of object (unknown) functions (dℑ/dEA), and the theory of integral equations is not applicable for the equation (1), [S. Ter-Antonyan,
arXiv:0706.4087,
arXiv:1405.5472].
We computed the kernel functions
KA(EA,û)
of integral equations (1) for û ≡ {N̂ch(e,γ,μ,h), N̂μ , ŝ, θ ̂} at the observation level of GAMMA experiment (700 g/cm²) using the CORSIKA6030 (NKG, EGS) EAS simulation code [D.Heck et al., FZKA, 6019, 1998] with QGSJET01 and SIBYLL2.1 interaction models for the 4 groups of primary nuclei: A ≡ H, He, O-like, Fe-like at the power law primary energy spectra f(EA) ∝ E−1.5, . Each secondary shower particle (e, μ, h, γ) obtained at the observation level from CORSIKA shower simulation code is passed online through the GAMMA shower array (scintillators). Furthermore, the transformation of computed energy deposit to the corresponding ADC code and final decoding into a number of detected particles simulates also the digitization errors of readout system.
 Simulation of shower particle passage through the GAMMA detectors
All EAS muons with energy Eμ > (4 GeV)/cosθ at the GAMMA observation level are passed through the 2500 g/cm² rock taking into account the fluctuations of ionization losses and electron (positron) accompaniment due to muon bremsstrahlung, direct pair production, knock-on and photo-nuclear interactions.
The reconstructions of shower parameters at the observation level (N̂ch, N̂μ , ŝ) on the basis of the simulated (detected) number of particles in the scintillators are carried out using NKG and Exponential lateral distribution functions for ground-based charged particle and high energy underground muon shower components respectively.
The computations of expected spectra {dF/dû} are performed using integration (1) for the simulated kernel function KA(EA,û) and universal parameterization of primary nuclei energy spectra reported in ANI98 Workshop (Hor-Amberd, Armenia, 1998 [hep-ex/0003006 (2000)]) by S. Ter-Antonyan:
dℑA/dE = ΦA⋅E −γ₁ [ 1 + ( E /Eknee, A ) ε ] −Δγ /ε
, (2)
where the parameter ε describes the sharpness of spectral knee and Δγ=γ₂−γ₁ for the asymptotic energy spectral power indices below (γ₁≃2.7 ± 0.02) and above (γ₂≃3.15 ± 0.05) the spectral rigidity-dependent knee energy, Eknee, A ≃ (3 PV)⋅ZA for the ZA charge of primary nucleus, A.
The parameterization (2) has been used as the solutions of inverse problem in the energy range 1015-1017eV (see arxiv.org/abs/1405.5472).
EAS Inverse Problem that is the reconstruction of primary energy spectra dℑ/dEA (object functions) has been carried out by the
solution of integral equations (1) as a set of the parameterized equations at the known kernel functions KA(EA,û), parameterizations (2) [see refs. S.Ter-Antonyan (2014, 2008, 2003, 2000) in Publications page] for rigidity-dependent steepening primary nuclei energy spectra in the knee region and the detected shower spectra {dF/dû} from GAMMA experiment.
The all-particle energy spectrum, dℑ/dE0 = ∑Adℑ/dEA , has also been obtained by the event-by-event primary energy E0 estimation method regardless of primary nucleus (A). The primary energy estimator,
lnE₀ = ƒ(û), was obtained from the best fit of shower simulated dataset {(E, A, θ) ⇒ u ⇒ û}, where û = {N̂ch , N̂μ , ŝ} is the observable shower vector parameter taking into account the measurement errors and uncertainties of GAMMA experiment. The derived 6-parametric best fit for the energy estimator of GAMMA shower array is the following:
lnE₀ =a₁ lnNch+a₂
√ s
/ cosθ +a₃ cosθ +a₄ +a₅ /( lnNch+a₆ lnNμ) , (3)
where a₁ , a₂ , ..., a₆ are approximation parameters.
The observable (reconstructed and measured) shower parameters in the expression (3) are:
Nch - the EAS size, Nμ - a truncated (Rμ<50 m) number of EAS muons with energies Eμ>5 GeV, s - the EAS age parameter, and θ - the zenith angle of shower core. The expression (3) provides the accuracy of energy estimator ΔE₀/E₀≲15% for the primary energies E₀≲200 PeV.
The method was first reported in GAMMA 2004 workshop and presented in ref. [Ter-Antonyan et al., astro-ph/0506588 (2005)] and [arXiv:1405.5472 [astro-ph.HE] (2014), Physical Review D 89, 123003 (2014)] (see also Publications in menu).
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