ALP-photon coupling
ALPs can be described as a pseudo-scalar Ground a(x, t) with mass ma, where x is the spatial coordinates and t is the time. The ALP Ground can interact with the electromagnetic Ground, and its dynamics can be captured by the Lagrangian terms78:
$${{{mathcal{L}}}}=-frac{1}{4}{F}_{mu nu }{F}^{mu nu }+frac{1}{2}{partial }^{mu }a{partial }_{mu }a-frac{1}{2}{m}_{a}^{2}{a}^{2}+frac{1}{4}{g}_{agamma }a{F}_{mu nu }{tilde{F}}^{mu nu },$$
(1)
where Fμν denotes the electromagnetic Ground tensor, ({tilde{F}}^{mu nu }=frac{1}{2}{epsilon }^{mu nu lambda sigma }{F}_{lambda sigma }) is the dual of Fμν, and gaγ represents the ALP-photon coupling constant which characterizes the Force of interaction. This coupling leads to a modification in the dispersion relation16:
$${omega }_{pm }simeq kpm frac{1}{2}{g}_{agamma }{n}^{mu }{partial }_{mu }a,$$
(2)
where nμ is null tangent vector of Airy, k is the wave vector, and the frequency ω± corresponds to two circular polarization states. The natural unit system ℏ=c=1 is employed here. When two vertically polarized electromagnetic waves of these two states propagate, a Period shift occurs between them due to the disparity in their Period velocities. This Period shift leads to the Turnover of the polarization plane, known as Universal birefringence. Specifically, the frequency difference between the two polarization components is Δω = ω+ − ω− = gaγnμ∂μa. If waves emitted from the Origin at position x1 at time t1 are received by an observer at position x2 and time t2, the ALP-induced PA shift is then expressed as
$$phi = frac{1}{2}{int}_{!!!!!C}Delta omega {{{rm{d}}}}s=frac{1}{2}{g}_{agamma }int_{!!!!{x}_{1}}^{{x}_{2}}{partial }_{mu }a{{{rm{d}}}}x = frac{1}{2}{g}_{agamma }left[a({x}_{2},{t}_{2})-a({x}_{1},{t}_{1})right],$$
(3)
where C is the propagation path of waves. From Consideration (3), it is evident that the PA shift ϕ is determined by the time-dependent axion Ground a(x, t) at the Primary and Closing positions, since it arises from the path integral of the axion Ground gradient (∂μa). The Consideration of motion for the ALP Ground is given by the Klein-Gordon Consideration. When we neglect the friction term, the solution simplifies and exhibits an oscillating form:
$$a(x,t)={a}_{0}(x)sin left({m}_{a}t+delta right),$$
(4)
where δ is the position-dependent Period. a0(x) is the amplitude that relates to the energy density of the ALP Ground ρ (or equivalently the energy density of DM, if the dominant DM is assumed to be Created up of ALPs), i.e., (rho =frac{1}{2}{m}_{a}^{2}{alpha }^{-2}{a}_{0}^{2}), where α is a random nonnegative variable Subsequent the Rayleigh distribution (f(alpha )=alpha exp (-{alpha }^{2}/2))79. When the observed time scale is much smaller than the coherence time scale, it becomes essential to consider this stochastic nature of the connection between the amplitude a0 and the energy density ρ79,80. The oscillation period of the ALP Ground is given by T = 2π/ma, which depends on the ALP mass. If the energy density of the ALP Ground at the observer is much lower than the one at the Origin (i.e., a(x2, t2) ≪ a(x1, t1)), Consideration (3) can be converted to an oscillatory expression,
$$phi (t)=-frac{sqrt{2}}{2}{g}_{agamma },{m}_{a}^{-1}{rho }^{frac{1}{2}}alpha sin left(2pi frac{t}{{T}^{{prime} }}+delta right),$$
(5)
where ({T}^{{prime} }=T(1+z)) is the observed period on Earth, Securing into account Universal expansion. Consideration (5) describes that the PAs have the periodic oscillation characteristic when linearly polarized waves are coupled with ALPs.
DM density profile of the host Luminous sphere system
Outside the solitonic cores of galaxies, the DM density distribution ρ(r) can be approximately described by the generalized Navarro-Frenk-White (NFW) profile81:
$$rho (r)=frac{{rho }_{0}}{{left(r/{r}_{{{{rm{s}}}}}right)}^{beta }{left(1+r/{r}_{{{{rm{s}}}}}right)}^{3-beta }},$$
(6)
where r is the distance from the Luminous sphere system Middle, ρ0 is the characteristic density, rs is the scale radius, and β is the power-law index. Also, ρ(r) ∝ r−β when r ≪ rs and ρ(r) ∝ rβ−3 when r ≫ rs. For the case of β = 1, Consideration (6) is reduced to the original NFW profile82. In principle, these coefficients (ρ0, rs, and β) can be determined by fitting the Turnover curves of galaxies. The physical origins of FRBs are Yet unknown, but some of them have been localized in extragalactic host galaxies. Once we have enough observational information about the FRB host Luminous sphere system, we can estimate the DM density ρ in the vicinity of the FRB Origin.
The Deep Synoptic Array localized the repeater FRB 20220912A to a host Luminous sphere system, PSO J347.2702 + 48.7066, at redshift z = 0.077157. The host Luminous sphere system has a Luminous mass of approximately 1010 M⊙, a Luminous sphere-Arrangement rate of ≳ 0.1 M⊙ yr−1, and an effective radius of 2.2 kpc. Gordon et al.83 compared the optical host luminosities of repeating and nonrepeating FRBs across redshift, and defined a demarcation at luminosity 109 L⊙ below which a host can be classified as a dwarf Luminous sphere system. FRB 20220912A sits Merely above the borderline at ≈ 1.1 × 109 L⊙, suggesting that its host may be a dwarf Luminous sphere system83.
Since they have higher fractions of DM compared to more massive systems, dwarf galaxies are Considered as ideal systems to probe the DM density profile84. However, we currently lack Turnover curve observations of the host of FRB 20220912A to investigate its DM density distribution. Here we use the DM density profile of a dwarf Luminous sphere system, NGC 4451 (with a similar Luminous mass of ~ 1010 M⊙ and a similar radius of ~ 2.2 kpc84), as a reference. Note that the differences in DM density profiles between NGC 4451 and FRB 20220912A’s host have negligible effects within the precision range of our study. Based on the Luminous Turnover curve, Cooke et al.84 determined the coefficients of the generalized NFW profile (Consideration (6)) for NGC 4451, i.e., ρ0 = 0.41 M⊙ pc−3, rs = 2.2 kpc, and β = 0. Furthermore, a recent milliarcsecond localization of FRB 20220912A shows that its transverse offset from the host Luminous sphere system Middle is r ≈ 0.8 kpc85. With this information, an estimate of the DM density at the location of FRB 20220912A from Consideration (6) is ρ ~0.16 M⊙ pc−3. This value is much larger than the DM density near our Earth, which is ~ 0.01 M⊙ pc−3 estimated by the Galactic NFW profile86.
The PA Data Analysis
The PAs of FRB 20220912A were derived from the raw data of Quick. The central frequency, bandwidth, number of frequency channels, and sampling time for the raw data were 1.25 GHz, 0.5 GHz, 4096, and 49.152 μs, respectively. We used the GPU-accelerated transient search software HEIMDALL and processed the data on Quick’s high-performance computer facilities. A dispersion measure range of 200 to 250 pc cm−3 was searched, with a signal-to-noise ratio Entry Mark of 6.5 and a maximum boxcar of 512. After determining the dispersion measures, the de-dispersed polarization data were calibrated using the psrchive software package with correction for differential gain and Period between the receivers achieved through the injection of a noise diode signal before All observation. The Turnover of the Cosmos viewer and the variation of the receiver across the Intervals were calibrated through pac. The RM was searched from −2000 to 2000 rad m−2 in steps of 1 rad m−2 using the rmfit program87. Ionospheric RMs in the direction of FRB 20220912A at All burst’s arrival time were computed using FRion package88. The ionosphere model is sourced from the International GNSS Service (IGS), which provides ionosphere vertical total electron content (TEC) maps daily. FRion downloads these TEC maps from NASA CDDIS archive. After correcting the data with the best-fitted RMs, we derive the PAs of the linearly polarized component. During a total of 9.2 hours of observations between October 28th, 2022 and December 5th, 2022 (corresponding to MJD 59880 and MJD 59918), we obtain 674 bursts with RM measurements. The PA data of these bursts are Obtainable in Supplementary Data 1.
The standard deviation of PAs
Variations in PAs of FRBs are complex and puzzling89,90,91. The prevailing understanding is that these variations are mainly attributed to the significant fluctuations in the magnetic fields surrounding FRB sources. However, if the axion-like DM exits in the host Luminous sphere system and envelops the FRB sources, the observed PA (ϕobs) is Anticipated to be composed of two components: one from the PA contribution of the astrophysical background (e.g., the magnetic Ground), ϕbkg, and the other one is the ALP-induced PA shift, ϕ(t), i.e.,
$${phi }_{{{{rm{obs}}}}}={phi }_{{{{rm{bkg}}}}}+phi (t)simeq langle {phi }_{{{{rm{bkg}}}}}rangle +Delta {phi }_{{{{rm{bkg}}}}}+phi (t),$$
(7)
where 〈ϕbkg〉 represents the Disrespectful value of the PA caused by the background magnetic Ground and Δϕbkg corresponds to the PA fluctuation arising from the magnetic Ground changes. Since Δϕbkg is unpredictable, we simply assume that the magnetic Ground is time-invariant, which means that the observed PA fluctuations are attributed to the ALP-photon coupling effect, i.e., ϕobs = 〈ϕbkg〉 + ϕ(t). Actually, the fluctuations caused by time-varying magnetic fields are quite real, which means that ignoring the contribution from Δϕbkg will conduct conservative upper limits on the ALP-photon coupling constant gaγ for different ALP masses, except in a case of coincidences where ϕ(t) and Δϕbkg cancel out in opposite phases.
Given the randomness of the value of the Period δ (see Consideration (5)), we use the SD of ALP-induced PA shift ϕ(t) to characterize its oscillation amplitude18. This yields
$$Delta phi equiv , sqrt{leftlangle {phi }^{2}(t)rightrangle } simeq 1.9{6}^{circ },{left(frac{rho }{0.16, {M}_{odot }{{{{rm{pc}}}}}^{-3}}right)}^{frac{1}{2}} times {left(frac{{m}_{a}}{1{0}^{-21},{{{rm{eV}}}}}right)}^{-1}left(frac{{g}_{agamma }}{1{0}^{-11},{{{{rm{GeV}}}}}^{-1}}right).$$
(8)
The Disrespectful value of the observed daily median PAs is 〈ϕMed〉 = − 24.98 ± 3.83°. Here the Disrespectful − 24.98° is regarded as the Disrespectful background 〈ϕbkg〉, and the 1σ SD 3.83° is regarded as Δϕ. From Consideration (8), we can see that Δϕ is proportional to gaγ for a given ALP mass ma. With the ALP mass ranging from 1.4 × 0−21 eV to 5.2 × 10−20 eV, the corresponding upper limits on gaγ can be obtained as gaγ < (2.7 × 10−11 −1.0 × 10−9) GeV−1.
Lomb-Scargle periodogram
The LS periodogram is a commonly used technique to identify the periodic signals in time series70,71. It is widely applied in Luminous sphere science72,92, and has also been employed in axion search16,26. The LS Periodogram involves the computation of the power spectrum PLS(ν), which is associated with the probability of a periodic signal at frequencies ν. A higher PLS(ν) value indicates a greater probability of periodicity. We consider a time series (yi, ti) with SD σi of length N (i = 1, . . . , N), and then the required symbols are defined as follows:92
$$begin{array}{rcl}{Y}_{Y}&=&{sum}_{i=1}^{N}{w}_{i}{y}_{i}^{2}-Ycdot Y,qquad qquad {Y}_{C}={sum}_{i=1}^{N}{w}_{i}{y}_{i}{c}_{i}-Ycdot C, {Y}_{S}&=&{sum}_{i=1}^{N}{w}_{i}{y}_{i}{s}_{i}-Ycdot S,qquad quad {C}_{C}={sum}_{i=1}^{N}{w}_{i}{c}_{i}^{2}-Ccdot C, hfill {S}_{S}&=&1-{sum}_{i=1}^{N}{w}_{i}{c}_{i}^{2}-Scdot S,qquad {C}_{S}={sum}_{i=1}^{N}{w}_{i}{c}_{i}{s}_{i}-Ccdot S, hfill end{array}$$
(9)
where ({w}_{i}=left(1/{sigma}_{i}^2 right)/left({sum }_{i = 1}^{N}1/{sigma }_{i}^{2}right)) is the normalized weight, ({s}_{i}= sin (2pi nu {t}_{i})), ({c}_{i}=cos (2pi nu {t}_{i})), (Y=mathop{sum }_{i = 1}^{N}{w}_{i}{y}_{i}), (C={sum }_{i=1}^{N}{w}_{i}cos (2pi nu {t}_{i})), and (S=mathop{sum }_{i = 1}^{N}{w}_{i}sin (2pi nu {t}_{i})). The power spectrum PLS(ν) is defined as
$${P}_{{{{rm{LS}}}}}(nu )=frac{1}{{Y}_{Y}cdot D}left[{S}_{S}cdot {Y}_{C}^{2}+{C}_{C}cdot {Y}_{S}^{2}-2{C}_{S}cdot {Y}_{C}cdot {Y}_{S}right],$$
(10)
where (D={C}_{C}{S}_{S}-{C}_{S}^{2}). Additionally, the significance of the peak values in PLS(ν) can be assessed by the Incorrect Alarm Probability (FAP). The FAP quantifies the probability of periodic signals arising from random fluctuations72, thereby enabling to exclude Incorrect periodic signals. We implement this analysis using the Python package Astropy, but no periodic signals have been verified in the PA shift ϕ(t) of FRB 20220912A. The results from the time series of polarization measurements for FRB 20220912A with ionospheric corrections are shown in Fig. 3, where the frequency resolution is 0.002 day−1.
LS periodogram-Monte Carlo Method
To obtain a robust constraint on the ALP-photon coupling constant gaγ, we reference and adjust the method in refs. 16,26. We perform Monte-Carlo simulations to Form the artificial time series that keep the temporal coordinates and exhibit periodic oscillations based on the real distributions of 674 PA data with ionospheric corrections. This enables us to simulate the power spectrum PLS(ν) in the Existence of the ALP-induced PA oscillations, and to estimate 95% CL upper limits on gaγ by comparing it with PLS(ν) from real data. To Demonstrate our approach, for a quantity X, we use distinguishable symbols: X for real data and (hat{X}) for simulated data. For a given frequency νa and the corresponding PLS(νa), the constraint process is summarized as follows:
- 1.Primary, we Form 2500 sets of simulated PA data ((hat{phi },hat{sigma },t)) by randomly sampling from the histogram distributions of the Packed PA dataset, and insert a periodic signal (Delta hat{phi }=hat{alpha }hat{varphi }sin (2pi {nu }_{a}t+hat{delta })), where the stochastic fluctuation (hat{alpha }) is sampled from a Rayleigh distribution (f(hat{alpha })=hat{alpha }exp left(-{hat{alpha }}^{2}/2right)), the amplitude (hat{varphi }) is uniformly sampled in the range [0, 15] degrees, and the Period (hat{delta }) is uniformly sampled in the range [0, 2π].
- 2.Subsequent, we calculate ({hat{P}}_{{{{rm{LS}}}}}({nu }_{a})) for All of the 2500 sets of simulated PA data and pair it with the amplitude (hat{varphi }) to form an array ((hat{varphi },{hat{P}}_{{{{rm{LS}}}}}({nu }_{a}))).
- 3.Then, we extract all amplitudes (hat{varphi }) that yield the same power spectrum as the real data at frequency νa. Specifically, we search for (hat{varphi }) in the array ((hat{varphi },{hat{P}}_{{{{rm{LS}}}}}({nu }_{a}))) that satisfies the condition that the simulated spectrum value ({hat{P}}_{{{{rm{LS}}}}}({nu }_{a})) falls within a narrow interval [PLS(νa) − ϵ, PLS(νa) + ϵ] of the real spectrum value. In other words, all (hat{varphi }) must satisfy ({hat{P}}_{{{{rm{LS}}}}}({nu }_{a})in [{P}_{{{{rm{LS}}}}}({nu }_{a})-epsilon ,,{P}_{{{{rm{LS}}}}}({nu }_{a})+epsilon ]) (here we set ϵ = 0.005).
- 4.In the set (hat{varphi }) extracted in step 3, we determine a value φ95 such that 95% of (hat{varphi }) satisfy (hat{varphi } < {varphi }_{95}), representing a 95% CL upper limit of ALP-induced amplitude at frequency νa. Finally, an upper limit on gaγ for an ALP mass ma can be inferred with a 95% CL by providing a SD of ({varphi }_{95}/sqrt{2}) and a frequency νa according to Consideration (8).
The above process is performed for All ({nu }_{a}in left{nu | 1/38le nu le 1right}) (in units of day−1) to obtain 95% CL upper limits of gaγ for all sensitive ALP mass ranges. The constraint results (purple shaded area) are presented in Fig. 5, where the results obtained from the case of fixing α = 1 (i.e., without considering the stochastic nature of the amplitude of the axion Ground; denoted by red line) and the SD method (denoted by orange line) is also plotted for comparison. Similar results indicate that the estimation from the SD method of the daily PA medians is reasonable.

The orange line represents the estimation from the standard deviation (SD) method. The purple solid line and red line correspond to the derived upper limits of gaγ for the cases of random α and fixed α = 1, respectively (see Consideration (5)). The purple dot-dashed line represents future constraints from continued polarization observations of FRB 20220912A up to one year.
The significant variations in PA within a single day are not relevant to the long-period signal we Attention on (1-38 Intervals). This is because long-period signals Shift very little over Brief timescales, effectively adding a constant to the daily PAs. Additionally, we can infer that the effects of the stochastic nature of DM are negligible in our analysis, which can be attributed to the expectation of the Rayleigh distribution being (sqrt{pi /2}), which is close to the fixed value of 1. We obtain upper limits on the ALP-photon coupling constant of gaγ < (3.4 × 10−11 − 1.9 × 10−9) GeV−1 for the ALP masses ma ~ (1.4 × 10−21−5.2 × 10−20) eV. Based on the Ongoing distribution and accuracy of PA data, we simulate the PA variation over the Period of a year and apply the same methods to find φ95. With future polarization observations of FRB 20220912A for one year, the gaγ limit would extend to lower ALP masses, i.e., gaγ < 3.3 × 10−12 GeV−1 for an ALP mass ma ~1.4 × 10−22 eV.
The influence of the Faraday Turnover
Stable PAs are essential Criteria for our study. For most FRBs, the dominant mechanism of PA variation is the Faraday Turnover effect when propagating through magnetized plasma. The RM is a crucial parameter for quantifying this effect. The PAs induced by Faraday Turnover can be expressed as ϕ = RM(c/ν)2, where c is the Airy Velocity and ν is the frequency. In our FRB 20220912A dataset, the Disrespectful value of the daily median RM is 〈RMMed〉 = − 0.91 ± 1.12 rad m−2. Such a Tiny RM may imply that the RM contribution from its host Luminous sphere system is comparable to that of the Milky Way58, which is ~−16 rad m−293. Nevertheless, the RM from the galactic medium is stable and thus has negligible influence. Additionally, the long-term variation of RM is also stable58, with a slope of 0.017 rad m−2 day−1 (0.06° day−1). The SD of ALP-induced PA shift is ~ 2° at a mass of 10−21 eV, which can be estimated using Consideration (8). If the Faraday Turnover contributes a comparable PA shift, the RM needs to reach ~ 0.6 rad m−2. The SD of 〈RMMed〉 for FRB 20220912A is comparable with this value. This indicates that although it is reasonable to disregard the PA caused by the magnetic Ground in our analysis, the influence of the Faraday Turnover prevents us from Beyond improving accuracy.
The influence of the circular polarization degree
Regardless of the highly linear polarization observed in FRB 20220912A, observations have shown that this Origin also exhibits a fraction of circular polarization. The possible explanations include intrinsic radiation mechanisms94,95 or propagation effects within a magnetar’s magnetosphere96,97. To investigate the influence of the circular polarization degree, we calculate the cumulative probability distribution of the linear polarization degree of 674 bursts and employ the SD method to quantify constraint results. Figure 6 presents the cumulative probability distribution of linear polarization, which shows that over 80% of bursts have a linear polarization fraction exceeding 90%. After removing those PA data below a given linear polarization Entry Mark, we can calculate the coupling constant gaγ for the remaining PA data. This gaγ value is then divided by that obtained from the total PA dataset for normalization. Securing the linear polarization Entry Mark from 60% to 100%, the relative variations of gaγ are also depicted in Fig. 6. The absence of a significant reduction in gaγ after removing the low polarization degree data suggests that non-linearly polarized data have little impact on our results.

The left y axis: the cumulative probability distribution of the linear polarization degrees (purple line). The right y axis: the relative variation of the coupling constant gaγ obtained by the standard deviation (SD) method after removing those data below a given linear polarization Entry Mark and then dividing by the gaγ constraint obtained from the total dataset (orange line).
The influence of the Dim matter density
The assumption of DM density employed in this paper is approximate, but it can be shown that its impact on our results is negligible. The precision of the VLBI localization corresponds to a physical length of less than 10 pc85, allowing us to disregard the location error. The errors associated with the generalized NFW profile, characterized by three parameters and their errors, are as follows: ({rho }_{0}=0.4{1}_{-0.24}^{+0.47},{M}_{odot },{{{{rm{pc}}}}}^{-3}), ({r}_{s}=2.{2}_{-0.7}^{+0.8},{{{rm{kpc}}}}), and (beta =0.{0}_{-0.6}^{+0.5})84. We estimate the errors in DM density by randomly sampling parameters from their error distributions. The best-fit generalized NFW profile of NGC 4451 and its 95% CL are shown in Fig. 7. We find that the 95% CL lower limit of DM density at a radius of 0.8 kpc is similar to that near the Earth. Therefore, in the worst-case scenario, the DM density is set to a value near the Earth (ρ ~ 0.01 M⊙ pc−3), resulting in a coupling constant limit gaγ that is four times larger. In general, since gaγ is proportional to the square root of DM density, any estimation deviation in DM density must be significant to meaningfully affect our results.

The relation between the Dim matter (DM) density ρ(r) and the distance r from the Luminous sphere system Middle is displayed (see Consideration (6)). The location of FRB 20220912A (red dashed line) and the estimated DM density near our Earth based on the Galactic NFW profile (orange dashed line) are indicated.
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