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Local Muon Density Spectra

Updated 8 July 2026
  • Local Muon Density Spectra are the distributions of muon counts per unit area in air showers, measured under fixed geometric and threshold conditions.
  • They convert detector signals—such as hit multiplicities and charge distributions—into muon densities using simulation-based calibration and correction factors.
  • Analyses of LMDS reveal key spectral features like the second knee and offer composition diagnostics by comparing observations with predictions from hadronic interaction models.

Searching arXiv for the cited LMDS and related muon-density papers to ground the article in current arXiv records. Local Muon Density Spectra (LMDS) are distributions of air-shower events as functions of the locally measured muon density at the observation level or, equivalently, on a plane perpendicular to the shower axis. In extensive air shower work, the observable is always conditioned by geometry and threshold: zenith angle, lateral distance from the shower core when relevant, and the detector’s effective muon-energy threshold. In that form, LMDS provide a detector-level bridge between measured muon content, the primary cosmic-ray spectrum, mass composition, and hadronic-interaction modeling. The concept is realized in different but compatible ways in the NEVOD complex, where muon-bundle multiplicities are converted to local densities, and in IceTop, where GeV muon densities are extracted from tank charge distributions at fixed reference radii (Kokoulin et al., 2017, Soldin, 2021, Cazon, 2020).

1. Definition and mathematical form

The local muon density ρμ\rho_\mu is the number of muons per unit area in a small region around the observation point for a given shower and arrival direction. In near-vertical IceTop analyses, the corresponding quantity is the number of GeV-scale muons per unit area at lateral distance rr from the shower axis, measured on a plane perpendicular to the shower axis. If λ(r)\lambda(r) is the expected muon count in a tank at distance rr and AeffA_{\mathrm{eff}} is the tank’s projected effective area, then

λ(r)=ρμ(r)Aeff,ρμ(r)=λ(r)Aeff.\lambda(r)=\rho_\mu(r)\,A_{\mathrm{eff}}, \qquad \rho_\mu(r)=\frac{\lambda(r)}{A_{\mathrm{eff}}}.

For muon bundles in NEVOD, an approximate multiplicity-to-density conversion is

ρμmAeff(θ),\rho_\mu \approx \frac{m}{A_{\text{eff}}(\theta)},

with mm the reconstructed bundle multiplicity and Aeff(θ)A_{\text{eff}}(\theta) the detector effective area for the zenith angle θ\theta (Soldin, 2021, Kokoulin et al., 2017).

The differential LMDS in a zenith bin can be written as

rr0

while a more general notation for the local muon density spectrum is rr1, the differential event rate as a function of the local density under specified geometry and threshold. At fixed IceTop reference distance rr2, one may also define an integral spectrum rr3 and a differential spectrum rr4 (Kokoulin et al., 2017, Cazon, 2020, Soldin, 2021).

The relation between LMDS and more familiar muon-size observables follows from the muon lateral distribution function (LDF). If the LDF factorizes as

rr5

then at fixed rr6, or within a fixed annulus where rr7 varies weakly over the interval considered, one has rr8, and the LMDS slope coincides with the muon-size spectrum slope. In KASCADE language, the truncated muon number is

rr9

so spectra in λ(r)\lambda(r)0 are integral transforms of LMDS over that radial band (Bijay et al., 2015).

2. Instrumental realizations and observation conditions

LMDS have been reconstructed with markedly different detector layouts. The NEVOD experimental complex uses the coordinate detector DECOR for inclined muon bundles and the Calibration Telescope System (CTS) for near-vertical bundles. IceTop uses water Cherenkov tanks on the surface of IceCube and derives local muon density from tank charge distributions in near-vertical air showers (Kokoulin et al., 2017, Soldin, 2021).

Instrument Muon observable Key conditions
DECOR Bundle multiplicity converted to λ(r)\lambda(r)1 Effective zenith angles λ(r)\lambda(r)2, λ(r)\lambda(r)3, λ(r)\lambda(r)4; λ(r)\lambda(r)5; about λ(r)\lambda(r)6 h live time
CTS Bottom-plane hit multiplicity converted to λ(r)\lambda(r)7 Effective zenith angle λ(r)\lambda(r)8; 3–40 hit counters; about λ(r)\lambda(r)9 h live time
IceTop rr0 at fixed rr1 from SLC charge fits rr2; rr3 m and rr4 m; about rr5 live days

DECOR consists of eight supermodules placed in building galleries around the Cherenkov water detector. Each supermodule contains eight vertical planes of streamer-tube chambers, each plane having area rr6, and the reconstructed muon-track angular accuracy is better than rr7. The analysis uses three inclined zenith bins, rr8–rr9, AeffA_{\mathrm{eff}}0–AeffA_{\mathrm{eff}}1, and AeffA_{\mathrm{eff}}2–AeffA_{\mathrm{eff}}3, with effective zenith angles of AeffA_{\mathrm{eff}}4, AeffA_{\mathrm{eff}}5, and AeffA_{\mathrm{eff}}6 respectively. The sample comprises about AeffA_{\mathrm{eff}}7 events with muon bundle multiplicity AeffA_{\mathrm{eff}}8, taken over two periods, 2002–2007 and 2012–2016, for a total live time of about AeffA_{\mathrm{eff}}9 h (Kokoulin et al., 2017).

CTS consists of two planes of scintillation counters arranged in a chess order over λ(r)=ρμ(r)Aeff,ρμ(r)=λ(r)Aeff.\lambda(r)=\rho_\mu(r)\,A_{\mathrm{eff}}, \qquad \rho_\mu(r)=\frac{\lambda(r)}{A_{\mathrm{eff}}}.0, with λ(r)=ρμ(r)Aeff,ρμ(r)=λ(r)Aeff.\lambda(r)=\rho_\mu(r)\,A_{\mathrm{eff}}, \qquad \rho_\mu(r)=\frac{\lambda(r)}{A_{\mathrm{eff}}}.1 counters per plane and counter dimensions λ(r)=ρμ(r)Aeff,ρμ(r)=λ(r)Aeff.\lambda(r)=\rho_\mu(r)\,A_{\mathrm{eff}}, \qquad \rho_\mu(r)=\frac{\lambda(r)}{A_{\mathrm{eff}}}.2. For LMDS, only the bottom plane is used, below an λ(r)=ρμ(r)Aeff,ρμ(r)=λ(r)Aeff.\lambda(r)=\rho_\mu(r)\,A_{\mathrm{eff}}, \qquad \rho_\mu(r)=\frac{\lambda(r)}{A_{\mathrm{eff}}}.3 m water layer that suppresses the electromagnetic component. Events are recorded when at least two bottom-plane counters fire, and LMDS are reconstructed from events with 3–40 hit counters. The effective zenith angle is taken as λ(r)=ρμ(r)Aeff,ρμ(r)=λ(r)Aeff.\lambda(r)=\rho_\mu(r)\,A_{\mathrm{eff}}, \qquad \rho_\mu(r)=\frac{\lambda(r)}{A_{\mathrm{eff}}}.4, assuming an angular distribution of muon bundles proportional to λ(r)=ρμ(r)Aeff,ρμ(r)=λ(r)Aeff.\lambda(r)=\rho_\mu(r)\,A_{\mathrm{eff}}, \qquad \rho_\mu(r)=\frac{\lambda(r)}{A_{\mathrm{eff}}}.5 (Kokoulin et al., 2017).

IceTop is located at altitude λ(r)=ρμ(r)Aeff,ρμ(r)=λ(r)Aeff.\lambda(r)=\rho_\mu(r)\,A_{\mathrm{eff}}, \qquad \rho_\mu(r)=\frac{\lambda(r)}{A_{\mathrm{eff}}}.6 km and atmospheric depth λ(r)=ρμ(r)Aeff,ρμ(r)=λ(r)Aeff.\lambda(r)=\rho_\mu(r)\,A_{\mathrm{eff}}, \qquad \rho_\mu(r)=\frac{\lambda(r)}{A_{\mathrm{eff}}}.7, and the measurement is quoted at an atmospheric depth of about λ(r)=ρμ(r)Aeff,ρμ(r)=λ(r)Aeff.\lambda(r)=\rho_\mu(r)\,A_{\mathrm{eff}}, \qquad \rho_\mu(r)=\frac{\lambda(r)}{A_{\mathrm{eff}}}.8. The array comprises 81 stations on a triangular grid with about λ(r)=ρμ(r)Aeff,ρμ(r)=λ(r)Aeff.\lambda(r)=\rho_\mu(r)\,A_{\mathrm{eff}}, \qquad \rho_\mu(r)=\frac{\lambda(r)}{A_{\mathrm{eff}}}.9 m spacing; each station has two water Cherenkov tanks about ρμmAeff(θ),\rho_\mu \approx \frac{m}{A_{\text{eff}}(\theta)},0 m apart. Signals are calibrated in units of Vertical Equivalent Muon (VEM). The analysis uses data from May 31, 2010 to May 2, 2013, corresponding to about ρμmAeff(θ),\rho_\mu \approx \frac{m}{A_{\text{eff}}(\theta)},1 live days and more than ρμmAeff(θ),\rho_\mu \approx \frac{m}{A_{\text{eff}}(\theta)},2 million selected events. The near-vertical requirement is ρμmAeff(θ),\rho_\mu \approx \frac{m}{A_{\text{eff}}(\theta)},3, and the reconstructed-energy threshold is ρμmAeff(θ),\rho_\mu \approx \frac{m}{A_{\text{eff}}(\theta)},4 PeV (Soldin, 2021).

3. Reconstruction of local muon density

In DECOR, muon bundles are identified through multiple reconstructed tracks consistent in direction and crossing DECOR planes. The conversion to local density is based on the effective area projected onto the plane perpendicular to the bundle direction, with acceptance and efficiency corrections from the established DECOR LMDS methodology. In this configuration, background from non-muon components is negligible for inclined bundles (Kokoulin et al., 2017).

In CTS, the bottom-plane hit multiplicity is converted to ρμmAeff(θ),\rho_\mu \approx \frac{m}{A_{\text{eff}}(\theta)},5 using the geometric counter coverage and plane area. A detector-specific correction is required because electromagnetic cascades and penetrating hadrons generated in building materials and water cause a systematic overestimation of ρμmAeff(θ),\rho_\mu \approx \frac{m}{A_{\text{eff}}(\theta)},6 by about ρμmAeff(θ),\rho_\mu \approx \frac{m}{A_{\text{eff}}(\theta)},7 in raw data. That factor was evaluated and corrected with Geant4 simulations of the CTS response (Kokoulin et al., 2017).

IceTop reconstructs the shower geometry, core, and size parameter ρμmAeff(θ),\rho_\mu \approx \frac{m}{A_{\text{eff}}(\theta)},8 with Hard Local Coincidence (HLC) signals, while muons are extracted mainly from Soft Local Coincidence (SLC) signals at large lateral distance, where the charge-versus-distance distribution exhibits the “Muon Thumb” near about ρμmAeff(θ),\rho_\mu \approx \frac{m}{A_{\text{eff}}(\theta)},9 VEM. In each mm0 bin, the SLC charge distribution is fitted with a log-likelihood multi-component model containing a muon response model, an electromagnetic signal model, and an accidental-background model. The muon response includes charge probability density functions for up to mm1 simultaneous muons; the EM component is represented by empirical models EM1 and EM2; and accidental background is modeled with a Poisson process based on off-time windows. The fit returns the mean number of muons per tank, mm2, and dividing by the tank projected area gives mm3 (Soldin, 2021).

The underlying stochastic model uses the Poisson law

mm4

with mm5, so that

mm6

IceTop denotes the raw reconstructed density by mm7. A small Monte Carlo bias is corrected with an energy-dependent factor

mm8

and the final density is

mm9

The applied correction is the average of the proton and iron corrections, and half of the proton–iron difference is assigned as a systematic uncertainty. The reconstructed Aeff(θ)A_{\text{eff}}(\theta)0 curves are then interpolated to the reference distances Aeff(θ)A_{\text{eff}}(\theta)1 m and Aeff(θ)A_{\text{eff}}(\theta)2 m (Soldin, 2021).

4. Spectral parameterizations and mapping to primary energy

The LMDS in a zenith bin are commonly represented by a power law,

Aeff(θ)A_{\text{eff}}(\theta)3

and, where a knee-like steepening is observed, by a broken power law

Aeff(θ)A_{\text{eff}}(\theta)4

In the NEVOD analysis, the two fitted density intervals correspond to primary-energy ranges Aeff(θ)A_{\text{eff}}(\theta)5–Aeff(θ)A_{\text{eff}}(\theta)6 eV and Aeff(θ)A_{\text{eff}}(\theta)7 eV, with the knee position Aeff(θ)A_{\text{eff}}(\theta)8 corresponding to a knee energy Aeff(θ)A_{\text{eff}}(\theta)9 eV. The mapping from θ\theta0 and θ\theta1 to primary energy is obtained from CORSIKA simulations; the contextual relation

θ\theta2

is cited, but explicit values of θ\theta3 and θ\theta4 are not quoted (Kokoulin et al., 2017).

A broader scaling framework is given in the combined analysis of eight air-shower experiments. The total muon number obeys

θ\theta5

with θ\theta6. For fixed θ\theta7, θ\theta8, and threshold, the local density scales similarly:

θ\theta9

If the cosmic-ray differential flux is rr00, then with rr01 one obtains the approximate LMDS scaling

rr02

This expresses how the event spectrum in primary energy is transferred into a spectrum in local muon density (Cazon, 2020).

The same mapping appears in size-spectrum analyses. If

rr03

then

rr04

Under a factorized muon LDF, LMDS at fixed rr05 follow

rr06

In this sense, LMDS inherit the same spectral information as muon-size spectra, while retaining explicit control of detector radius or fiducial band (Bijay et al., 2015).

For IceTop, the conversion from measured rr07 to a local muon density spectrum at fixed rr08 is written as

rr09

and

rr10

Above rr11 PeV, the IceTop efficiency is close to rr12 for all masses, so rr13 in the considered range (Soldin, 2021).

5. Measured spectral features and the second knee

The clearest direct LMDS feature reported in the supplied literature is a steepening above primary energies of about rr14 eV in NEVOD data. Both DECOR and CTS show an increase in the LMDS slope above that energy, interpreted as a “second knee” in the local muon density spectra (Kokoulin et al., 2017).

Data set Below-knee slope Above-knee slope
DECOR, combined inclined bins rr15 rr16
CTS, near-vertical rr17 rr18

For DECOR, the combined independent inclined bins give

rr19

which corresponds to about rr20 statistical significance. The individual DECOR fits are also reported: at rr21, rr22 in the rr23–rr24 eV interval; at rr25, rr26 below the knee and rr27 above; at rr28, rr29 above the knee. For CTS, the corresponding slope change is

rr30

or about rr31. In both setups the knee energy is again about rr32 eV, although the corresponding rr33 values are indicated in the spectra rather than tabulated (Kokoulin et al., 2017).

IceTop probes a lower energy domain with fixed-radius local densities rather than explicit broken-power-law LMDS fits. It reports rr34 at rr35 m for rr36–rr37 PeV and at rr38 m for rr39–rr40 PeV. The measured densities increase monotonically with energy at both reference radii. The internal consistency check is that densities are lower at rr41 m than at rr42 m for the same energy, while both radii show the same monotonic energy trend. The published results are graphical, with statistical error bars and bracketed systematic uncertainties; the paper does not provide numerical tables or explicit power-law fit coefficients for rr43 (Soldin, 2021).

6. Composition sensitivity and hadronic-interaction tests

Muon-density observables are explicitly composition sensitive. In IceTop, this is encoded in the parameter

rr44

where rr45 is the measured density and rr46 and rr47 are the proton and iron predictions of a given hadronic model. Values near rr48 are proton-like and values near rr49 are iron-like. The measured rr50 values are compared to expectations from the cosmic-ray flux models GSF, GST, and H3a (Soldin, 2021).

At IceTop energies, Sibyll 2.1 predictions agree with the measured rr51 within uncertainties for physically reasonable cosmic-ray flux models, at least up to about rr52 PeV. By contrast, EPOS-LHC and QGSJet-II.04 predict higher muon densities than Sibyll 2.1 and than the data over much of the rr53–rr54 PeV interval. At low energies below about rr55 PeV, the post-LHC models imply an unrealistically light composition if one attempts to force agreement through composition alone. In the IceTop analysis, Sibyll 2.1 yields rr56 values consistent with GSF, GST, and H3a within uncertainties, whereas EPOS-LHC and QGSJet-II.04 yield too-light compositions (Soldin, 2021).

The combined analysis introduces a universal reference scale,

rr57

for detector-level muon density estimates. If simulations are perfect, this scale maps linearly from rr58 for pure proton to rr59 for pure iron, with

rr60

To isolate model deviations from composition trends, the analysis fits

rr61

where rr62. The baseline slopes are rr63 for EPOS-LHC and rr64 for QGSJet-II.04, and robustness studies give rr65 to rr66 for EPOS-LHC and rr67 to rr68 for QGSJet-II.04. In all cases the slope differs from model expectations at more than rr69. Above about rr70 PeV, most experimental data show a muon excess relative to simulations, so the measured LMDS are shifted to higher local densities than the corresponding Monte Carlo predictions (Cazon, 2020).

This composition sensitivity also clarifies why LMDS and charged-particle spectra can lead to different inferences near a knee. In the Monte Carlo study of simultaneous charged and muon spectra, the mapping

rr71

implies that the muon-spectrum or LMDS break tracks the primary-spectrum break in a manner that is less sensitive to abrupt composition changes than the charged-particle spectrum. In the simulated imposed-knee examples, the muon-spectrum break remains at rr72–rr73, whereas the charged-particle break can vary much more strongly, reaching rr74 in a rr75 transition (Bijay et al., 2015).

7. Uncertainties, cross-calibration, and interpretive limits

The systematic budget depends strongly on the detector implementation. In IceTop, four dominant sources are identified. The energy scale and resolution translate to about rr76 uncertainty in rr77; the EM signal model choice, assessed by comparing EM1 and EM2, induces up to about rr78 uncertainty; the Monte Carlo correction factor depends on composition and on hadronic model choice; and detector-related effects such as snow attenuation and VEM calibration are folded into the energy and EM-model systematics. Statistical uncertainties are shown as error bars and systematic uncertainties as brackets around the points (Soldin, 2021).

In NEVOD, DECOR quotes a track-reconstruction accuracy better than rr79, and acceptance and efficiency follow established procedures, but systematic uncertainties on the fitted rr80 values are not itemized separately in the paper. For CTS, the principal explicit correction is the Geant4-derived factor of about rr81 accounting for accompanying particles under building materials and water. The residual systematic effect of that correction on the LMDS slopes is not numerically quoted (Kokoulin et al., 2017).

Cross-experiment synthesis introduces an additional calibration layer. Because rr82 with rr83, even a rr84 energy-scale offset induces about an rr85 offset in muon density. The combined analysis therefore cross-calibrates energy scales using the isotropic cosmic-ray flux as reference. The residual uncertainty of the cross-calibrated energy scale is at least rr86, implying a collective uncertainty of about rr87 in the rr88 scale. The same study emphasizes that measurements span a wide range of rr89 values, lateral distances, and effective production-energy thresholds, with rr90 spanning about rr91–rr92 GeV; extreme zenith angles such as rr93 add complications from atmospheric-density gradients, rr94 critical energies, and effective core distance for muon bundles (Cazon, 2020).

Several formal limitations remain explicit in the source literature. IceTop does not tabulate rr95 values or analytic fit coefficients for rr96, so exact numerical LMDS at rr97 m and rr98 m require digitizing the plotted points or using a supplemental data release if available. In the NEVOD second-knee analysis, the knee positions rr99 are indicated graphically rather than tabulated, and the specific hadronic-interaction models used in the CORSIKA energy mapping are not stated. These omissions do not alter the reported qualitative results, but they constrain exact reproduction of LMDS parameterizations from the text alone (Soldin, 2021, Kokoulin et al., 2017).

Taken together, the supplied studies establish LMDS as a compact but information-rich muon observable. At detector level, LMDS encode the local muon content of showers across fixed geometry and threshold conditions; through simulation or fitted scaling relations they map onto primary energy; and through proton–iron bracketing they become composition diagnostics. The published measurements show both a second-knee steepening around λ(r)\lambda(r)00 eV in NEVOD LMDS and, in the broader PeV-to-EeV comparison, an energy-growing muon excess above about λ(r)\lambda(r)01 PeV relative to recent hadronic-interaction models (Kokoulin et al., 2017, Cazon, 2020).

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