Introduction
Transmission muography, which utilizes naturally existing cosmic-ray muons, images the internal structures of objects penetrated by muons. Because of their high average energy (~4 GeV at the sea level [1]), cosmic-ray muons have strong penetrating power and nearly straight-line trajectories. Additionally, they are ubiquitous on Earth. These characteristics make cosmic-ray muons particularly suitable for the nondestructive imaging of large-scale objects such as volcanoes [2-4], faults [5-7], mineral deposits [8-11], cultural heritage [12-16], and nuclear reactors [17-19].
The flux attenuation due to the energy loss of muons interacting with matter relates to both the thickness and density of the material penetrated by the muons. Analyzing the cosmic-ray muon flux detected from a single view and combining it with prior topographic information yield the average density along the line of sight, allowing for the identification of density anomalies within the object. This 2D transmission muography ("muon radiography") has a limitation: the density map is only a 2D projection. This introduces ambiguities when internal structure is complex, as density anomalies may overlap along the measurement direction, creating degenerate structures. To reduce this ambiguity, obtaining 3D information requires at least two different views of cosmic-ray muon flux measurements to locate density anomalies. In the ScanPyramids experiment of the Khufu Pyramid in 2017 [12], three independent muon measurements were conducted, each using two distinct observation positions for triangulation. The resulting locations were consistent across all three analyses, providing high-confidence confirmation of the hidden chamber. The positions from the three analyses agreed, confirming the discovery. With muon flux data from multiple views, reconstructing the 3D density distribution becomes possible—this approach is called "muon tomography."
Owing to the characteristics of cosmic-ray muons, muon tomography presents two major challenges. First, because of the relatively low flux of cosmic-ray muons, which is approximately 1 cm-2 min-1 at the sea level [1], the number of views is limited by both the experimental time and the availability of muon detectors. Additionally, the choice of detector sites is constrained given that the structure under test in transmission muography is often a large-scale object located in the field, and the surroundings are complicated. Consequently, the image reconstruction problem in muon tomography is often under-constrained, potentially leading to ambiguous results. Second, fluctuations in cosmic-ray muon flux data can disturb image reconstruction in muon tomography, including statistical fluctuations caused by the low statistics of cosmic-ray muons and directional fluctuations caused by multiple Coulomb scattering of muons penetrating objects [20].
To address the two challenges mentioned above, efforts can be made from two perspectives: combining cosmic-ray muon data with other types of geophysical data for joint inversion and improving image reconstruction algorithms. From the perspective of joint inversion, both transmission muography and gravimetry are sensitive to the density of objects, making them naturally suitable for joint inversion. Thus, muon data are often combined with gravity data for such inversions. Several studies have reported inversion results that combine cosmic-ray muon data with gravity data. For instance, Nishiyama et al. combined single-view cosmic-ray muon data with gravity data obtained from 30 gravity stations to reconstruct the 3D density structure of the Showa-Shinzan lava dome. They also demonstrated (through the inversion of synthesized data) that the results of joint inversion using both gravity and cosmic-ray muon data had better resolution than that obtained using only gravity data [21]. However, Jourde et al. noted in their study that when an object is covered by cosmic-ray muon data from more than two viewpoints, the improvement in image quality from adding gravity data is insignificant [22].
For enhancing image reconstruction algorithms, establishing robust algorithms with strong noise resistance is crucial, as muon tomography involves reconstructing images from noisy and incomplete data. The algorithms for 3D image reconstruction in muon tomography fall into two main categories. The first is the linear inversion method based on Bayesian principles, widely used in geophysical model inversion and applicable to muon tomography. Nagahara et al. used linear inversion to reconstruct the 3D density distribution of the Omuroyama scoria cone from cosmic-ray muon data from 10 viewpoints [23]. Barnoud et al. used this method for joint inversion of single-view cosmic-ray muon data and gravimetric data to reconstruct the Puy de Dôme volcano’s 3D density structure [24]. However, this method requires careful tuning of multiple a priori parameters that affect inversion results, and density smoothing constraints may blur density anomaly boundaries [25]. The second category is algebraic reconstruction techniques, commonly used in medical CT image reconstruction and suitable for incomplete and noisy data. Erlandson et al. used the algebraic reconstruction technique (ART) algorithm for cosmic-ray muon tomography reconstruction of the ZED-2 research reactor [26]. S. Procureur reconstructed images of a simulated concrete cube with cavities using the simultaneous ART algorithm [27]. Hartling et al. simulated a 12-view muon tomography for a cylindrical model containing a uranium rod and compared various iterative reconstruction algorithms, concluding that the simultaneous iterative reconstruction technique (SIRT) is a suitable algorithm for muon tomography reconstruction [28]. Compared to the classic ART algorithm, the SIRT algorithm can better suppress noise.
Additional information can be incorporated into the SIRT algorithm to further improve the reconstructed image quality. Total-variation (TV) minimization is an effective constraint. Signals or images with transform sparsity can be reconstructed from a small number of samples by minimizing the L1-Norm of the transform coefficients [29-31]. For piecewise constant images, their gradient-magnitude images meet the transform sparsity condition, and TV is the L1-Norm of gradient-magnitude image. Therefore, TV-minimization-based image reconstruction algorithms may achieve high-precision reconstruction from a limited number of views [32, 33]. The density distribution of large cultural heritage structures, such as the Khufu Pyramid is piecewise constant, making them suitable for TV-minimization. Therefore, combining SIRT with TV-minimization could enhance the quality of muon tomography reconstruction images for such cases.
In 2022, our group reported the preliminary results of a cultural heritage muon radiography simulation study based on the archaeological data of the QinShiHuang tomb. This study demonstrated that muon radiography could identify the inner structures of the underground palace, including the tomb chamber, walls, and rammed earth. The length, width, and burial depth of the tomb chamber were estimated from the muon radiography simulation results obtained from two viewpoints [34]. Based on previous research, in this study, we performed 3D image reconstruction for muon tomography of the QinShiHuang tomb. A digital phantom built based on the archaeological data of the QinShiHuang tomb, was used for the transmission muography simulation in Geant4 and for testing the image reconstruction algorithm. The SIRT-TV algorithm, which combined SIRT and TV minimization, was applied to the image reconstruction of 12-view muon tomography images. The remainder of this paper is organized as follows. Section 2 introduces the principles of transmission muography and the SIRT-TV algorithm. Section 3 describes the simulation setup and presents the 2D slices of the reconstructed images obtained using the SIRT-TV and SIRT algorithms. The slices reconstructed using the two algorithms, with the same number of iterations, are compared visually. Section 4 evaluates the reconstructed image quality based on the geometric-similarity index for the structures of the underground palace, providing a quantitative comparison between SIRT and SIRT-TV. This section also discusses some factors that may influence the reconstructed image quality, including the value of the TV-minimization algorithm parameters, the number of views in muon tomography, and the statistics of the muon data. The final section concludes the study.
Methods
Principles of muon radiography
When passing through an object, muons interact with the matter and lose energy through ionization, bremsstrahlung, pair production, and photonuclear reactions. The energy loss behavior can generally be described as


Combining Eqs. (1)–(3) and the sea-level cosmic-ray muon energy spectrum model, the density length of the object in different directions can be obtained, resulting in a 2D projection map of the object’s density length X.
3D image reconstruction of muon tomography
Based on a 2D projection map of X obtained from Sect. 2.1, the 3D density distribution can be solved for. Let m be the number of directions. By uniformly dividing the 3D region of interest (ROI) into n voxels, the integral 

Because the density length data are obtained from cosmic-ray muon flux data, which are usually noisy and incomplete, the linear equations in Eq. (5) faces issues such as being underdetermined and inconsistent and having a large sparse system matrix. Algebraic reconstruction techniques are commonly employed to address these problems. The most basic algebraic reconstruction algorithm is the ART algorithm [37], which is based on the Kaczmarz optimization algorithm. The ART principle can be understood as the gradual projection of a trial solution onto the hyperplanes determined by each equation to obtain a new solution. If the system of equations has a unique solution, then the trial solution converges iteratively. In every iteration of the ART algorithm, each equation of Eq. (5) updates ρ once. This equation-by-equation update method is sensitive to noise and can cause divergence if the noise is severe. The SIRT algorithm was developed based on the basic ART algorithm [38]. In each iteration of the SIRT algorithm, the contribution of each equation to ρ is first calculated without updating ρ. After going through all the equations, their contributions are averaged and ρ is updated accordingly. The updated equation for SIRT is
Both ART and SIRT solve the reconstruction problem based solely on the projection data X, without introducing additional constraints. However, muon tomography often lacks sufficient views, resulting in the ill-posedness of the image reconstruction. To improve the quality of the reconstructed image further, additional constraints must be introduced during the reconstruction procedure. We observed that the density distribution of the targets in the muon tomography analysis typically exhibited piecewise constancy, indicating that its gradient-magnitude image was sparse. This feature allowed using TV minimization as a constraint.
Let the voxel density at the coordinates 






Simulation and reconstruction
Muography simulation
The simulation is performed using Geant4, which is a Monte Carlo toolkit developed by CERN based on C++ [39]. Geant4 can simulate the transport and interactions of particles in matter and is a commonly used and reliable simulation platform for transmission muography. The simulation model can be divided into three parts: the QinShiHuang tomb phantom, muon track detector, and cosmic-ray muon source.
The QinShiHuang tomb was studied using 20 geophysical approaches as part of the National 863 Hi-tech Project. Archaeological results confirmed the depth of the underground palace, as well as the size and location of the tomb chamber and surrounding walls [40]. Based on these archaeological data, we built a phantom model of the QinShiHuang tomb for our simulation, which included the mound, rammed earth, loam wall, stone wall, burial chamber, and surrounding land, as shown in Fig. 2.

The cosmic-ray muon source is sampled using the Reyna formula [41]:
The coordinate system is defined as shown in Fig. 2(b)–(d). The muon track detector is a 1 m × 1 m ideal detector placed horizontally, recording cosmic-ray muons’ direction. The detector positions are 5 m away from the underground palace boundaries. Notably, 12 detector locations are evenly spaced at 30° surrounding the palace center, numbered 1 to 12, as shown in Fig. 2(b). Because cosmic-ray muons travel downward, detectors must be positioned below the palace level to ensure that the field of view covers the ROI. The detector depth affects the angular size of the ROI, overburden thickness, and muon zenith angles. We set the detectors’ burial depth to 90 m, as shown in Fig. 2(c), where maximum zenith angle of muons crossing ROI is 75°. Following Ref. [42], we determined the minimum muon energy required to reach the detector through the phantom, sampling only muons above this threshold. The simulated cosmic-ray muon statistics per view equal a 180-d physical measurement.
Image reconstruction
Since the tomb phantom is much larger than the detectors, they are treated as points for calculating muon flux and density length maps. Simulated cosmic-ray muon fluxes after penetrating the QinShiHuang tomb phantom, detected by each detector, are divided into 75 × 180 directions by zenith and azimuth angles, as shown in Fig. 3. Each pixel’s direction in Fig. 3 is represented by its center coordinate. The minimum energy Emin of cosmic-ray muons penetrating the phantom is calculated using Eq. (3). For density length conversion, Geant4 simulates the average muon penetration range in loess, with results in Fig. 4. A second-order polynomial is fitted to the curve in Fig. 4.


Since we are interested in the underground palace structure, we define the ROI as shown in Fig. 2(c) and (d) and perform 3D reconstruction for density distribution within the ROI. The density length data from different directions includes contributions from inside and outside the ROI. For the tomb phantom, knowing the density distribution outside the ROI allows us to calculate its density length. Subtracting this from the obtained data gives density length within the ROI, as shown in Fig. 5. Some directions have negative density length values due to cosmic-ray muon flux fluctuations. Only non-negative values are used in reconstruction.

In 3D image reconstruction, the ROI is divided into 60 × 50 × 20 voxels, with a voxel size of 3 m × 3.2 m × 4 m. This voxelization ensures appropriate voxel numbers for solving linear equations in Eq. (5) while maintaining resolution for fine structure reconstruction. SIRT and SIRT-TV reconstruct images from the same density length data for comparison. Following Ref. [32], we set λ=1, α=0.2, and NTV=20. Initial density values are set to ρ0=1.6 g/cm3, matching the loess density in the phantom. Both algorithms iterate Nmax=50 times. An additional constraint in each iteration restricts voxel density outside the burial mound to 0.00129 g/cm3, matching the phantom’s air density. Slices at three representative locations are selected for comparison with phantom slices, as shown in Fig. 6.

A comparison of the reconstructed image slices, obtained by the two algorithms, with those of the phantom reveals that the shapes and positions of the tomb chamber and walls in the SIRT-TV reconstruction results match those of the phantom. By contrast, the slices obtained using the SIRT algorithm exhibit significant salt-and-pepper artifacts, particularly at the bottom of the reconstructed image, around the tomb chamber, and at the top of the burial mound. These artifacts can potentially lead to misinterpretation of the underground palace’s structure. The reconstruction results obtained using SIRT-TV do not show such significant artifacts, preliminarily verifying that the inclusion of TV minimization can effectively suppress artifacts.
Discussion
Reconstructed image quality assessment
Figure 6 shows a visual comparison of the reconstructed images obtained using SIRT and SIRT-TV. However, visual comparison lacks quantitative information and is noncomprehensive because the reconstructed images are 3D. To quantitatively compare the reconstruction results of SIRT and SIRT-TV, using appropriate image quality assessment metrics is crucial. Classic metrics include mean squared error (MSE), peak signal-to-noise ratio (PSNR), and structural similarity (SSIM) [43]. These metrics can evaluate the overall similarity between the reconstructed image and phantom. However, this study is primarily focused on the feasibility of accurately reconstructing the structures of the underground palace, specifically the tomb chamber and walls. Referring to the image quality assessment metrics used in Refs. [28], we use the Jaccard similarity index J to assess the geometric similarity of the reconstructed images to the phantom for the tomb chamber and walls. J is defined as follows:






Both the wall and tomb chamber geometries in the SIRT reconstruction result show noticeable overflow compared to the phantom. In contrast, the counterparts extracted from the SIRT-TV reconstructed image align better with the phantom. Table 1 lists the J-calculation results for the structures in the reconstructed images obtained using the two algorithms. Both Jchamber and Jwall in the SIRT-TV reconstruction results are superior to those obtained using SIRT. In particular, Jwall is 2.8 times that of SIRT.
| Algorithm | ||
|---|---|---|
| SIRT-TV | 0.5929 | 0.5498 |
| SIRT | 0.4611 | 0.1978 |
Iterative convergence
Convergence speed is an important metric for evaluating iterative image reconstruction algorithms. In Sect. 4.1, Jchamber and Jwall of the reconstruction results are compared after the same number of iterations for both algorithms. However, the number of iterations required for each algorithm to converge may differ. To compare the convergence speeds of the two algorithms, they were iterated 150 times, and the curves showing the changes in Jchamber and Jwall with the number of iterations are plotted in Fig. 8. Jchamber and Jwall of SIRT-TV generally increased with the number of iterations until convergence, whereas those for SIRT initially increased but then decreased with additional iterations before convergence.

To quantitively evaluate the convergence speed, we defined a convergence metric as follows:
Impact of TV parameters on reconstruction
The parameter values in the TV-minimization algorithm may affect the quality of the reconstructed images. To assess this impact, we varied the maximum iteration number NTV and the TV gradient descent step size α. Jchamber and Jwall are shown as functions of the number of iterations for different parameter values in Fig. 9.

For most
Overall, the different parameter values in Fig. 9 (except NTV=10 or α=0.1) do not significantly affect the reconstruction results, indicating that the SIRT-TV algorithm can reliably produce high-quality images.
Impact of measurement configuration and duration
As mentioned in Sect. 1, the main challenges in 3D reconstruction of muon tomography are the presence of noise and incomplete data. In Sect. 3, we simulated relatively ideal conditions to test the feasibility of the algorithm. This section discusses the impact of less-ideal measurement configurations and durations (i.e., fewer views and lower muon statistics) on reconstruction with SIRT-TV.
Measurement configuration
Using the same simulation data from Sect. 3, the number of views is reduced to four, and three different detector configurations are selected for reconstruction. The parameters of the image reconstruction algorithm were the same as those used in Sect. 3. Figure 10 shows slices of the phantom and the reconstructed images for the 12-view and three 4-view configurations. Reducing the number of views leads to more severe artifacts. Among these 4-view configurations, the symmetrical 4-view configuration shows better geometric symmetry in its reconstruction results, whereas the reconstruction results for the other two 4-view configurations exhibit distortions in the shapes of the tomb chamber and walls. The calculation results of Jchamber and Jwall in Table 2 also indicate that, among the three different 4-view configurations, the reconstructed image quality is the highest for the symmetrical 4-view configuration. These artifacts can be explained by the ray densities in the voxels. Given that the voxelization for each reconstruction is the same, more views lead to more rays, higher ray densities in the voxels, and more information regarding voxel density. When voxelization and the number of views were the same for each reconstruction, asymmetrical measurement configurations caused greater variation in ray densities across voxels. This implies that some voxels are crossed by only a few rays, making it difficult to reconstruct their densities. A symmetrical measurement configuration results in better reconstruction quality.

| Measurement configuration | ||
|---|---|---|
| 12-view | 0.5929 | 0.5498 |
| 4-view configuration 1 | 0.5161 | 0.4552 |
| 4-view configuration 2 | 0.4818 | 0.4452 |
| 4-view configuration 3 | 0.4576 | 0.3777 |
Measurement duration
The number of cosmic-ray muons detected by the detectors is proportional to the measurement duration. This affects the statistical fluctuations, which, in turn, affects the quality of the reconstructed image. To investigate the reconstructed image quality for different measurement durations, we select datasets from the beginning of the simulation data in Sect. 3, corresponding to 7, 14, 30, 90, and 180 d of equivalent measurement time. The algorithm parameters are the same as those used in Sect. 3. Slices of the reconstructed images are shown in Fig. 11.

In the reconstructed image slices for 7-d and 14-d measurement durations, severe artifacts appear between the chamber and walls, especially at the bottom. For measurement durations beyond 30 d, artifacts are suppressed, and the chamber-earth boundary becomes clearer. The 90-d and 180-d reconstructed image slices show similar results, with Jchamber and Jwall both
| Time (day) | ||
|---|---|---|
| 7 | 0.2615 | 0.2050 |
| 14 | 0.4514 | 0.2465 |
| 30 | 0.5123 | 0.3383 |
| 90 | 0.5525 | 0.4994 |
| 180 | 0.5929 | 0.5498 |
Conclusion
In this study, we simulated 3D image reconstruction of muon tomography for the QinShiHuang tomb phantom using the SIRT-TV algorithm. The results show that compared to SIRT, the SIRT-TV algorithm effectively suppresses salt-and-pepper artifacts, improves geometric similarity Jchamber by nearly one-third and Jwall by nearly twofold, and converges faster. This result indicates that SIRT-TV is more suitable for 3D image reconstruction of large-scale cultural heritage muon tomography. Using this algorithm with 12-view cosmic-ray muon data, locations and shapes of the tomb chamber and walls are reconstructed.
We investigated TV-minimization algorithm parameters’ impact on image quality by varying maximum iteration number NTV and TV gradient descent step size α. While optimal TV parameters differ between walls and tomb chamber reconstruction, selecting parameters within a reasonable range achieves high-quality reconstructions. Considering the potential constraints in experiments, this paper also discusses the impact of measurement configurations and durations on the reconstruction results. The results show that reducing the number of views from 12 to 4 decreases J. Among the 4-view configurations, J values are highest when detectors are positioned along ROI symmetry axes. For 12-view configuration, J values increase with equivalent measurement duration, with both Jchamber and
Although SIRT-TV shows improved reconstruction quality compared to SIRT, enhancement opportunities remain: walls with different densities remain indistinguishable, and geometric similarity J can be improved. Future work could enhance image quality through machine learning techniques, using reconstructed images from varying viewpoints as training inputs.
While the QinShiHuang tomb phantom is simplified, it retains essential structural features of the underground palace. As a well-known imperial tomb, its structure is likely representative, and this simulation would provide insights for potential transmission muography experiments on other imperial tombs.
Review of particle physics
. Prog. Theor. Exp. Phys. 2020,Method of probing inner-structure of geophysical substance with the horizontal cosmic-ray muons and possible application to volcanic-eruption prediction
. Nucl. Instrum. Methods Phys. Res. Sect. A-Accel. Spectrom. Dect. Assoc. Equip. 356, 585–595 (1995). https://doi.org/10.1016/0168-9002(94)01169-9Three-dimensional computational axial tomography scan of a volcano with cosmic ray muon radiography
. J. Geophys. Res.-Solid Earth 115,Imaging internal density structure of the Laoheishan volcanic cone with cosmic ray muon radiography
. Nucl. Sci. Tech. 33, 88 (2022). https://doi.org/10.1007/s41365-022-01072-4Cosmic muon imaging of hidden seismic fault zones: rainwater permeation into the mechanical fractured zones in Itoigawa–Shizuoka Tectonic Line, Japan
. Earth Planet. Sci. Lett. 306, 156–162 (2011). https://doi.org/10.1016/j.epsl.2011.03.036Muography of 1949 fault in La Palma, Canary Islands, Spain
. Ann. Geophys. 60, 9 (2017). https://doi.org/10.4401/ag-7385Development of detector and method for density structure measurement of fault zones using cosmic ray muons
. Nucl. Instrum. Methods Phys. Res. Sect. A-Accel. Spectrom. Dect. Assoc. Equip. 1031,Blind test of muon geotomography for mineral exploration
. ASEG Extended Abstracts 2015, 1–3 (2015). https://doi.org/10.1071/ASEG2015ab054Muon tomography applied to a dense uranium deposit at the McArthur River Mine
. J. Geophys. Res.-Solid Earth 123, 8637–8652 (2018). https://doi.org/10.1029/2018JB015626Deep investigation of muography in discovering geological structures in mineral exploration: a case study of Zaozigou gold mine
. Geophys. J. Int. 237, 588–603 (2024). https://doi.org/10.1093/gji/ggae057Discovery of a big void in Khufu’s Pyramid by observation of cosmic-ray muons
. Nature 552, 386–390 (2017). https://doi.org/10.1038/nature246473D Muography for the search of hidden cavities
. Sci. Rep. 9, 2974 (2019). https://doi.org/10.1038/s41598-019-39682-5Muography as a new tool to study the historic earthquakes recorded in ancient burial mounds
. Geosci. Instrum. Methods Data Syst. 9, 357–364 (2020). https://doi.org/10.5194/gi-9-357-2020High-precision muography in archaeogeophysics: a case study on Xi’an defensive walls
. J. Appl. Phys. 133, 14901 (2023). https://doi.org/10.1063/5.0123337Muography as a support technique for non-invasive research and three-dimensional localization of tombs in archaeological sites: a case study from Palazzone Necropolis (Perugia–Italy)
. J. Instrum. 19,Performance of a remotely located muon radiography system to identify the inner structure of a nuclear plant
. Prog. Theor. Exp. Phys. 2013,Cosmic-ray muon radiography for reactor core observation
. Ann. Nucl. Energy. 78, 166–175 (2015). https://doi.org/10.1016/j.anucene.2014.12.017Investigation of the Unit-1 nuclear reactor of Fukushima Daiichi by cosmic muon radiography
. Prog. Theor. Exp. Phys. 2020,Influence of multiple Coulomb scattering on accuracy of muon transmission imaging of small-scale matter
. Acta Phys. Sin. 72,Integrated processing of muon radiography and gravity anomaly data toward the realization of high-resolution 3-D density structural analysis of volcanoes: case study of Showa-Shinzan lava dome, Usu, Japan
. J. Geophys. Res.-Solid Earth 119, 699–710 (2014). https://doi.org/10.1002/2013JB010234Improvement of density models of geological structures by fusion of gravity data and cosmic muon radiographies
. Geosci. Instrum. Methods Data Syst. 4, 177–188 (2015). https://doi.org/10.5194/gi-4-177-2015Three-dimensional density tomography determined from multi-directional muography of the Omuroyama scoria cone, Higashi–Izu monogenetic volcano field, Japan
. Bull. Volcanol. 84, 94 (2022). https://doi.org/10.1007/s00445-022-01596-yRobust Bayesian joint inversion of gravimetric and muographicdata for the Density Imaging of the Puy de Dôme volcano (France)
. Front. Earth Sci. 8,The research on Bayesian inference for geophysical inversion
. Reviews of Geophysics and Planetary Physics 53, 159–171 (2022). https://doi.org/10.19975/j.dqyxx.2021-042One-sided muon tomography—a portable method for imaging critical infrastructure with a single muon detector
. arXiv:1605.01565 (2016). https://doi.org/10.48550/arXiv.1605.01565. arXiv:1605.01565Muon tomography of large structures with 2D projections
. Nucl. Instrum. Methods Phys. Res. Sect. A-Accel. Spectrom. Dect. Assoc. Equip. 1013,A comparison of algebraic reconstruction techniques for a single-detector muon computed tomography system
. Nucl. Instrum. Methods Phys. Res. Sect. A-Accel. Spectrom. Dect. Assoc. Equip. 987,Robust uncertainty principles: exact signal reconstruction from highly incomplete frequency information
. IEEE Trans. Inf. Theory 52, 489–509 (2006). https://doi.org/10.1109/TIT.2005.862083Stable signal recovery from incomplete and inaccurate measurements
. Commun. Pure Appl. Math. 59, 1207–1223 (2006). https://doi.org/10.1002/cpa.20124Compressed sensing
. IEEE Trans. Inf. Theory 52, 1289–1306 (2006). https://doi.org/10.1109/TIT.2006.871582Accurate image reconstruction from few-views and limited-angle data in divergent-beam CT
. J. X-Ray Sci. Technol. 14, 119–139 (2006). https://doi.org/10.3233/XST-2006-00155Image reconstruction in circular cone-beam computed tomography by constrained, total-variation minimization
. Phys. Med. Biol. 53, 4777–4807 (2008). https://doi.org/10.1088/0031-9155/53/17/021Muon radiography simulation for underground palace of Qinshihuang Mausoleum
. Acta Phys. Sin. 71, 64201 (2022). https://doi.org/10.7498/aps.71.20211582Muon stopping power and range tables 10 MeV–100 TeV
. Atom. Data Nucl. Data Tables 78, 183–356 (2001). https://doi.org/10.1006/adnd.2001.0861A comparison of muon flux models at sea level for muon imaging and low background experiments
. Front. Energy Res. 9,Algebraic reconstruction techniques (ART) for three-dimensional electron microscopy and X-ray photography
. J. theor. Biol. 29, 471–481 (1970). https://doi.org/10.1016/0022-5193(70)90109-8Iterative methods for the three-dimensional reconstruction of an object from projections
. J. Theor. Biol. 36, 105–117 (1972). https://doi.org/10.1016/0022-5193(72)90180-4Geant4—a simulation toolkit
. Nucl. Instrum. Methods Phys. Res. Sect. A-Accel. Spectrom. Dect. Assoc. Equip. 506, 250–303 (2003). https://doi.org/10.1016/S0168-9002(03)01368-8A simple parameterization of the cosmic-ray muon momentum spectra at the surface as a function of zenith angle
. arXiv:hep-ph/0604145 (2006). https://doi.org/10.48550/arXiv.hep-ph/0604145Fast simulation study of muon absorption radiography based on energy loss calculation
. At. Energy Sci. Technol. 56, 2765–2772 (2022). https://doi.org/10.7538/yzk.2022.youxian.0509Image quality assessment: from error visibility to structural similarity
. IEEE Trans. Image Process. 13, 600–612 (2004). https://doi.org/10.1109/TIP.2003.819861Yuan-Yuan Liu is an editorial board member for Nuclear Science and Techniques and was not involved in the editorial review, or the decision to publish this article. All authors declare that there are no competing interests.

