A Magnetar-asteroid Impact Model for FRB 200428 Associated with an X-Ray Burst from SGR 1935+2154

Published 2020 July 14 © 2020. The American Astronomical Society. All rights reserved.
, , Citation Z. G. Dai 2020 ApJL 897 L40 DOI 10.3847/2041-8213/aba11b

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2041-8205/897/2/L40

Abstract

Very recently, an extremely bright fast radio burst (FRB) 200428 with two submillisecond pulses was discovered coming from the direction of the Galactic magnetar SGR 1935+2154, and an X-ray burst (XRB) counterpart was detected simultaneously. These observations favor magnetar-based interior-driven models. In this Letter, we propose a different model for FRB 200428 associated with an XRB from SGR 1935+2154 in which a magnetar with high proper velocity encounters an asteroid of mass ∼1020 g. This infalling asteroid in the stellar gravitational field is first possibly disrupted tidally into a great number of fragments at a radius of ∼a few times 1010 cm, and then slowed around the Alfvén radius by an ultra-strong magnetic field, and in the meantime two major fragments of mass ∼1017 g that cross magnetic field lines produce two pulses of FRB 200428. The whole asteroid is eventually accreted onto the poles along magnetic field lines, impacting the stellar surface, creating a photon-e± pair fireball trapped initially in the stellar magnetosphere, and further leading to an XRB. We show that this gravitationally powered model can interpret all of the observed features self-consistently.

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1. Introduction

Fast radio bursts (FRBs) are mysterious millisecond-duration transients of gigahertz radio emission (Lorimer et al. 2007; Thornton et al. 2013) because their physical origin and mechanism remain unknown (for observational and theoretical reviews, see Katz 2018; Cordes & Chatterjee 2019; Petroff et al. 2019; Platts et al. 2019). This year, the first light of understanding FRBs seems to have arisen due to two discoveries. First, a ∼16 day period repeating source FRB 180916.J0158+65 was discovered (CHIME/FRB Collaboration et al. 2020a). Activity lasting a longer period of ∼160 days for the first repeating FRB 121102 was then reported (Rajwade et al. 2020). These observations suggest that FRBs could arise from periodic objects such as precessing magnetars (Levin et al. 2020; Yang & Zou 2020; Zanazzi & Lai 2020) or magnetized neutron stars in binaries (Dai & Zhong 2020; Ioka & Zhang 2020; Lyutikov et al. 2020). For the former models, however, starquake-like events occurring at a stellar fixed region are required to produce an FRB 180916.J0158+65-like periodic phenomenon.

Second, an extremely bright FRB 200428 with two pulses of intrinsic durations ∼0.60 ms and ∼0.34 ms from the direction of the Galactic magnetar SGR 1935+2154 was reported (Bochenek et al. 2020; CHIME/FRB Collaboration et al. 2020b). The two pulses are separated by ∼28.9 ms. This burst was detected to have an average fluence of ∼700 kJy ms and 1.5 ± 0.3 MJy ms by the CHIME and STARE2 telescopes, respectively, which imply the isotropic-equivalent energy release of ${E}_{\mathrm{CHIME}}={3}_{-1.6}^{+3.0}\,\times {10}^{34}$ erg and ESTARE2 = (2.2 ± 0.4) × 1035 erg in two different frequency bands for the source's distance D ∼ 10 kpc. Very fortunately, an X-ray burst (XRB) with two corresponding pulses associated with FRB 200428 was simultaneously detected by high-energy satellites such as Insight-HXMT (Li et al. 2020), AGILE (Tavani et al. 2020), INTEGRAL (Mereghetti et al. 2020), and Konus–Wind (Ridnaia et al. 2020). The isotropic-equivalent emission energy release of the XRB in the soft X-ray to soft gamma-ray energy band is EX ∼ (0.8–1.2) × 1040(D/10 kpc)2 erg (Li et al. 2020; Mereghetti et al. 2020; Ridnaia et al. 2020; Tavani et al. 2020). The spectrum seems to be fitted by either a cutoff power-law model (Li et al. 2020; Mereghetti et al. 2020; Ridnaia et al. 2020; Tavani et al. 2020) or a double-temperature blackbody model (kT1 ∼ 11 keV and kT2 ∼ 30 keV, Mereghetti et al. 2020; Ridnaia et al. 2020).

The physical parameters of the magnetar SGR 1935+2154 include the rotation period P ≃ 3.24 s, spin-down rate $\dot{P}\,\simeq 1.43\times {10}^{-11}\,{\rm{s}}\,{{\rm{s}}}^{-1}$, surface dipole magnetic field strength Bs ≃ 2.2 × 1014 G, and spin-down age t ∼ 3.6 kyr (Israel et al. 2016). The source is hosted in the Galactic supernova remnant (SNR) G57.2+0.8 (Gaensler 2014). However, some estimates of the distance D and age of the SNR remain highly debated, e.g., D is in a range of ∼6.6 to ∼12.5 kpc (Pavlović et al. 2013; Surnis et al. 2016; Kothes et al. 2018; Zhong et al. 2020; Zhou et al. 2020). Inferred recently from the observed dispersion measure and Faraday rotation measure, D turns out to be 9.0 ± 2.5 kpc (Zhong et al. 2020). Although this range implies that the isotropic-equivalent energy release of FRB 200428 is close to the low energy end of cosmological FRBs (Bochenek et al. 2020; CHIME/FRB Collaboration et al. 2020b), the association of the FRB with SGR 1935+2154 clearly indicates a magnetar origin at least for some FRBs. Based on the frame of a magnetar, some models for the association of an FRB/XRB were discussed (Lu et al. 2020; Lyutikov & Popov 2020; Margalit et al. 2020) in which both FRBs and XRBs are triggered by starquake-like explosions and powered magnetically. We call these models interior-driven ones.

In this Letter, we propose a different model for the association of FRB 200428 with an XRB from SGR 1935+2154, in which a magnetar encounters an asteroid. We show that such an impact can interpret all of the observed features self-consistently. The impact and radiation physics were discussed in detail when a moderately magnetized pulsar encounters an asteroid (Dai et al. 2016), in which case an asteroid can freely fall onto the stellar surface and lead to a bright cosmological FRB. For a magnetar, however, an asteroid during its free infall must be impeded around the Alfvén radius by an ultra-strong magnetic field and then accreted onto the poles along magnetic field lines, colliding with the stellar surface instantaneously and generating an XRB (see Figure 1). Although it is undetected at cosmological distances, such an XRB in the Galaxy is bright enough to be observed by X-ray satellites (for a discussion, see Dai et al. 2016). It should be pointed out that this gravitationally powered model does not exclude magnetar-based interior-driven models (for a brief summary of four kinds of energy sources, see Dai et al. 2017), some of which, together with our mechanism, might be able to take place for an FRB/XRB. This Letter is organized as follows. We describe our model in Section 2 and constrain the model parameters in Section 3. We present our conclusions in Section 4.

Figure 1.

Figure 1. Schematic picture of magnetar-asteroid impact. A rocky asteroid of mass ma ∼ 1020 g is disrupted tidally into a great number of fragments at Rd ∼ a few × 1010 cm, of which two major fragments of mass m ∼ 1017 g are then distorted tidally at breakup radius Rb ∼ 109 cm. A broken-up, elongated fragment (blue shaded region) freely falls in the gravitational field of a magnetar (gray shaded region) below Rb and meanwhile crosses magnetic field lines downwards to the magnetic interaction radius Rm, and then is accreted onto the poles along magnetic field lines. Panel (a): an electric field (E2) induced outside of the fragment by this crossing has such a large component parallel to the magnetic field around Rm that electrons are torn off the asteroidal surface and accelerated to ultra-relativistic energies instantaneously. The electrons subsequently move along magnetic field lines and their coherent curvature radiation causes an FRB. Panel (b): the asteroid eventually collides with the stellar surface, creating a hot spot (orange shaded region) and an e±-pair fireball (pink shaded region). The fireball is initially trapped by closed magnetic field lines and subsequently expands relativistically. Its energy may be released via the following processes: X-rays are emitted from a photosphere and superposition of thermal emission from different photospheres (corresponding to different fragments impacting the stellar surface) and nonthermal emission from collisions between some shells in the relativistic fireball could generate an XRB (blue wave arrows).

Standard image High-resolution image

2. The Model

The Hubble Space Telescope observations of the magnetar SGR 1935+2154 with an ultra-strong magnetic dipole field show that this magnetar is moving at a high proper velocity Vp = (600 ± 400)(D/10 kpc)km s−1 (Levan et al. 2018). This leads to our assumption that the magnetar could catch up with decelerated supernova ejecta and encounter a rocky asteroid of mass ma ∼ 1020 g. Such an asteroid, which is further assumed to include an iron–nickel component of mass m ∼ 1017 g, could be one of the asteroids hosted by the magnetar's progenitor before supernova explosion (corresponding to the first scenario of Tremaine & Zytkow 1986) or could be formed during the collapse of a part of supernova ejecta in SNR G57.2+0.8 or could happen to wander nearby the magnetar from the outside. The rate of asteroid-neutron star collisions in the Milky Way has been estimated in different scenarios (Tremaine & Zytkow 1986; Wasserman & Salpeter 1994; Siraj & Loeb 2019). In particular, the rate of such events may be as high as ∼0.1–1 per day under reasonable conditions (Wasserman & Salpeter 1994) and could even reach ∼10 per day at flux ∼1 Jy in the radio band (Siraj & Loeb 2019).

The stellar mass, radius, and surface dipole field strength are taken to be M, R*, and Bs, respectively. The asteroid is first disrupted tidally into a great number of fragments in the stellar gravitational field at radius Rd ∼ (M/ma)1/3ra ∼ 6.1 × 1010(M/1.4M)1/3 cm, where ra ∼ 2.0 × 106(ma/1020 g)1/3 cm is the rocky asteroid's original radius, and then two major fragments of mass ∼m are further distorted tidally by the magnetar at breakup radius, Rb = 1.3 × 109(m/1017 g)2/9(M/1.4M)1/3 cm, where the fragmental tensile strength and original mass density have been taken for iron–nickel matter (Colgate & Petscheck 1981). The time difference of arrival of leading and lagging parts of a fragment at any radius is estimated by

Equation (1)

where r0 is the fragmental original radius (Dai et al. 2016). This timescale is independent of freefall radius (R) and thus can be considered as the duration of an FRB (Geng & Huang 2015). A requirement of the first-pulse intrinsic duration Δt ∼ 0.6 ms of FRB 200428 (Bochenek et al. 2020; CHIME/FRB Collaboration et al. 2020b) leads to the fragmental mass

Equation (2)

In the following, we discuss the geometry of an FRB-emitting region and observed features of an FRB/XRB.

2.1. Geometry of an FRB-emitting Region

Dai et al. (2016) analyzed the fragmental size and mass density as functions of R during the freefall. Physically, the fragment is initially elongated as an incompressible flow from Rb and subsequently further transversely compressed to a cylinder (Colgate & Petscheck 1981). Here we present two evolutional results. First, the radius of the cylindrical fragment at R is written as

Equation (3)

Second, the freefall fragment is significantly affected by the stellar magnetic field, whose interaction radius (Rm) is approximately equal to the Alfvén radius (Ghosh & Lamb 1979). At the latter radius, the kinetic energy density of the fragment is equal to the magnetic energy density. Assuming that the magnetic dipole moment $\mu ={B}_{{\rm{s}}}{R}_{* }^{3}$ and the freefall velocity vff = (2GM/R)1/2, we thus derive

Equation (4)

where following Litwin & Rosner (2001) we have assumed that at R ∼ Rm the plasma in the fragment becomes thoroughly "threaded" by the magnetic field so that a strong electric field E2 is induced and meanwhile the fragment is significantly slowed because around this radius the external magnetic field is commonly believed to penetrate the plasma (Lamb et al. 1973; Burnard et al. 1983; Hameury et al. 1986). Inserting Equations (2) and (4) into Equation (3), we further obtain the cylindrical radius at Rm,

Equation (5)

This radius together with Rm determines an FRB-emitting region (i.e., yellow shaded region in Figure 2), whose relevant disk looks like an openmouthed clam and its inclination angle from the symmetric plane is

Equation (6)

It will be seen in Section 3 that this angle is much smaller than the inverse of the typical bulk Lorentz factor of FRB-emitting electrons (i.e., γ ∼ 120).

Figure 2.

Figure 2. Schematic picture of the geometry of an FRB-emitting region for relativistic electrons (with bulk Lorentz factor γ) moving from right to left along magnetic field lines of a magnetar (gray shaded region). The emitting disk looks like an openmouthed clam, on which mouth (yellow shaded region) relativistic electrons radiate an FRB (red wave arrows). The inclination angle from the symmetric plane of the emitting disk is approximated by θi ≃ r(Rm)/Rm ≪ 1/γ for FRB 200428 and thus the FRB's solid angle is given by ${\rm{\Delta }}{\rm{\Omega }}\simeq 2\pi \times \max ({\theta }_{{\rm{i}}}$, $1/\gamma )=2\pi /\gamma $.

Standard image High-resolution image

2.2. Features of an FRB/XRB

2.2.1. An FRB

When the fragment crosses the stellar magnetic field lines over Rm, as shown in Dai et al. (2016), an electric field (E2 = −vff × B/c) is not only induced outside of the fragment but it also has such a strong component parallel to the stellar magnetic field that electrons are torn off the fragmental surface and accelerated to ultra-relativistic energies instantaneously. Subsequent movement of these electrons along magnetic field lines leads to coherent curvature radiation. This emission component can account for the following features of an FRB.

First, as they move along a magnetic field line with curvature radius ρc at radius Rm, ultra-relativistic electrons produce curvature radiation and their typical Lorentz factor γ at Rm can be calculated by

Equation (7)

where σT is the Thomson scattering cross section, the parameter χ is introduced by Dai & Zhong (2020), and the maximum Lorentz factor γmax is given by Equation (12) of Dai et al. (2016). Therefore, the characteristic frequency of curvature radiation observed at an angle (θv) from the symmetric plane of the openmouthed-clam-shaped disk becomes

Equation (8)

where $\delta =1/\{2{\gamma }^{2}[1-\beta \cos ({\theta }_{{\rm{v}}}-{\theta }_{{\rm{i}}})]\}$ is the factor related with the Doppler effect: δ = 1 for θv ≤ θi, δ ≃ 1/[γ(θv − θi)]2 for 1/γ ≪ θv − θi ≪ 1, and otherwise δ ≃ 1/(2γ2) (see Lin et al. 2020). It is noted that the second equality of Equation (8) has used ρc = 0.635Rm near the equator from Appendix G of Yang & Zhang (2018).

Second, by considering the region of coherent curvature radiation (as shown in Figure 2), the total luminosity (Ltot) of a beamed FRB has been given by Equation (15) of Dai et al. (2016),

Equation (9)

where the factor 1/χ3 is added as χ is introduced in Equation (7). The isotropic-equivalent emission energy of the FRB observed at angle θv is thus estimated by

Equation (10)

where f ≡ ΔΩ/(4π) ≃ 1/(2γ) is the beaming factor because the FRB's solid angle ${\rm{\Delta }}{\rm{\Omega }}\simeq 2\pi \times \max ({\theta }_{{\rm{i}}},1/\gamma )=2\pi /\gamma $ (see Figure 2). Inserting Equations (2), (4), (7), and (9) into Equation (10), therefore, we obtain

Equation (11)

2.2.2. An XRB

If an infalling asteroid was diamagnetic, it would become an accretion sheet near a magnetar under the compression of an ultra-strong magnetic field (Colgate & Petscheck 1981). In this case, a fan-shaped hot plasma would be ejected during the collision of the asteroid with stellar surface, even though the collision physics is a little complicated. However, following Litwin & Rosner (2001), as widely argued in the literature (e.g., Lamb et al. 1973; Burnard et al. 1983; Hameury et al. 1986), a broken-up asteroid is thoroughly threaded by an ultra-strong magnetic field so that it is significantly slowed around Rm and then moves along magnetic field lines from Rm onto the poles, possibly giving rise to two accretion columns (Meszaros 1992). The total asteroid-magnetar gravitational energy is given by

Equation (12)

This energy is released in a timescale (Dai et al. 2016)

Equation (13)

When the asteroid collides with the stellar surface, a conical hot plasma (or more likely a hemispherical fireball, as shown by the pink shaded region in Figure 1) is ejected, which is different from the fan-shaped outflow discussed by Colgate & Petscheck (1981). This hot fireball is initially trapped by closed magnetic field lines and thus its temperature is estimated by (Thompson & Duncan 1995)

Equation (14)

where a is the radiation energy density constant and B is the magnetic field strength. Owing to the fact that kTfb is greater than the electron rest energy, a huge optical depth to photon–photon annihilation reaction in the fireball, ${\tau }_{\gamma \gamma }\sim {\sigma }_{T}{E}_{{\rm{G}}}/[(2\pi {r}_{{\rm{i}}}^{2})(2.7{{kT}}_{\mathrm{fb}})]$$3\times {10}^{10}{({E}_{{\rm{G}}}/{10}^{40}\mathrm{erg})({r}_{{\rm{i}}}/{10}^{5}\mathrm{cm})}^{-2}{({T}_{\mathrm{fb}}/{10}^{10}{\rm{K}})}^{-1}$ (where ri is the fireball's initial radius and 2.7kTfb is the mean thermal photon energy), inevitably leads to a dense population of e± pairs, further making the fireball become highly collisional and opaque. This thus drives a relativistic outflow that traps radiation near the star and releases energy at radius much larger than R* (Thompson & Duncan 1995; Kaspi & Beloborodov 2017). This process resembles what happens in cosmological gamma-ray bursts (Kumar & Zhang 2015). On the one hand, thermal X-rays are emitted from a photosphere of the outflow, and the superposition of thermal emission from different photospheres (corresponding to different fragments colliding with the stellar surface) possibly generates a multitemperature spectrum of an XRB, whose duration is of order ∼ta estimated by Equation (13). On the other hand, collisions between different shells in the relativistic outflow could produce an additional nonthermal emission.

3. Constraints on Model Parameters

FRB 200428 has two pulses separated by ∼28.9 ms. Their intrinsic durations are ∼0.6 ms and ∼0.34 ms, respectively, and their fluence ratio is ξ ∼ 480/220 = 2.2 (CHIME/FRB Collaboration et al. 2020b). The isotropic-equivalent energy release of the first pulse as an example is thus Eradio ≃ [ξ/(1 + ξ)] × (ECHIME + ESTARE2) ∼ 1.7 × 1035t/0.6 ms)erg for D ∼ 10 kpc (for D also see Zhong et al. 2020), where ECHIME and ESTARE2 are the isotropic-equivalent radio emission energies observed by the CHIME and STARE2 telescopes (Bochenek et al. 2020; CHIME/FRB Collaboration et al. 2020b), respectively. Therefore, we can constrain the model parameters.

First, from Equation (2), we find the fragmental mass

Equation (15)

If Bs = 2.2 × 1014 G, M = 1.4M, and R* = 106 cm are adopted, we obtain the magnetic interaction radius

Equation (16)

the cylindrical radius

Equation (17)

and the inclination angle of an FRB-emitting region

Equation (18)

Equations (16)–(18) give the parameters of the geometry of FRB 200428's emitting region in our model.

Second, as for the radio properties, FRB 200428 was detected by the STARE2 telescope (Bochenek et al. 2020), implying that νcurv ∼ 1.4 GHz, that is,

Equation (19)

and

Equation (20)

The isotropic-equivalent energy release becomes

Equation (21)

A requirement of Eradio ∼ 1.7 × 1035t/0.6 ms)erg leads to

Equation (22)

The solution of Equations (20) and (22) is

Equation (23)

and

Equation (24)

It can be seen that χ ≲ 1 and δ ∼ 1, showing that our model is self-consistent. This also implies that our line of sight is just within the solid angle of FRB 200428. In addition, combining Equations (19) and (23), we find the electrons' typical Lorentz factor γ ∼ 120 for Δt ∼ 0.6 ms.

Third, as for the XRB properties, Equation (12) shows

Equation (25)

where ζ is the X-ray radiation efficiency and its upper limit is ∼1/2 because at least half of the gravitational energy release EG is transferred inward to the thermal energy of the stellar matter and eventually emitted by neutrinos. Equation (25) is consistent with the total energy of the observed XRB from SGR 1935+2154 as long as ζ(ma/1020 g) ∼ 0.5, indicating that our model can also well explain the XRB. For a more massive asteroid (i.e., ma > 0.5 × 1020ζ−1 g), this conclusion is more viable. On the other hand, as the asteroid collides with the stellar surface, a resultant hot fireball has such a high temperature Tfb estimated by Equation (14) that a dense population of e±-pairs are inevitably created. Thermal X-rays from a photosphere in the relativistically expanding fireball are emitted, and the superposition of radiation from different photospheres could generate a multitemperature spectrum of an XRB. In addition, collisions between different shells in the fireball may lead to nonthermal emission. It would be expected that these processes can explain the observed spectrum of the XRB (Li et al. 2020; Mereghetti et al. 2020; Ridnaia et al. 2020; Tavani et al. 2020), as discussed in Section 2. A full discussion of the spectrum is well beyond the scope of this Letter and will be left for future work.

Fourth, the above constraints are given for the first pulse of FRB 200428. For the second pulse of this burst, Δt ∼ 0.34 ms and Eradio ≃ [1/(1 + ξ)] × (ECHIME + ESTARE2) ∼ 0.8 × 1035t/0.34 ms)erg for the distance D ∼ 10 kpc. These observed data have been used to provide similar constraints on model parameters.

Fifth, the observed light curve of FRB 200428 requires that the time interval (∼28.9 ms) between two submillisecond pulses should be smaller than the total asteroidal accretion timescale ta (i.e., Equation (13)), implying that ma > 3 × 1018 g. This constraint is naturally satisfied for the mass limit from XRB observations.

Finally, during an active period of 29 XRBs from SGR 1935+2154 observed by Fermi/GBM prior to FRB 200428, the FAST radio telescope observed the magnetar but did not detect any FRB (Lin et al. 2020). This nondetection result can be understood in our model: δ ≃ 1/(2γ2) ∼ 3.5 × 10−5 for θv ≫ θi, in which case the isotropic-equivalent radio emission energy observed at θv is ∼0.7 × 1022 erg even if a fragment has a similar mass. This energy is too low for the FAST telescope to be able to detect any FRB. Furthermore, for a less massive fragment, any FRB-like signal from SGR 1935+2154 at large θv cannot be observed because of a lower intrinsical isotropic-equivalent energy release Eradio.

4. Conclusions

In this Letter, we have proposed a new model for the association of FRB 200428 with an XRB from SGR 1935+2154, in which a magnetar encounters an asteroid with mass of ∼1020 g. We have shown that such an impact can self-consistently interpret the emission properties of FRB 200428 and its associated XRB. This model is different from that of Dai et al. (2016), because we here considered the magnetic interaction radius Rm, around which the asteroid during its free infall must be impeded by an ultra-strong magnetic field and then accreted onto the poles along magnetic field lines, colliding with the stellar surface and generating an XRB. Although it is undetected at cosmological distances, such an XRB in the Galaxy is bright enough to be observed by current X-ray satellites, as discussed in Dai et al. (2016). We constrained the model parameters. Our conclusions are summarized as follows.

  • 1.  
    FRB 200428-emitting region looks like an openmouthed clam, whose inclination angle and magnetic interaction radius are θi ∼ 1.7 × 10−3 and Rm ∼ 1.2 × 107 cm, respectively. The FRB emits along magnetic field lines around Rm.
  • 2.  
    The typical Lorentz factor γ ∼ 120 of emitting electrons is found to understand a low isotropic-equivalent energy of FRB 200428 as compared to cosmological FRBs. Our line of sight is just within the solid angle of this burst. If the viewing angle is much larger than θi (i.e., an off-plane case), the isotropic-equivalent energy release becomes extremely low. This is why the FAST telescope has not detected any FRB-like signal during the active phase of 29 XRBs observed by Fermi/GBM.
  • 3.  
    As the asteroid collides with the stellar surface, a resultant hot fireball has a temperature ∼1.8 × 1010 K. This leads to a dense population of e± pairs. The superposition of thermal emission from different photospheres and nonthermal emission from collisions between different shells in the fireball is expected to account for the observed XRB's spectrum.3 In addition, from Equation (13), the typical duration (ta) of an XRB is of order ∼0.1(ma/1020 g)1/3 s, which is basically consistent with the X-ray observations.

What should be pointed out is that in this Letter we have only discussed the asteroid-neutron star direct collision case in which the impact area πb2 (where b is the so-called impact parameter) is smaller than the capture cross section given by Equation (18) of Dai et al. (2016), that is, πb2 < σa = 2.4 × 1019R*,6(M/1.4M)Vp,7−2 cm2, where R*,6 = R*/106 cm and Vp,7 = Vp/107 cm s−1, implying that $b\lt {b}_{\mathrm{cr}}={({\sigma }_{{\rm{a}}}/\pi )}^{1/2}$ = $2.8\times {10}^{9}{R}_{* ,6}^{1/2}{(M/1.4{M}_{\odot })}^{1/2}{V}_{{\rm{p}},7}^{-1}\,\mathrm{cm}$. In this case, an asteroid is not only captured by a neutron star but also eventually impacts the stellar surface. If b > bcr, on the other hand, an asteroid cannot be captured and instead it flies out nearby the neutron star, in which case the asteroid still interacts with the stellar magnetosphere, perhaps leading to a faint burst-like electromagnetic signal due to the effect of a weak outer magnetic field.

I would like to thank the anonymous referee for helpful comments that have allowed me to improve the presentation of this Letter. I also thank Lin Lin, Xiangyu Wang, Xuefeng Wu, Yunwei Yu, Bing Zhang, and Shuangnan Zhang for their useful discussions. This work was supported by the National Key Research and Development Program of China (grant No. 2017YFA0402600) and the National Natural Science Foundation of China (grant No. 11833003).

Noted added in proof

Mereghetti et al. (2020) found that the brightest peak of the XRB had a delay of 6.5 ± 1 ms with respect to the 1.4 GHz radio pulse. Such a time delay is understandable based on the physical processes shown in Figure 1: a pulse of the FRB is originally produced from one of two major fragments crossing magnetic field lines around Rm and a corresponding peak of the XRB is subsequently emitted from a relativistically expanding fireball arising from collision of the same fragment with the stellar surface. This time delay together with a possible polar origin of the XRB seems to support our model.

Footnotes

  • After the submission of this Letter, Younes et al. (2020) suggested a possible polar origin of the FRB 200428-associated XRB, based on the fact that such an XRB has an extremely low occurrence rate (at most around 1 in 7000) and an unusual spectrum (e.g., the spectral cutoff energy is much higher than those of 24 XRBs emitted in 13 hours prior to the FRB). This suggestion is clearly consistent with the physical picture shown in Figure 1.

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10.3847/2041-8213/aba11b