Direct and indirect detection of dissipative dark matter
We study the constraints from direct detection and solar capture on dark matter scenarios with a subdominant dissipative component. This dissipative dark matter component in general has both a symmetric and asymmetric relic abundance. Dissipative dynamics allow this subdominant dark matter component to cool, resulting in its partial or total collapse into a smaller volume inside the halo (e.g., a dark disk) as well as a reduced thermal velocity dispersion compared to that of normal cold dark matter. We first show that these features considerably relax the limits from direct detection experiments on the couplings between standard model (SM) particles and dissipative dark matter. On the other hand, indirect detection of the annihilation of the symmetric dissipative dark matter component inside the Sun sets stringent and robust constraints on the properties of the dissipative dark matter. In particular, IceCube observations force dissipative dark matter particles with mass above 50 GeV to either have a small coupling to the SM or a low local density in the solar system, or to have a nearly asymmetric relic abundance. Possible helioseismology signals associated with purely asymmetric dissipative dark matter are discussed, with no present constraints.
a,b]JiJi Fan, a]Andrey Katz, a]and Jessie Shelton \affiliation[a]Department of Physics, Harvard University, Cambridge, MA 02138 \affiliation[b]Physics Department, Syracuse University, Syracuse, NY, 13244
The existence of dark matter (DM) is well established by gravitational observations and serves as the most tantalizing evidence for physics beyond the
Standard Model (SM). Yet very little is known about the composition
and interactions of dark matter beyond the universal gravitational
interaction. A tremendous amount of theoretical effort has been
invested in scenarios with single-component, cold, collisionless dark
matter, a picture mainly inspired by large-scale structure
observations and theoretical simplicity. However, we know very little about the dark world and, as the visible world consists of
a complicated multi-scale combination of thermal and non-thermal relics, it is important to
explore less minimal possibilities for the dark world. Such exploration
will also help us fully understand the implications of data from
current and future dark matter experiments. One such example is the
recently proposed “partially interacting dark matter” scenario
(PIDM), in which only a subdominant component of dark matter undergoes
significant self-interactions [1, 2]. In one
subclass of this scenario, “double-disk dark matter” (DDDM), this
subdominant component is charged under a long-range force which leads
to dissipative dynamics and the formation of a dark disk.
This scenario opens up interesting new possibilities for the dark world. Partially interacting dark sectors are less constrained by halo-shape observations [4, 5, 6, 7, 8], relative to the early works on self-interacting dark matter, which always assumed that all dark matter self-interacts [9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22]. However meaningful constrains on PDDM apply from dark acoustic oscillations (DAO) . On the other hand, the partially dissipative scenario makes several distinctive predictions for dark matter spatial and velocity distributions as well as composition, yielding dramatical novel predictions for both direct and indirect detection signals, as we now detail.
First, the spatial distribution of partially dissipative DM differs significantly from the usual ellipsoidal dark matter halos. While the dominant component of dark matter, e.g., axions or some neutral component of the dark sector, still acts as collisionless cold dark matter and forms halos, the subdominant self-interacting dark matter could (partially) cool via its long-range self-interaction and collapse into a smaller volume within the larger halo, analogous to the collapse of baryons into a disk through electromagnetic interactions. If the cooling is sufficiently rapid, a dark disk could be formed, as happens in the DDDM scenario. The collapsed spatial profile of partially or wholly cooled dissipative dark matter results in very different predictions for dark matter abundance, both locally in our solar system and in galaxy halos, affecting both the types and magnitudes of signals for any kind of dissipative dark matter detection. The term “dark disk” has already been employed in the literature in reference to the possibility that dark matter accretes onto the baryonic disk during mergers . However, besides the differing origin of our dark disk, dissipatively-formed dark disks have an important difference which leads to sharply different observational consequences. In the gravitationally formed “dark disk” scenario, dark matter in the disk is the same particle species as the dark matter in the halo, while in the DDDM scenario, the subdominant dark matter mostly resides in the disk and has different properties and interactions than the dark matter forming the bulk of the halo.
Second, the velocity distribution of a cooled sub-dominant component of dark matter will have a smaller thermal velocity dispersion compared to that of standard cold dark matter. Also, due to the altered spatial distribution of dissipative dark matter, its velocity distribution will in general be far from isotropic, and the relative velocity between this component of dark matter and the solar system can be very different from standard expectations. In the usual cold dark matter scenario, the average velocity of dark matter with respect to the Sun is of order the Sun’s rotational velocity. In the DDDM scenario, if the dark disk co-rotates with the baryonic disk, the relative velocity of DDDM to the Sun is instead of order the Sun’s peculiar velocity, an order of magnitude below the Sun’s rotational velocity.
Third, a dissipative dark sector necessarily contains multiple particle species. For cooling to happen, a light species with long-range interactions must exist, requiring the abundance of the light species to be set by a number asymmetry. This also implies that an additional (“heavy”) particle species with equal and opposite charge under the long-range dark force must exist with an equal number asymmetry. Generically, as we will review in Sec. 2, both an asymmetric and a symmetric relic abundance of the heavy species will co-exist.
In this paper, we will show that due to these new characteristic features of partially dissipative dark matter, dark matter direct detection constraints on cool dark matter in PIDM/DDDM scenarios will be considerably relaxed compared to those of normal cold dark matter, and in some cases can even disappear. To understand constraints coming from indirect detection, we focus on possible signals from solar capture. Since the velocity dispersion of cooled DM is smaller than that of standard cold DM, cooled DM is more easily captured in massive bodies. When there is a symmetric component of the relic abundance, dark matter annihilations inside the Sun yields signals in neutrino telescopes; when the asymmetric population dominates, dark matter instead builds up inside the Sun, yielding potential constraints from helioseismology [25, 26].
Depending on the cooling time and other parameters of the dark sector (reviewed in Section 2), the present-day spatial and velocity distributions of the dissipative DM can vary. Therefore in this study we will be agnostic both about the exact values of the velocity dispersion and the local number density of the PIDM, keeping them as free parameters of our theory, without necessarily assuming full cooling into a dark disk distribution. We will also not discuss here possible cosmic ray signals of dissipative DM outside the solar system, since these observables are very sensitive to our assumptions about the spatial distribution of the PIDM.
We also emphasize that many of our results regarding direct and indirect measurements largely apply also to cold flows of regular cold non-interacting DM. Such flows are predicted, for example, by models of late infall of non-virialized DM into the the Galactic halo. These streams will typically have much smaller velocity dispersion than the virialized DM [27, 28, 29].
The paper is organized as follows: first we review the basics of dissipative dark matter in Sec. 2. In Sec. 3, we discuss the relaxation of direct detection constraints on the couplings between dissipative dark matter and the SM particles. In Sec. 4, we study the general theory of solar capture of dissipative dark matter and highlight the differences with respect to the standard scenario. In Sec. 5, we discuss constraints from neutrino telescopes such as IceCube on dissipative dark matter annihilation inside the Sun, and comment on capture in the Earth. In Sec. 6, we discuss helioseismology constraints on purely asymmetric dissipative dark matter accumulated inside the Sun. We conclude and discuss future directions in Sec. 7. The demonstration of the validity of key assumptions in our analysis of solar capture are relegated to the appendix.
2 Review of dissipative DM
2.1 Spectrum and relic abundance of dissipative DM
The dissipative dark matter sector we consider here is broadly analogous to our baryonic sector. There are two species of particles, a light species denoted by (for “coolant”) with mass , analogous to the electron, and a heavy one denoted by with mass , analogous to the proton. Both and transform under an unbroken dark gauge group associated with a long-range dark force. The simplest possibility is that the gauge group is Abelian, a , with a coupling strength . The light “dark electron” particles annihilate away efficiently in the early Universe through [1, 2]. Thus any current population of particles must be asymmetric. Without loss of generality, we will assume that only exists now. To keep the universe neutral under the , there must be a compensating asymmetric number abundance of particles, which we take to have equal and opposite charge as .
On the other hand, the annihilation rate of is much slower than that of as the
annihilation rate decreases with increasing mass. Thus it is possible
to have a symmetric thermal relic abundance of on top of
the asymmetric relic abundance of .
Therefore the most generic scenario for dissipative dark matter
includes both a symmetric and asymmetric component. The relative
fraction of symmetric and asymmetric components in the relic density
has no impact on direct detection, in the experimentally interesting
case where the heavy species dominates the dark sector couplings
to the SM.
2.2 Dissipative dynamics
In the early Universe, the asymmetric component of the relic abundance, made of and particles, largely recombines into dark atoms once the temperature of the universe drops below the binding energy. After the dark matter particles fall into the galactic halo, however, they will be shock heated to the halo virial temperature, which is generally high enough to ionize the dark atoms and form a fully ionized dark plasma. A symmetric relic density of , adds additional dark ions to the plasma.
The existence of a long-range dark force then allows the dark plasma to cool through:
Bremsstrahlung process: . Dissipative dark matter scatters, emitting a soft dark photon which carries away energy;
Compton scattering: . Dark matter particles scatter off dark photons, depositing energy into the dark CMB.
When the dark plasma is cooled enough that dark recombination can happen again, further cooling through atomic or molecular processes will take place, which we do not consider further.
Since the rates of both bremsstrahlung and Compton scattering increase with decreasing mass, it is dominantly the light particle which can efficiently transfer energy to the dark radiation. One necessary condition for sufficient cooling to form a dark disk is that the cooling time scale is shorter than the age of the Universe. This requirement sets a constraint on the mass of the “coolant” particle, MeV. The Rutherford scattering between and particles transfers energy between and , allowing the entire plasma to cool. In the portion of parameter space in which the time scale for energy equipartition is shorter than the cooling time scale, cooling proceeds adiabatically. For very small , the Rutherford scattering rate is so slow that the plasma may cool out of equilibrium.
Similar to baryons, the dark plasma acquires angular momentum via tidal torques during structure formation. Thus when both the cooling time scale and energy equipartition time scale are shorter than the age of the Universe, the dark plasma could potentially form a rotationally supported disk. However, it is also of interest to consider a broader range of parameter space, in which either the cooling or the energy equipartition time scale is longer than the age of the Universe. Here some partial cooling will still occur and the dark plasma will collapse into a smaller volume in the halo without forming a disk. This nonequilibrium regime could be fruitfully addressed by future -body simulations.
We caution the reader that a very thin disk might be unstable in the sense that it may fragment and large gaseous clouds may form. We estimated the Jeans mass for this fragmentation in a previous paper . Once clouds above the Jeans mass begin to collapse, further cooling through atomic and molecular processes might lead to the formation of dark stars. In the absence of numerical simulations it is difficult to further quantify these effects.
2.3 Velocity distribution and density distribution
The velocity dispersion of dissipative dark matter at the present day, , is set by the temperature at which cooling stops, . As a crude estimate, we expect that cooling stops when dark recombination happens. The velocity dispersion is then estimated to be
As one can see from Eq. 1, the thermal velocity dispersion of dissipative dark matter could be much smaller than that of normal cold dark matter, which is . Strictly speaking, this estimate for the velocity dispersion should only be trusted when sufficient cooling happens. If the cooling time scale is slightly longer than the age of the universe, the temperature of the dark plasma nowadays will generally be above the binding energy. Even in the case when sufficient cooling occurs, we neglect additional heating and cooling from atomic and molecular processes, which have opposite effects on the velocity dispersion. Thus the estimate of Eq. 1 should be taken with a grain of salt. More robust estimates would require future numerical simulations. For our purpose, it suffices to take the velocity dispersion as a free parameter, varying from ,
Another important velocity relevant for both direct and indirect detection signals is the relative velocity between the flux of dark matter particles and the Sun. If dissipative dark matter particles cool into a rotationally supported disk as in the DDDM scenario, they will move around the center of the galaxy in largely coplanar circular orbits. If the dark disk is aligned and co-rotating with the baryonic disk, then in the vicinity of the Sun both dark matter particles and baryonic structures will move in the same mean circular orbit. This means that the average relative velocity of dark matter particles with respect to the Sun comes from deviations from the baryonic disk’s average rotational velocity, that is the peculiar velocity of the Sun, of order . Similarly the relative velocity between the flux of dark matter particles and the Earth is the Earth’s peculiar velocity, which is again of order . These observations also hold true for normal cold dark matter in a dark disk formed by accretion onto the baryonic disk, as first noticed in [30, 31]. However, there is one major difference between our dissipative dark disk and their accretional dark disk. In Refs. [30, 31], cold dark matter has both a halo component and a disk component while in our scenario, dissipative dark matter particles mostly reside in the disk. This will lead to a relaxation of the constraints on the couplings between dark matter particles and the SM particles from direct detections, which will be demonstrated in the following section. If the dark disk anti-rotates with the baryonic disk, or if the dissipative dark matter only cools into a non-rotational clump, the relative velocities are still of order , comparable to that of ordinary cold dark matter. Thus in what follows we focus on relative velocities in the physically interesting range .
In our analysis, we assume that the dissipative dark matter has a Maxwell-Boltzmann velocity distribution. For both direct and indirect searches which we will discuss, the signal rate is only sensitive to ) when these two velocities are of different orders of magnitude. In Table 1, we list all velocities relevant to direct and indirect detection signals in order to fix the notation we will use below.
|Sun’s rotational velocity||(0, 220, 0) km/s|
|Sun’s peculiar velocity||(10, 5.25, 7.17) km/s|
|Earth’s peculiar velocity||29.8 km/s|
|escape velocity of the galaxy||540 km/s|
|escape velocity inside the Sun as a function of radius||km/s|
|DM velocity dispersion|
|average velocity of DM in the galactic frame|
|relative velocity of dissipative DM to the Sun|
Finally we comment on the local density of dissipative dark matter near the Sun. This quantity depends crucially on the dark disk thickness and the alignment of the dark disk with respect to the baryonic disk. In general, there is only a weak constraint on the local dissipative dark matter density from the Oort limit, which allows a local density up to a few GeV/cm . The Oort limit is derived from subtracting from the measured overall surface density below a height in the Milky Way the contribution from the stellar disk, gas disk and other visible baryonic matter.
Strictly speaking, the local densities relevant to direct detection and solar capture are different. We will consider the most optimistic case for both signals, where a dark disk is precisely aligned with our baryonic disk. As the Sun could oscillate around the plane of dark disk, for direct detection experiments, the relevant local density is the current density of dissipative dark matter in the solar system. On the other hand, for indirect detection depending on solar capture, it is the local density averaged over the Sun’s age that matters. As long as the oscillation period is much shorter than the Sun’s age, the averaged local density is only sensitive to the local density in the middle of the dark plane. In our analysis, we do not differentiate between the current and the averaged local densities. But it is worthwhile to emphasize that although currently the solar system could be outside the dark disk and thus direct detection experiments could be completely insensitive to the dark disk, indirect detection could still potentially set interesting constraints.
3 Direct detection of dissipative DM
Direct detection of dissipative dark matter is highly model dependent and can be evaded easily. For instance, in the DDDM scenario, if the dark disk is not aligned with the baryonic disk, or if the dar disk is aligned with the baryonic disk but is so thin ( pc) that the Sun is outside the DDDM disk, there will be no direct detection signals at all. On the other hand, if the two disks are approximately aligned and the solar system is inside the DDDM disk, predictions for direct detection can be dramatically different from that of normal cold dark matter. In this section, we will assume the most optimistic case for direct detection, with our solar system inside the DDDM disk, and focus on the possibility of dissipative dark matter scattering elastically off target nucleons in detectors. We will show that in this case, the direct detection constraints can be considerably relaxed. The possibility of inelastic scattering of light dark matter as an explanation for the three possible signal events observed in CDMS II silicon data  was discussed in .
First we briefly review the kinematics of elastic scattering of dark matter particles in direct detection. A dark matter particle moves with a nonrelativistic velocity, , in the lab frame, then scatters off a nucleus in the detector. Depending on the scattering angle, the recoil energy imparted to the nucleus varies from zero to
where is the mass of the target atom, and is the reduced mass of the dark matter–nucleus system. Most experiments are only sensitive to energies above a threshold energy, , below which noise and different backgrounds overwhelm possible dark matter signals. The typical threshold for nuclear recoil energies in current direct detection experiments is a few keV. Having a threshold means that for a given dark matter particle mass each experiment is only sensitive to a minimum value of the dark matter relative velocity :
For elastic scattering of heavy dark matter with a given DM mass of order GeV), choosing heavier nuclei reduces the DM velocity threshold . Thus direct detection detectors with heavier nuclei will sample more of the dark matter velocity distribution and have greater sensitivity. This is shown in Fig. 1, in which we plot regions in the () plane to which each of some representative direct detection analysis [37, 35, 38, 39] is sensitive. It is clear from the figure that for a heavy dark matter particle with mass around 100 GeV, the relative velocity has to be about or above to trigger a signal in at least one of the direct detection experiments.
Now consider a dark matter flux with a velocity distribution . The rate for spin-independent elastic scattering is:
where and are the number, mass, and atomic number of the target atoms; , and are the the mass, local density, and velocity of DDDM at the Sun; is the zero-momentum spin-independent DDDM–nucleon scattering cross section; is the reduced mass of the DDDM–nucleon system; is the nuclear form factor; the minimum DDDM velocity needed to create a nuclear recoil with recoil energy and the galactic escape velocity of DDDM. We assume that the DDDM couplings to all nucleons are equal for simplicity. Before taking into account the nuclear form factor , the spectrum is flat between 0 and . However, the nuclear form factor is in general an exponentially falling function, which suppresses higher energy recoils, yielding a falling spectrum with an end point at . Thus the shape of the recoil spectrum for elastic scattering of a DDDM particle off nucleons is still similar to that of ordinary cold dark
We assume that the dissipative dark matter velocity distribution is given by a Maxwell-Boltzman distribution in the frame of the detector
with corresponding to the velocity dispersion and relative velocity with respect to the Earth respectively. The strongest current constraints of all the direct detection experiments come from LUX , and we plot them in Fig. 2. We assume the average velocity of DDDM in the galactic frame, , is the rotational velocity of the baryonic disk and thus , the peculiar velocity of the Earth. We plot the constraints on the DM-nucleon cross section, , times the ratio of the local DDDM density normalized by the normal cold dark matter density near the Sun, = 0.4 GeV/cm, for two different velocity dispersions km/s and km/s. We used Yellin’s maximal gap method  to set limits. We also plot the constraints on normal cold dark matter with standard halo model, km/s, for comparison. For velocity dispersions smaller than the peculiar velocity of the Earth, however, the constraints will not be relaxed further as the direct detection is only sensitive to .
In Fig. 2 we see that, if the dissipative dark matter velocity dispersion is as small as the relative velocity , for dark matter with mass about or below 70 GeV, a big scattering cross section scattering off nucleons, cm, which is of order of -exchange cross section, is still allowed assuming the local density of dissipative dark matter is the same as that of normal cold dark matter at the Sun, 0.4 GeV/cm. If the local density of the dissipative dark matter near the Sun is smaller than 0.4 GeV/cm, allowed values for can be even larger. Even if the local density near the Sun is one order of magnitude above 0.4 GeV/cm, for 70 GeV DDDM with velocity dispersion of , the allowed scattering cross section is cm, namely, five orders of magnitude larger than that permitted for normal cold dark matter.
In summary, due to the small velocity dispersion of DDDM, only the energy bins close to an experimental threshold are sensitive to DDDM scattering. The constraints on the cross sections for DDDM scattering off nucleons are greatly relaxed, and for velocity dispersion , a large cross section of order the -exchange cross section is still allowed for DM with mass below 70 GeV! So far, the importance of understanding and improving energy calibration around the threshold has been mostly emphasized for ruling in or out the light DM scenario. Yet from the discussions above, pushing direct direction thresholds lower could also be important for the DDDM scenario, or in general, for the detection of any dark matter component with a low mean velocity.
4 Solar capture of dissipative DM
We demonstrated in the previous section that when dissipative DM has both small velocity dispersion and small mean velocity relative to the Earth, direct detection experiments set much weaker constraints on the coupling between dissipative dark matter and the SM than is the case for normal cold dark matter. Now we turn to the indirect constraints on this dissipative dark matter scenario coming from the solar capture of dark matter. In this section, we will first derive the self-capture rate for dissipative dark matter within the Sun. Due to the long-range dark force, the scattering cross section for self-capture is velocity-dependent. This results in an enhanced self-capture rate with a very different parametric dependence from the one derived in Ref , which assumed that the differential cross section for the capturing process is velocity-independent. We then discuss two limiting cases: capture of dark matter with a symmetric relic abundance and capture of dark matter with an asymmetric relic abundance. In general, dissipative dark matter will be a mixture of both symmetric and asymmetric relic abundances and thus its capture interpolates between the two limits. We end this section by writing down the most general equations governing the capture of dissipative dark matter particles.
4.1 Self-capture of dark matter particles
We begin the discussion of solar capture by deriving the self-capture rate per target captured DM particle. We follow the standard procedure for calculating the capture rate as developed by Gould in Refs [42, 43, 44]. The main novelty in the derivation is that the differential cross section of the self-capture process is now velocity-dependent.
In Gould’s procedure, one first considers capture in an individual spherical shell of a massive body, here the Sun, of radius and local escape velocity . For the Sun, km/s and km/s. Outside the shell, consider a bounding surface of radius with such that the gravitational field due to the Sun is negligible at . The one-dimensional speed distribution function of dissipative dark matter particles at is given by , with the speed at ,
where the dimensionless variables are given by and with corresponds to the relative velocity between dark matter flux and the Sun. The infalling dark matter particles reach the shell at with a speed . Taking to be the rate at which a dark matter particle with speed at the shell scatters to a speed less than while the target particle does not gain energy above the local escape energy, the capture rate of particles per unit shell volume as an integral over the speed distribution at infinity is then given by
where is the total number of captured dissipative dark matter particles inside the Sun and is the local number density of .
The rate is given by , with the number density of dark matter targets at the location of the shell and the cross section of self-scattering processes leading to capture. Under the assumption that dark matter in the Sun can be described by a thermal distribution at the solar core temperature K, the target number density is , where is the gravitational potential as a function of position within the Sun. We will demonstrate the validity of the thermalization assumption in the Appendix. In the dissipative dark matter scenario, the dominant self-capture process, e.g., ions captured by bound (or ) ions, proceeds through Rutherford scattering with the differential cross section
Again, in adopting the formula above we assumed that the target dark matter particles are in thermal equilibrium with the solar core. The velocity of the infalling dark matter particles is much larger than the thermal velocity of the target dark matter particles and thus we can always approximate their relative velocity by . The infrared divergence is regulated by the fact that there is always a minimal scattering angle associated with the capture: an incoming dark matter particle has to lose at least a fraction of its kinetic energy to be captured. Also taking into account that the target dark matter particle cannot gain energy at or above (otherwise, there will be no net gain in the number of captured dark matter particles), for net capture to occur the cosine of the scattering angle must lie in the range
a necessary but not sufficient condition for capture to take place is . For cooled dark matter, the average velocity is much smaller than the escape velocity inside the Sun, , and this condition is almost always satisfied. The cross section for capture without ejection is then
Notice that it is enhanced by compared to the cross section for hard Rutherford scattering with order one scattering angles, .
Another subtlety associated with capture due to Rutherford scattering is that there is a finite impact parameter above which the dark charges of either the incoming dark matter particles or the dark matter targets are screened, and for impact parameters larger than this charge-screening length, the interaction is suppressed. For the capture of dark ions, this length is the Debye screening length of the dark plasma inside the Sun,
where is the captured dark matter density at the center of the Sun. Notice that is time-dependent, and decreases with time as the number of accumulated dark matter targets increases. For the capture of dark atoms, the charge-screening length is the Bohr radius of the dark atom
At scales smaller than , the dark atom capture is dominated by the capture of the nucleus inside the dark atom through Rutherford scattering. Above , the capture of dark atom has to go through short-range dipole interactions, for which the cross sections are small. The maximal impact parameter is related to the the minimal velocity through
Thus for Rutherford capture to be effective, the minimal velocities for dark ions and dark atoms have to be
Plugging in for the cross section and velocity distribution function and integrating over the velocity and volume , the self-capture rate is given by
where in the first line the upper limit of integration is the galactic escape velocity , which is always smaller than the Sun’s escape velocity . In the second and third line, we approximated by 1 and take the two limits and (i.e, ) to demonstrate the parametric dependence of the self-capture rate. We have checked numerically that the approximated formula agrees with the exact results up to the 5% level. These capture rates are very different from the self-capture rate for a velocity-independent differential cross section discussed in . In that case, the velocity dependence of self-capture is given by , which is approximately for and for .
When , or equivalently when the relative velocity is comparable to the velocity dispersion , the main contribution to the integral is from small for which the integrand is approximately proportional to . Thus the self-capture rate is logarithmically sensitive to and therefore the charge-screening length. For capture of dark ions, as the Debye length is a time-dependent quantity, the self-capture rate of dark ions for decreases logarithmically with time.
For , the relative velocity is much larger than the velocity dispersion. In this case, the contribution from small is suppressed by and the integrand is maximized when or equivalently . The self-capture rate is only sensitive to the relative velocity and is not enhanced for small velocity dispersion .
The approximated analytic formulas confirm that only matters for the self-capture rate. Given that the magnitude of the relative velocity cannot be smaller than that of the Sun’s peculiar velocity and is always in the range of , for , the velocity dispersion cannot be smaller than . For smaller velocity dispersions, , is usually satisfied. Thus for a given relative velocity, velocity dispersions smaller than that relative velocity do not enhance the self-capture rate.
An upper bound for the total dissipative dark matter self-capture rate arises when the sum of the self-interaction cross sections over all dark matter targets is equal to the surface of the volume occupied by the targets:
where is the capture cross section averaged with velocity distribution ,
where is the Dawson integral . When , and when , . The radius of the volume occupied by the targets, , can be estimated as
where the Sun’s radius is cm. One can see that as long as captured dark matter particles are thermalized with the Sun’s core, they will only occupy a small region inside the Sun.
Once the geometric limit is satisfied, the self-capture rate becomes , obtained via replacing in by . Numerically, can be approximated as
One can also estimate the total number of targets when the self-capture rate saturates the geometric bound,
where is the total number of nucleons in the Sun.
4.2 Capture of purely symmetric self-interacting DM
To make contact with the existing literature, we first consider the scenario with a negligible asymmetric relic abundance of . This scenario may not necessarily undergo (significant) cooling
Here is the rate of capture by nucleons in the Sun, is the rate for captured dark matter to annihilate inside the Sun, and is the dark matter self-capture rate computed in the the previous section. Nuclear capture rates have been calculated in [42, 43, 44] in terms of , the cross section for dark matter to scatter off a nucleus. We will consider only spin-independent scattering, in which case the nucleus-DM scattering cross section is given by :
where is the dark matter-nucleon scattering cross section, is the atomic number of the nucleus, and is the mass of the nucleus. Loss of coherence is accounted for in the full formula in [43, 44] by multiplying the cross section by an exponential nuclear form factor. For the solar capture of heavy dark matter particles with masses above 30 GeV, the most important contribution to comes from dark matter scattering off oxygen atoms with [44, 41].
The annihilation rate coefficient is
where is the relative velocity between annihilating and particles. In the dissipative dark matter scenario, dark matter particles annihilate into dark photons with a Sommerfeld-enhanced cross section
where the annihilation cross section is averaged over a Maxwell-Boltzman distribution with velocity dispersion set by as the captured dark matter particles are fully thermalized in the solar core before annihilation. We will validate this assumption in the appendix. As shown in the previous section, captured dark matter particles only occupy a small region in the core of the Sun, in which we can approximate the density as constant, g/cm . This allows us to obtain a simple analytic formula for the annihilation rate coefficient :
where the ’s are known as effective volumes. Note that only depends on the dark coupling strength in the formula above and not on . In deriving this formula, we assume that annihilations into SM particles are subdominant compared to annihilations into dark photons, or with defined as
However, for large cm, could be comparable or larger than 1. Then the total annihilation rate is with computed in Eq. (27).
Notice there is an additional factor of 2 in the last term of Eq. \eqrefeq:capture1 compared to the self-capture term in . This is because the capture rates for by and by are the same up to higher order corrections. The additional contribution to the capture of particles by targets from -channel annihilation is suppressed by GeV/ compared to that from Rutherford scattering.
When the self-interactions are turned off, Eq. \eqrefeq:capture1 has a well-known solution
defining the timescale for dark matter to reach an equilibrium abundance in the Sun. For ordinary cold dark matter, as long as the dark matter-nucleon cross-section is above cm, this timescale is much shorter than the age of the Sun, Gyr, and the dark matter density in the Sun has reached a steady state with . The total flux of SM particles, e.g., boson pairs, resulting from dark matter annihilations is then . Generically, neutrinos will be produced in the decay of the SM annihilation products, yielding a time-independent neutrino flux that can be detected by neutrino telescopes such as Super-Kamiokande  and IceCube . Thus neutrino telescopes provide an important probe of dark matter-nucleon scattering which is complementary to direct detection experiments.
When , one obtains an equilibrium abundance
Two interesting limiting cases are nuclear capture domination, , and self-capture domination, . In the case of nuclear capture domination, self-capture is largely irrelevant, and the solution reduces to that in Eq. \eqrefeq:solnonint. In the case of self-capture domination, the steady-state abundance becomes and the flux of SM particles from dark matter annihilation is given by
As we showed in the previous section, for , the self-capture rate coefficient depends logarithmically on . This explicit time-dependence slightly modifies the growth of the captured dark matter particles. Yet it does not affect the the existence of a steady-state solution, and in Eq. (30) should be understood as the self-capture rate when the steady state is reached.
One can define a parameter that indicates which capture process dominates,
where we approximated nuclear capture by the dominant oxygen capture. It is evident that self-capture can only dominate for relatively small nucleon scattering cross-sections.
4.3 Solar capture of partially asymmetric dissipative dark matter
As discussed in Sec. 2, generic dissipative dark matter sectors will have both a symmetric relic abundance composed of equal numbers of and ions and an asymmetric relic abundance in the form of dark atoms, i.e., bound states of . As the temperature inside the Sun is significantly larger than the binding energy of the dark atom, K keV , once dark atoms are captured and thermalized in the core of the Sun, they become fully ionized. Thus the relevant number abundances we wish to compute are those of the dark charged particle species, , , and . The most general -preserving equations for the solar abundance of these populations are
The rates , , and are, respectively, the nuclear capture rates for ions and dark atoms, ions, and dark atoms alone. Analogously, , , and are the self-capture rates for ions and dark atoms, ions, and dark atoms alone.
As already mentioned in Sec. 4.1, the capture of dark atoms through self-capture (as well as nuclear interactions) is short-range in
comparison to the dark Bohr radius . Thus to leading order dark atom capture occurs via the capture of the heavy particle inside the
atom, with the light following as a consequence of its dark electromagnetic interactions.
The case when the dark atom abundance is negligible in comparison to the ion abundance, , is the symmetric case discussed in the previous section. Another interesting limit takes the dissipative dark matter to be purely asymmetric, comprised only of atoms, . In this case there are no annihilations, and the solution to Eq. \eqrefeq:generalcapture1 is simply
neglecting the possible time dependence of , which only brings a minor modification to the numerical result. For , the amount of captured dark matter grows linearly, with the growth becoming exponential for . However, after the self-capture cross section reaches at a time , the number of captured dark atoms grows linearly again,
Since the number density grows linearly, one might worry that the number of dark matter particles could become comparable to the number of baryons in the Sun. This is not the case. The number of captured dark atoms as a function of time is shown in Fig. 3 for 10 (100) GeV dark matter with cm, GeV/cm, and . From this figure, one can see that the captured dark matter always constitutes only a small fraction of the total solar mass. Even for a big spin-independent DM-nucleon cross section of order of that of -exchange, cm, the total captured dark number is about or below of the total baryon number inside the Sun at the present day.
The general case where dissipative dark matter has both a symmetric and an asymmetric relic abundance interpolates between the two limits discussed above. It is straightforward to solve the capture equations numerically, and our results for neutrino signals in the following section will be presented for the general case.
5 Neutrino telescope constraints on dissipative DM in the Sun
In Sec. 3, we have demonstrated that for dissipative dark matter with mass around or below 70 GeV, a large cross section of order of that of exchange is still allowed by direct detection. Moreover, direct detection constraints could be totally absent if the solar system oscillates around the disk and is currently outside the dark disk. In this section we want to explore whether such large cross sections are also allowed by indirect detection experiments looking for products of dark matter annihilation inside the Sun. We will discuss constraints from neutrino telescopes, i.e, IceCube , which search for muon neutrinos from dark matter annihilation in the center of the Sun. The flux of SM particles from dissipative dark matter annihilation is given by
In deriving all our numerical results, we use the standard solar model with parameters in . For a specific velocity distribution of dissipative dark matter, at a given mass and DM–nucleon cross section, the constraint on the flux of SM particles from dissipative dark matter annihilation is translated into a constraint on with GeV/cm. Strictly speaking, in a specific model, is related to . For our model-independent analysis, we first treat and as free parameters and comment on their possible correlations at the end of this section.
As mentioned in the previous section, a general dissipative dark matter scenario with both symmetric and asymmetric components has a solar accumulation history interpolating between the limits with a purely symmetric or purely asymmetric relic abundance. This is demonstrated in Fig. 4. It is evident from the figure that even with a small asymmetric DM component of order , the accumulated dark matter particles never reach a steady state. keeps growing with the elapse of time but first grows and then decreases. At the beginning, the nuclear capture rate is much larger than the annihilation rate, and both and grow. Then at the time when the annihilation rate surpasses the smaller capture rate of , starts to drop but keeps growing. After that, as there are always more ’s to annihilate with captured , keeps being depleted. Yet the total capture rate of is always larger than the annihilation rate, so continues growing. The details of the growth (decrease) of vary with parameters as demonstrated in Fig. 4. For example, in the upper left panel, the growth of is linear; in the upper right panel, the growth has a kink due to the saturation of the self-capture rate at the geometric limit, and in the lower panel, the nuclear capture rate is smaller and the growth is exponentially fast at late times.
Now we use the IceCube bounds on the solar muon neutrino flux to set bounds on dissipative dark matter annihilating into two representative classes of SM final states: ( for lighter dark matter with mass below 80 GeV) and . We choose two representative velocity parameters: . For , all the capture rates only depend on and the results are unchanged. The final results are presented in Fig. 5. For , nuclear capture dominates as long as the cross section is not small and GeV. For , the constraints get stronger due to enhanced capture rates. Self-capture could become important and the geometric self-capture limit will be saturated for GeV for