ABSTRACT
Using two-dimensional and three-dimensional simulations, we study the "robustness" of the double detonation scenario for Type Ia supernovae, in which a detonation in the helium shell of a carbon–oxygen white dwarf induces a secondary detonation in the underlying core. We find that a helium detonation cannot easily descend into the core unless it commences (artificially) well above the hottest layer calculated for the helium shell in current presupernova models. Compressional waves induced by the sliding helium detonation, however, robustly generate hot spots which trigger a detonation in the core. Our simulations show that this is true even for non-axisymmetric initial conditions. If the helium is ignited at multiple points, then the internal waves can pass through one another or be reflected, but this added complexity does not defeat the generation of the hot spot. The ignition of very low-mass helium shells depends on whether a thermonuclear runaway can simultaneously commence in a sufficiently large region.
1. INTRODUCTION
In the double detonation scenario, a carbon–oxygen (CO) white dwarf (WD) accumulates a layer of helium through accretion from a helium main-sequence star. The accretion rate, typically on the order of 10−8 to 10−7 M☉ yr−1 (e.g., Taam 1980; Woosley & Weaver 1994), and the mass of the WD determine the critical thickness of the helium layer. Generally, a low accretion rate allows more helium to accumulate before a thermonuclear runaway commences near the base of the helium shell, the temperature of which is determined by gravitational compression, convection, and eventually nuclear burning. It is often assumed that a detonation in the helium induces a secondary detonation in the CO core, thus producing a Type Ia supernova.
If and how a secondary core detonation develops is ambiguous, however. One possibility is that the core is ignited directly at the core–shell interface when hit by the helium detonation front. This is sometimes called "direct drive," "edge-lit scenario," or "prompt detonation." It has long been realized that this does not always work and that its realization depends on the altitude at which the helium detonation starts (e.g., Livne & Glasner 1990; Benz 1997; García-Senz et al. 1999). A helium detonation directly at the interface almost certainly fails to start a detonation in the core, but evolution models of accreting WDs suggest that the most likely place for a detonation to start could be higher up (Woosley & Kasen 2011). One of the aims of the present work is to determine whether a helium detonation ignited at a point in the hottest helium layer would lead to core detonation by direct drive.
If direct drive fails, the core may still ignite, with considerable delay, after the detonation wave has consumed the entire helium layer through compressional waves which focus inside the core. In the simplest (and most unrealistic) scenario, the star is spherically symmetric and the helium is ignited instantaneously in a spherical shell. This induces a radially inward propagating compressional wave that converges at the exact center of the star, where, depending upon the resolution of the study, it always ignites the core (e.g., Livne 1990).
Since convective mixing is not able to keep the temperature at a given radius constant before the runaway, it is more likely that helium ignition starts in one or more isolated regions with sizes of perhaps a pressure scale height (Woosley & Kasen 2011). If the detonation starts at a single point, the sliding helium detonation creates an oblique (with respect to the core–shell interface) shock wave that converges inside the core at the axis of symmetry and potentially triggers an off-center core detonation (Dgani & Livio 1990; Livne & Glasner 1990, 1991; Livne & Arnett 1995). In their simulations of double detonation supernovae, Fink et al. (2007) considered a variety of one-dimensional (1D) and two-dimensional (2D) helium ignition scenarios, confirming the high ignition potential of the inward propagating shock wave. They showed that the core detonation resulting from the detonation of the helium in a single spot is very likely even for low-mass helium shells, for instance, 0.0035 M☉ in combination with a 1.3850 M☉ core (Fink et al. 2010), and for core masses as low as 0.45 M☉ (Sim et al. 2012).
In a scenario with less or no symmetry, for example, if helium detonations commence at multiple points, then the secondary detonation of the core is less certain. In their smoothed particle hydrodynamics simulations, García-Senz et al. (1999) first explored, using coarse resolution, the possibility of starting detonations at multiple points in the helium layer. In particular, they studied a case with asynchronous ignition at five points, finding that the core detonation could still result from the collision of the various helium detonations.
If the core does not ignite, the helium explosion alone could produce a sub-luminous, "point Ia," supernova (Bildsten et al. 2007). This raises the question as to how robust the triggering of the secondary core detonation is. If it is robust, a detonation of the helium shell alone might be very rare or even impossible in the case of CO cores (the less common oxygen–neon cores are in general much harder to ignite with converging shocks; see Shen & Bildsten 2013).
We here revisit the double detonation scenario using some of the WD models generated with KEPLER and presented in Woosley & Kasen (2011). Following a description of the numerical methods in Section 2, we first discuss the results of simulations that test the viability of direct drive in Section 3.1. In Section 3.2, we study sliding helium detonations that lead to a hot spot inside the core, with the helium detonation started at one, two, or three points. The initiation of detonations in lightweight helium shells is investigated in Section 3.2.6. In Section 3.4, we present nucleosynthesis yields from runs following the complete detonation of WDs. We conclude with a discussion and summary in Section 4.
2. NUMERICAL METHODS
2.1. Hydrodynamics
For our multi-dimensional studies, we use the Eulerian hydrodynamics code CASTRO (Almgren et al. 2010; Zhang et al. 2011) to solve the equations for compressible fluid dynamics in combination with a nuclear reaction network. We employ an equation of state based on the Helmholtz free energy (Timmes & Arnett 1999; Timmes & Swesty 2000) and a 19 isotope network to compute energy generation and nucleosynthesis (the same as in KEPLER; see Section 2.2 for details). Gravitational forces are calculated with a monopole approximation, taking into account the mass enclosed within a given distance from the center of the star at any given time. In many simulations, we make use of CASTRO's capabilities for adaptive mesh refinement (AMR). The initial models for the multi-dimensional CASTRO simulations presented here were constructed with the implicit Lagrangian hydrodynamics code KEPLER in 1D (Weaver et al. 1978; Woosley et al. 2002). The evolution of several helium-accreting WDs was followed with a model for convection based on mixing-length theory; see Woosley & Kasen (2011). The CASTRO simulations start from KEPLER snapshots taken before a thermonuclear runaway sets in. Their key properties are listed in Table 1.
Table 1. White Dwarf Models
Modela | Mcore | MHe | rcore | ΔrHeb | r(Tmax) | Tmax | ρ(r(Tmax)) | ρ(rcore) | ρ(r = 0) |
---|---|---|---|---|---|---|---|---|---|
(M☉) | (M☉) | (km) | (km) | (km) | (108 K) | (106 g cm−3) | (106 g cm−3) | (107 g cm−3) | |
A (8B) | 0.801 | 0.143 | 4081 | 2080 | 4267 | 2.06 | 1.19 | 1.66 | 2.21 |
B (10B) | 1.000 | 0.082 | 3616 | 1370 | 3765 | 2.42 | 1.30 | 1.93 | 5.67 |
C (10C) | 1.000 | 0.091 | 3518 | 1380 | 3624 | 2.31 | 1.63 | 2.18 | 6.02 |
D (10HC) | 1.002 | 0.045 | 4161 | 1260 | 4187 | 2.80 | 0.717 | 0.932 | 4.24 |
E (10HD) | 1.001 | 0.078 | 3696 | 1350 | 3724 | 2.36 | 1.50 | 1.77 | 5.33 |
Notes. aThe model identifiers in Woosley & Kasen (2011) are written in parentheses. bApproximate helium shell thickness, with the outer boundary defined to be where the density is 1/100 of the value at the core–shell interface.
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In Eulerian simulations, adding a relatively small amount of hot gas to a cold zone can raise the average temperature above the threshold for ignition, thus igniting the whole zone. Without any correction, the speed with which a "detonation front" propagates would thus be dependent on the size of the zones and driven entirely by artificial advection. To simulate detonation more realistically, we introduce a delay timer that suppresses the burning in a particular zone for half a sound crossing time. If, at any time, the necessary conditions for nuclear burning are not satisfied, the timer is set to zero. If they are satisfied, the timer starts counting and when half a sound crossing time (Courant time) has passed, nuclear burning processes are switched on in this particular zone.
In simulations of the whole star, the density of the artificial external medium is set to 1 g cm−3 and is given the same temperature as the outer edge of the helium shell. This means that as the shock of the helium detonation breaks out of the star, it is accelerated by a very steep pressure gradient. As the time step of our simulations is limited by the largest fluid velocities or sound speeds in the entire domain, the calculations become very expensive. To contain the detrimental effect on the time step, we apply a velocity cap of 1.5 × 109 cm s−1 in the ambient medium. To distinguish the ambient from stellar material at all times of the simulation, we give it a unique composition of 100% 16O.
We used no velocity cap and lower ambient densities in runs where the expansion of the ejecta was followed (Section 3.4). Whenever the ejecta reached the boundaries of the current computational domain, the solution was embedded into a new, larger domain (twice as large in each dimension, but with the same resolution at the coarsest level). The embedded solution was initially kept at a higher mesh refinement level (such that it expands into the coarser grid, rather than being mapped into it). This step was repeated several times until homologous expansion was reached. The final domain had an extent of 1.6 × 109 cm in cylindrical radius and twice that value in the z-direction. During the remaps into larger domains, the densities of the ambient media were lowered by factors of 10 from 10−2 g cm−3 (in the original domain) to 10−5 g cm−3. While ambient material piles up at the explosion front, the total mass of this material is low, on the order of 10−4 M☉, and we do not expect it to have significant influence on either the ejecta structure or the velocities.
We generally make use of symmetries to reduce the computational load. With only one detonator, the problem is axisymmetric and its solution can be computed in 2D. For a simulation with two synchronous spherical detonators, it is sufficient to perform a three-dimensional (3D) calculation of only a quarter of the star, with mirror symmetry at two boundaries (the x = 0 and y = 0 boundaries in our simulations). Two asynchronous detonators require a half-star simulation with mirror symmetry at one boundary (the x = 0 boundary in our simulations).
2.2. Nuclear Energy Generation and Nucleosynthesis
Energy generation and approximate nucleosynthesis were calculated in all cases using a 19 isotope network with constituent species as defined by Weaver et al. (1978) and nuclear reaction rates updated to current values (Woosley & Heger 2007). Screening corrections were implemented for all rates. This network includes an "alpha-chain" (Z = N = 2n, n = an integer) of nuclei from 12C through 56Ni, plus the species n, p, 3He, 14N, and 54Fe. Simulated steady state links (i.e., dYi/dt ≈ 0 within a time step) also approximate the presence of the odd Z isotopes from 23Na through 55Co (i.e., isotopes with Z = 2n + 1, N = 2n + 2). For this study, the photodisintegration of 56Ni to 54Fe + 2p was not allowed, which meant that electron capture and 54Fe were essentially omitted from the network. Furthermore, 1H, 3He, 14N, n, and p never achieved any significant abundances, so the effective network really just contained the 13 alpha-chain isotopes. Past studies (Timmes et al. 2000) have shown that such a limited network gives good agreement with the results of much larger networks, provided one is interested only in bulk nucleosynthesis and energy generation.
The network itself was employed in all carbon-rich zones always and, in most cases, for the helium shell. In some cases, however, it was computationally expedient to use a table that was prepared off-line using the network. Those cases included studies of helium shell detonation where the whole star was carried (Section 3.2), up until the generation of a hot spot in the core. The simulations for which detailed yields are given (Section 3.4) make use of the full network from the beginning to the end, as do the local simulations of direct drive (Section 3.1).
The use of a table here was novel and warrants some discussion. Unlike isobaric burning in, e.g., carbon deflagration supernovae, the table here must work reliably in dynamic situations where both the temperature and density are rapidly varying and where the outcome is sensitive to the time history of both. Using the network, a large table was generated using the results of many off-line studies of helium burning at constant temperature and density. Values of temperature in the range 108.5–109.65 K (Δlog T = 0.05) and density in the range 105–107.1 g cm−3 (Δlog ρ = 0.10) were included. Results of the burning—the composition, average binding energy per nucleon, and time derivative of the helium mass fraction—were sampled for 50 values of helium mass fraction ranging from 0.02 to 1.0 in steps of 0.02. To preserve accuracy, the rate equation for the helium mass fraction was divided by the leading order term in the 3α reaction rate, i.e.,
This resulted in a slowly varying function of T9, ρ, and Xα in the table.
When using the table in a multi-dimensional simulation, triple variable interpolation in log ρ, log T9, and XHe gave the current composition and dXHe/dt. The current time step and dXHe/dt gave a new helium abundance at the end of the step. Another call to the table using the new helium abundance gave a revised composition for the other species, and the change in composition gave a change in nuclear binding energy, hence an energy generation, and the process continued.
A shortcoming of this approach is that the entries in the table were generated at a constant temperature. This neglects additional variables because a given temperature, density, and helium abundance can be reached by a variety of histories and the instantaneous abundances of the other nuclei are sensitive to which history was followed. Some additional rules are imposed to avoid unphysical and poorly behaved solutions. The helium abundance was only allowed to decrease, i.e., dXHe/dt had to be negative, or no composition change or energy generation is allowed. Further, no modification of the composition occurred unless both the abundance of 56Ni and the nuclear binding energy increased during a time step. When these conditions were met, a change in composition was allowed, but the new composition was not just taken from the table. Instead, a fraction of the new composition at the given temperature and density was added to the old one, with that fraction determined by the change of the helium abundance during the step. Essentially, this procedure partitions the nuclear evolution for an arbitrarily varying temperature and density history into a series of small steps taken at constant temperature and density. For the conditions of the problem, the requirement that the time step be a small fraction of the Courant time proved adequate to preserve accuracy.
To demonstrate the validity of the procedure, a series of simulated explosive helium burning studies were carried out off line using both the network and the table. Starting with a composition of pure helium, matter was expanded from a peak temperature T0 and a corresponding peak density
along paths given by
with τ = 0.2 s being the timescale for the explosion. The final composition was examined when the temperature had declined below 108 K. The results are shown in Figure 1. In general, the agreement between the network results and those obtained using the table is quite good. Using the table gives a smaller final abundance for helium because burning at a constant low temperature gives a smaller mean nuclear mass and charge than explosive burning cooling from a higher temperature to the same helium mass fraction, density, and temperature. Lighter nuclei have larger cross sections for α-capture. One could improve the fit by adding a fourth independent variable, the mean nuclear charge (excluding helium itself), but the present approach was deemed adequate for this study. Some test runs at constant temperature and density using the table and the network gave a near perfect agreement, showing that the table had been correctly implemented.
Figure 1. Variation of the final composition in explosive helium burning, expanded along paths parameterized by the peak temperature T0 (see the text). The solid and dashed lines represent the results obtained with the full network and the table, respectively.
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Standard image High-resolution imageWe further tested the tables by calculating the yields of 2D helium detonations in model A, with a setup similar to run 5 presented in Section 3, but using closed boundaries at all sides to prevent hot ash from leaving the computational domain (which we chose to keep small for this test). The detonation wave converges after ≈1.20 s on the other side of the star. Compared to the calculation with the table, the detonation with the network is only slightly faster (the detonation front is ahead by about 4° as measured from the center at t = 1.15 s, with about half of the discrepancy being due to a slower start of the artificial detonator with the table). We measured the yields at t = 1.70 s, at which time the helium burning has ceased (we suppressed the burning of carbon). With the network, we thus get a 56Ni yield of 0.0721 M☉, burning 0.0934 M☉ of 4He. With the table, the numbers are 0.0687 and 0.0909. The energy produced is 2.78 × 1050 erg with the network, and 2.66 × 1050 erg with the table. This is adequate for our purposes.
3. RESULTS
3.1. Direct Drive
Here we consider the possibility of a helium detonation wave that traverses the core–shell interface beneath its origin, directly igniting the core at the outer edge. In the first two sections, we present several simulations calculated in 2D using CASTRO. Pursuing the hypothesis that direct drive is related to a critical mass, we then discuss the results of idealized 1D simulations using the KEPLER code in Section 3.1.3.
3.1.1. Altitude, Shape, and Interface Composition
Taking the (0.801 + 0.143) M☉ WD model A as an initial condition, we did a series of 2D simulations that cover a local region including the core–shell interface. The domain range in most cases is 0 < R8 < 1 and 3.3 < z8 < 5.3 in cylindrical coordinates (R, z), the core–shell interface being at the spherical radius r8 = 4.08. The grid resolution in most cases is 0.977 km (no AMR). The gravitational field is taken to be static and the boundary conditions are usually reflecting on all sides (as the detonation proceeds supersonically, the choice of boundary conditions is not critical). All simulations employed a full 19 isotope network that covers helium, carbon, and oxygen burning. The detonation spots used to start the detonation had a radius of 50 km, a temperature of 2 × 109 K at the center and 1.8 × 109 K at the outer edge (linearly decreasing), and a radial velocity of 8000 km s−1 at the outer edge (increasing linearly from zero) and twice the ambient density.
Table 2 contains a list of setups and results, and Figure 2 depicts snapshots of several cases. In the standard case (a), the helium detonator is centered at the radius at which the temperature is maximal, 186 km above the core–shell interface. While the detonation creates an indentation in the interface, and some of the carbon at the outer edge of the core burns as a result of the entering shock, the burning does not support a detonation in the core. Direct drive clearly fails in this case.
Figure 2. Density (left, upper color bar) and temperature (right, lower color bar) in local 2D simulations of helium detonations hitting upon the carbon–oxygen core. The black circles indicate the perimeters of the helium detonation spots at the beginning of each simulation. The solid and dashed gray lines represent the mass fraction contours for 49% 12C and 49% 16O, respectively.
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Standard image High-resolution imageTable 2. Direct Drive in Model A
Runa | Δx | Altitudeb | Specialtyc | Works/Fails |
---|---|---|---|---|
(km) | (km) | |||
a | 0.977 | 0 | ⋅⋅⋅ | Fails |
b | 0.977 | 200 | ⋅⋅⋅ | Fails |
c | 0.977 | 400 | ⋅⋅⋅ | Works |
d | 1.953 | 200 | ⋅⋅⋅ | Works |
e | 0.977 | 0 | 3:1 spheroidal detonator | Fails |
– | 0.977 | 0 | 4:1 spheroidal detonator | Fails |
f | 0.977 | 0 | Mixed (70% 4He) a&b | Works |
g | 0.977 | 0 | Mixed (70% 4He) | Fails |
– | 1.953 | 0 | Mixed (70% 4He) | Fails |
h | 0.977 | 0 | Mixed (50% 4He) | Fails |
– | 0.977 | 0 | Mixed (80% 4He) | Fails |
Notes. aLabels are the same as in Figure 2; "–" denotes runs mentioned in the text only. bDistance to the hottest helium layer. c"Mixed" stands for a mixed layer of helium and core material above and below ("a&b") or only below the original core–shell interface.
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With the helium detonation initiated 200 km higher, case (b), the detonation penetrates into the core. The front is unstable though, developing dents filled with compressed material that fails to ignite. The formation of these instabilities appears to be the result of complex interactions of reflecting shock waves. Figure 3 shows snapshots of the temperature in the detonation front in case (b). There are small indentations in the front, seemingly related to waves in the post-detonation region (top panel, indicated by cyan arrows). A few hundred kilometers below the core–shell interface, a big dent forms (at R ⩽ 200 km in the plots). While it is later consumed by a secondary detonation front, a new dent forms (middle and bottom panels, olive-green arrows). The vortical structures visible in the plots on a high zoom level are indicative of Richtmyer–Meshkov instabilities (RMIs; e.g., Brouillette 2002). The presence of RMIs is supported by the fact that the pressure gradient behind the detonation is normal to the front, whereas the density gradient across the interface is radial with respect to the center of the star, i.e., the pressure and density gradients are misaligned, as is typical for RMIs. It is possible, however, that RMIs here emerge as a secondary phenomenon. Global simulations, presumably in 3D, would be needed to determine whether such an unstable detonation eventually blows out or consumes the core, but they are too expensive at this resolution. Recognizing that these are marginal cases, we opted not to follow such pathological detonations in this study and dismissed them as failures.
Figure 3. Snapshots of the detonation front in case (b) of the models for direct drive discussed in Section 3.1.1. The panel in the middle is a blowup of Figure 2(b); the inset zooms in on vortical structures in the ash, with the temperatures in the plot ranging from (2.24–2.45) × 109 K (black to white). The arrows indicate indentations in the detonation front.
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Standard image High-resolution imageWith the helium detonation initiated 400 km above the temperature maximum, case (c), the detonation stably penetrates into the core. This strengthens our assumption that the instabilities described above are indicative of marginal cases. To make sure that the detonation stays stable, we followed it in a global simulation that encompasses half of the star, with the same resolution (≈1 km) as in the local simulation in a region that extends from the detonation spot to the center of the star (R8 < 1 and z8 < 5). This detonation stably proceeds all the way to the center. Oxygen burning starts 830 km below the interface (at 80% of the core radius).
In a simulation similar to case (b) with half resolution (1.95 km), case (d), the front is stable. The formation of indentations in the front is completely suppressed. We followed this detonation until a depth of 1780 km beneath the core–shell interface. Oxygen starts to burn 1130 km below the interface (at 72% of the core radius; see the lower dashed line in panel (d)), where the density exceeds 5.3 × 106 g cm−3.
The fronts of detonations started at different altitudes have different curvatures when they hit upon the core–shell interface. This raises the question as to whether the curvature of the detonation front plays a key role. Apart from altitude, the curvature is determined by the shape of the detonation spot, provided the spot is sufficiently close to the interface (for isotropic expansion velocities, any explosion eventually becomes spherical). A detonator in the form of an oblate spheroid fares better than a spherical one, compare panels (e) and (a). However, the detonation front also starts out considerably hotter than in the spherical case ( instead of 2.88 at t = 0.01 s), indicating that part of the observed difference is possibly related to the details of how the detonation was started, rather than curvature alone.1 The detonation spot in case (e) is stretched by a factor of three in the radial direction, its extent in the vertical direction being the same as that of the spherical spots. Shortly before it reaches the core–shell interface, the curvature of the underside of the oblate detonation front roughly corresponds to a sphere centered 200 km above the hottest layer, i.e., it is comparable to the detonation in case (b). A simulation with a detonator stretched by a factor of four (i.e., even more oblate) gives a very similar result (not shown in Figure 2). The curvature in this case corresponds to a sphere centered more than 400 km above the hottest layer, i.e., one would expect from case (c) that the detonation should enter the core without problems, yet it does not. We therefore surmise that curvature is not as important as altitude.
We also considered the possibility of a layer where helium mixes with core material. In case (f), we start with a mixture of 70%/20%/10% 4He/12C/16O in the region 3.98 < r8 < 4.18, i.e., 100 km above and below the original core–shell interface. The detonation stably transcends into the core in this case. We surmise that a mixed layer on both sides of the interface effectively increases the distance from the detonator to the core, thus facilitating direct drive.
In cases (g) and (h), we start with a mixture of 70%/20%/10% 4He/12C/16O and 50%/30%/20% 4He/12C/16O, respectively, in a 100 km wide region above the original interface only. Although the detonation changes when it enters the mixed region, becoming hotter and faster, it fails to penetrate the core and stay intact in both cases. Even with half resolution, the detonation in case (g) shows the same instability (unlike case (d), for which the coarser resolution helped to suppress instabilities in the detonation front). A mixture of 80%/20% 4He/12C in a 100 km wide region also leads to failure (not shown in Figure 2).
3.1.2. Heavy White Dwarfs
The above discussion shows that direct drive is not likely for model A if the helium detonation starts where the gas is hottest, i.e., the most natural location for a detonator. Models B and C both have a denser 1.0 M☉ core which in principle should detonate more easily than the 0.8 M☉ core of model A. Model C is slightly more compact than model B.
Following a similar procedure, we tested for the possibility of direct ignition with detonators at different altitudes for these models. The radius of the detonation "hot spots" was 20 km and the distance between the core–shell interface and the temperature maximum was 149 km and 106 km in models B and C, respectively. In both cases, direct ignition failed if the detonation was started at this altitude.
If we started the helium detonation 100 km above the hottest layer of model B, however, the detonation front smoothly transcended into the core. If ignited 50 km above the hot layer, the detonation fragmented and died upon passing into the core. In model C, the direct drive worked with detonators at altitudes of 100 km, 50 km, and even 25 km above the hottest layer. At 12 km, however, it failed.2 These results for direct drive with detonators at different altitudes are summarized in Table 3.
Table 3. Direct Drive: Masses of the Helium Detonation Spheres at Core Contact
Model | rdetonator | Δra | MHe-sphereb | Works/Fails |
---|---|---|---|---|
(km) | (km) | (g) | ||
A | 4270 | 189 | 3.89 × 1028 | Fails |
A | 4470 | 389 | 2.80 × 1029 | Fails |
A | 4670 | 589 | 8.28 × 1029 | Works |
B | 3765 | 149 | 2.17 × 1028 | Fails |
B | 3815 | 199 | 4.75 × 1028 | Fails |
B | 3865 | 249 | 8.71 × 1028 | Works |
C | 3624 | 106 | 9.40 × 1027 | Fails |
C | 3636 | 118 | 1.26 × 1028 | Fails |
C | 3649 | 131 | 1.68 × 1028 | Works |
C | 3674 | 156 | 2.75 × 1028 | Works |
C | 3724 | 206 | 5.91 × 1028 | Works |
Notes. aDistance from the core–shell interface to the detonator center. bDefined as twice the mass of the helium contained in the half-sphere of the radius Δr below z = rdetonator.
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3.1.3. The Critical Altitude for Direct Drive
To explore the relevant physics underlying the existence of a critical altitude for directly driving a detonation into the CO core beneath the ignition point in the helium layer, a series of idealized calculations were carried out using the KEPLER code. The hypothesis to be explored was that successful propagation requires a critical amount of momentum in the downwardly moving shock wave. That momentum should be greater than or equal to that of a "critical mass" (Niemeyer & Woosley 1997; Röpke et al. 2007; Seitenzahl et al. 2009) of carbon and oxygen at the same density as exists at the helium–carbon interface. In addition, that momentum should be focused into an area comparable to the geometrical size of the critical mass. Stated another way, the altitude of the initial helium detonation should exceed the radius of the critical mass required for initiating a successful carbon detonation evaluated at a density equal to that at the helium–carbon interface.
Of course, this is quite approximate. The density and pressure are not constant in either the helium layer or the carbon underneath, and the energy yield from helium detonation is different from that of carbon detonation. We do not know if the helium detonation ignites at a point, which implies spherical propagation, or in an extended region which might have a more planar geometry. These complexities can be partly compensated for, however. The effective radius of the helium is one that encloses a critical mass (evaluated at the density of the interface), even though the density within that sphere varies. The detonation can be studied in a two-phase medium with a helium detonator surrounded by a thick shell of carbon and oxygen. The detonation should occur in spherical geometry so long as the size of the region in the helium layer that initially runs away is small compared with its altitude above the interface. We note that if, pending further study, the latter assumption were violated, the required altitude would be reduced (compare Tables 1 and 4 in Seitenzahl et al. 2009).
In the first study, spheres of 50% carbon and 50% oxygen were prepared with a constant density of 1.93 × 106 g cm−3, as appropriate to the interface in model B. In a 1D spherical region of variable radius, the temperature was given a constant gradient (with respect to radius, not mass, even though the code is Lagrangian) with values ranging from 2.8 × 109 K at the center to 1.0 × 108 K at the edge. This 200 zone region was surrounded by 300 zones of carbon and oxygen at 108 K. All zones had the same radial thickness. The radius of the region with the temperature gradient was varied and its ability to generate a self-sustaining detonation was determined. The central value of 2.8 × 109 K was sufficiently high to guarantee that carbon burning propagated with a phase velocity that was initially supersonic. This procedure is very similar to the one previously followed by Niemeyer & Woosley (1997) and Röpke et al. (2007).
For a "detonator" radius of 150 km, an initially strong detonation decayed away after traversing an additional 70 km of "cold" carbon and oxygen. For a radius of 200 km, however, the detonation propagated successfully to the edge of the grid at 500 km. This is sufficiently far, considering that in the real star the density would have become higher and the detonation more robust. These detonators enclosed masses of 2.73 × 1028 g (150 km) and 6.47 × 1028 g (200 km), respectively.
A more precise descriptor of the critical detonation size may be the temperature gradient rather than the critical mass. For the two runs described here, the temperature gradients are 120 K cm−1 (failed detonation) and 90 K cm−1 (successful), respectively. Seitenzahl et al. (2009) studied the initiation of carbon detonation in spherical geometry and found a critical gradient of 4360 K cm−1 at a density of 5 × 106 g cm−3 (their Table 4). Our value is consistent with an admittedly uncertain extrapolation of their Figure 9 to 1.93 × 106 g cm−3.
More realistically, though, the detonator consists of helium, not carbon and oxygen, and the initial background is better approximated as isobaric rather than assuming constant density. An initial temperature of 2.8 × 109 K in the carbon also implies an unrealistically high energy density, not likely to be achieved at these low densities. A pure helium sphere with variable radius was surrounded by a thick shell of 50% 12C and 50% 16O again at 1.93 × 106 g cm−3 with a temperature of 1.0 × 108 K. The helium core was comprised of 200 Lagrangian mass shells of equal mass with a central temperature of only 1.0 × 109 K and a temperature at the edge of 1.0 × 108 K, and a constant gradient (with respect to radius) in between. As with the carbon detonator, the large value of central temperature assured a phase velocity for the helium burning that was initially supersonic and the well-zoned gradient implied the existence of a region where it was sonic. The density within the helium core was varied so as to provide a constant pressure equal to the pressure in the cold CO layer. Thus, pressure on the entire grid was initially 7.25 × 1022 dyne cm−2. Gravity was neglected and the pressure was initially held constant by applying a boundary pressure equal to the pressure on the grid. If the radius of the helium sphere was 211 km enclosing 6.37 × 1028 g, the detonation successfully propagated into the surrounding carbon. Another run with a helium sphere radius of 159 km (2.69 × 1028 g) failed to detonate the carbon shell, however.
The energy yield from carbon detonation at this density, taken from the calculation, is 3.3 × 1017 erg g−1. Oxygen does not burn here, but carbon and neon do, to magnesium and silicon. The yield from helium detonation, on the other hand, is only (5...6) × 1017 erg g−1 because only about one-third of the helium burns to 56Ni immediately behind the shock (the helium burning reaction rate saturates at high temperature). Some helium continues to burn well after the shock has passed, eventually raising the energy yield to 7 × 1017 erg g−1, but this energy is not so important for sustaining the shock wave. The critical radius is also the cube root of the critical mass. This explains the similarity between the runs using a CO detonator and a helium detonator at this density.
These results qualitatively agree with those obtained using a 2D representation of the full star in the CASTRO code (Table 3). They also agree reasonably well with the pure CO study at constant density described above. Apparently, the critical altitude (or detonator radius) is not very sensitive to the different energy yields of carbon and helium burning. This is somewhat surprising, but confirms the hypothesis that the critical altitude in the helium layer is one that would enclose the critical mass of carbon required for detonation at the interface density.
3.2. Shock Collisions and Hot Spots
To study the sliding helium detonation and the internal compressional wave which potentially produces the seed for a core detonation, we suppress nuclear burning in zones with more than 10% 12C. This is to prevent spurious carbon burning at the core–shell boundary due to the mixing of hot helium with cold carbon in a zone, and to prevent core detonation before the waves in the core have fully converged and produced the highest possible temperatures and densities (which we want to determine). For the sake of comparability, we here focus on the (0.801 + 0.143) M☉ model A for the most part. The detonation of WDs with 1.00 M☉ cores and lightweight helium shells is discussed in Section 3.2.6.
3.2.1. One Detonator
Here we consider the case of a single, spherical detonation spot setting off a helium detonation where the hottest layer (at r8 = 4.27) intersects with the positive z-axis in our coordinate system. This axisymmetric problem was investigated with different resolutions in three 2D runs (1, 4, and 5), and one 3D run (11) in a quarter-star-sized domain and mirror symmetries at the inner boundaries.
The helium detonation wave wraps around the star (see Figure 4(a)) and reaches the antipode of the detonator after about 1.2 s. For comparison, a sound wave in the helium shell would need about 5.6 s to reach the other side of the star. This corresponds to a front velocity of ∼1.1 × 109 cm s−1. The polar (latitudinal) velocity of the ash directly behind the front and the sound speed in the ash both are roughly 6.9 × 108 cm s−1. Their sum is larger than the actual front velocity, consistent with incomplete burning rather than a Chapman–Jouguet detonation (cf. Sim et al. 2012). The 56Ni fraction far (∼1000 km) behind the detonation front is about 70%.
Figure 4. Snapshots of simulations with one (a) and two synchronous detonators ((b) 54° separation and (c) 90° separation) during the helium detonation stage (upper panels) and during the presence of a hot spot in the core (lower panels). ((b) and (c)) x = 0 plane (right half), which contains the two detonators and the center of the star, is symmetric with respect to the y = 0 plane (left half) and vice versa; the long ticks at R = 0 indicate that these plots show not one but two orthogonal planes. The black contour lines represent, from the center outward, ρ = 2 × 107 g cm−3 (long dashed line), ρ = 107 g cm−3 (dotted line), XC = 0.49 (dashed line), ρ = 105 g cm−3 (dot-dashed line), and ρ = 104 g cm−3 (dot-dot-dot-dashed line).
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Standard image High-resolution imageThe sliding detonation induces an internal compressional wave that converges off-center inside the core on the z-axis (in general, the axis of symmetry in the problem). The average velocity with which the perturbation propagates in a negative z-direction from the helium ignition point to the final convergence point is ∼4.0 × 108 cm s−1, a little larger than the mean sound speed inside the core (3.4 × 108 cm s−1).
The temperatures and densities in some zones of run 1 are high enough to potentially3 trigger a core detonation where the internal wave finally converges (Niemeyer & Woosley 1997; Röpke et al. 2007; Seitenzahl et al. 2009). However, it is likely that the core ignites earlier, at a larger distance from the center and close to the core–shell interface on the z-axis, where the internal wave front converges in the polar direction (but not in the radial direction), and the converging helium detonation drives a hot, thin inflow of 56Ni in a positive direction along the z-axis. As a numerical experiment, we restarted run 1 without suppressing the burning of carbon-rich zones at times t = 1.2 s (when the helium detonation converges), 1.3 s, 1.4 s, and 1.5 s (when the internal wave converges). In all of these cases, a detonation wave in the core forms immediately.
Table 4. Conditions at the Hot Spot Induced by Converging Compressional Waves in the Core
Run | Model | αa | τb | Δxc | Δtd | t | z | re | T | ρ | Typef |
---|---|---|---|---|---|---|---|---|---|---|---|
(s) | (km) | (s) | (s) | (108 cm) | (108 cm) | (109 K) | (107 g cm−3) | ||||
1 | A | ⋅⋅⋅ | ⋅⋅⋅ | 6.51 | 0.05 | 1.50 | −1.90 | 1.90 | 5.25 | 6.21 | p |
2 | A | 180° | ⋅⋅⋅ | 6.51 | 0.05 | 1.40 | ±1.45 | 1.45 | 1.93 | 3.55 | r |
3 | A | 180° | 0.30 | 6.51 | 0.05 | 1.45 | −1.72 | 1.72 | 3.34 | 4.00 | r |
4 | A | ⋅⋅⋅ | ⋅⋅⋅ | 14.6 | 0.02 | 1.48 | −1.87 | 1.87 | 8.09 | 2.68 | p |
3.66g | 0.02 | 1.48 | −1.92 | 1.92 | 9.61 | 2.54 | p | ||||
5 | A | ⋅⋅⋅ | ⋅⋅⋅ | 25.0 | 0.05 | 1.55 | −1.96 | 1.96 | 3.09 | 4.29 | p |
25.0 | 0.005 | 1.515 | −1.91 | 1.91 | 5.51 | 20.9 | p | ||||
6 | A | 54° | ⋅⋅⋅ | 25.0 | 0.05 | 1.40 | −1.76 | 1.77 | 2.81 | 5.66 | p |
7 | A | 54° | 0.15 | 25.0 | 0.05 | 1.45 | −1.74 | 1.80 | 3.67 | 9.51 | p |
8 | A | 90° | ⋅⋅⋅ | 25.0 | 0.05 | 1.40 | −1.39 | 1.54 | 2.17 | 5.04 | t |
9 | A | 120° | 0.30 | 25.0 | 0.05 | 1.50 | −0.91 | 1.96 | 2.86 | 3.59 | t |
10 | A | 120°, 90°, 100° | 0.30, 0.20 | 25.0 | 0.05 | 1.45 | −0.71 | 1.65 | 2.19 | 5.27 | t |
11h | A | ⋅⋅⋅ | ⋅⋅⋅ | 52.1 | 0.05 | 1.55 | −1.95 | 1.95 | 2.96 | 7.56 | p |
12 | A | 36° | ⋅⋅⋅ | 52.1 | 0.05 | 1.45 | −1.74 | 1.74 | 2.19 | 4.93 | p |
13 | A | 54° | ⋅⋅⋅ | 52.1 | 0.05 | 1.45 | −1.74 | 1.81 | 2.00 | 4.24 | p |
14 | E | ⋅⋅⋅ | ⋅⋅⋅ | 6.51 | 0.05 | 1.40 | −1.70 | 1.40 | 3.52 | 4.54 | p |
15 | E | 180° | ⋅⋅⋅ | 6.51 | 0.05 | 0.60 | 0 | 3.48 | 3.48 | 0.60 | b |
16 | D | ⋅⋅⋅ | ⋅⋅⋅ | 6.51 | 0.05 | 1.80 | −2.13 | 2.13 | 2.44 | 3.31 | p |
17 | D | 180° | ⋅⋅⋅ | 6.51 | 0.05 | ⋅⋅⋅ | ⋅⋅⋅ | ⋅⋅⋅ | ⋅⋅⋅ | ⋅⋅⋅ | ⋅⋅⋅ |
Notes. aAngular separation(s) of the detonators in cases with multiple detonators. bDelay of the second (and third) detonator. cGrid resolution at the highest AMR level that includes the hot spot. dCadence of the considered snapshots. eDistance from the center (spherical radius). fType of the listed hot spot: (p) where primary waves converge, (r) where reflected waves collide, (t) where a wave passes through others and converges, or (b) near the core boundary, where primary waves first collide. gRestarted with finer zoning in the region where the internal wave converges. hDespite this being a 2D problem, this run was done in 3D.
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The values of the density and temperature in the hot spot are dependent on the spatial resolution Δx of the grid as well as on the temporal separation Δt of the considered snapshots (for practical reasons, we do not edit and analyze the results at every time step), cf., the values of temperature and density in the hot spots of runs 1, 4, 5, and 11 listed in Table 4. However, all results unequivocally indicate that the core would detonate. We expect that a higher resolution would only increase the likelihood for detonation.
3.2.2. Opposite Detonators
As a limiting case of multi-point ignition, we at first consider two detonators at opposite points in the helium shell (run 2). While it is unlikely for such detonators to be synchronous, this poses a computationally inexpensive 2D problem which can be regarded as a numerical experiment. The internal waves in this case collide on the z = 0 plane (the detonators being centered on the z-axis at z8 = ±4.27), beginning at the outer edge of the core at t = 0.60 s and reaching the center at t = 1.05 s. The final wave collision in the central part of the star takes place on a ∼1400 km wide disk without generating a discernible hot spot. However, temperatures ≳ 109 K occur on the collision plane at large radii (r8 ∼ 1.8–3.2). While the material is not compressed there, we observe a radially inward moving core detonation in a run where the burning of carbon is allowed for t ⩾ 0.65 s. If carbon burning is suppressed, the original core waves are reflected at the z = 0 plane. The reflected waves collide on the z-axis (symmetrically on both sides of the z = 0 plane), creating dense hot spots at z8 = ±1.45 that would very likely have ignited the core if ignition had failed earlier.
When one of the detonators (in our case the one on the negative side of the z-axis) is delayed by 0.30 s, the two helium detonation fronts collide at t = 0.75 s at an angle of 112° with respect to the positive z-axis; see Figure 5. As in the synchronous case, the collision of the primary internal waves, which here happens on a slightly curved disk at z ≈ −600 km, does not generate a hot spot. However, a wave reflected toward the negative z-axis produces a hot spot that is sufficiently dense to trigger core detonation.
Figure 5. Three snapshots of a 2D simulation with asynchronous detonators on opposite sides (run 3): when the helium detonation fronts collide (left), when the internal wave converges (middle), and when reflected waves produce a hot spot (right). The blue dashed line indicates the core–shell boundary. Only the inner part of the simulation box is shown.
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Standard image High-resolution image3.2.3. Two Synchronous Detonators
Before discussing 3D cases of two-point ignition in the helium, it is worth noting that a single, small aspherical detonator is virtually equivalent to a spherical one, regardless of how strongly deformed it is (as long as it sets off a detonation). As the detonation expands with constant velocity in every direction, the original asphericity is quickly lost. To assess the effects of non-axisymmetry on the focusing of the internal waves, we therefore consider cases with two detonators at varying but significant separation from one another. For two synchronous detonators, it suffices to perform a 3D simulation of a quarter of the star, with mirror symmetry at the inner boundaries.
In cases with two moderately separated, synchronous detonators (we consider angular separations of 36°, 54°, and 90°), the initially separate helium detonation fronts collide halfway between the two spots on the geodesic connecting them on the core surface, in our case the positive z-axis. While the detonations merge, the combined front proceeds toward the antipode of this collision point. The front initially has a head start on the plane that connects the two spots with the center of the star (the x = 0 plane in our simulations), but the deficit becomes smaller as the detonations continue to merge.4 As it approaches the antipode, the detonation front has the shape of a pointed ellipse. This shape can easily be understood considering the combined detonation as a superposition of two detonations: the pointed ellipse is the intersection between two circles (or, more precisely, lines of constant latitude, if the ignition points are regarded as poles) whose centers are the respective antipodes of the ignition points. In a simulation, the detonation finally converges when the width of the pointed ellipse approaches the size of a grid zone. Theoretically, the ratio of the length of the ellipse compared to its width increases indefinitely, i.e., the wave always converges in a line rather than a point and the difference between having one and two detonators should become larger with increasing grid resolution or diffusion length.
In cases with 36° and 54° detonator separation, the region in which the internal waves converge becomes sufficiently hot and dense to trigger a core detonation; see Table 4 and Figure 4(b). We explicitly confirmed this for run 13 by switching on carbon burning for t > 1.40 s. When two synchronous detonators are 90° apart (run 8), there is no hot spot at the site where the two primary waves converge at the z-axis (in general, the intersection of the two planes of symmetry in this problem). However, the waves induced by the two detonators pass through one another and form two hot spots at a considerable distance (660 km) from the z-axis; see Figure 4(c).
3.2.4. Two Asynchronous Detonators
We next consider a case of two asynchronous detonators with an angular separation of 54°, run 7. Note that this scenario is less symmetric than the case of two synchronous detonators, there being only one mirror symmetry in the problem, across the plane which intersects both detonators. We therefore use a 3D domain that comprises half of the star and assume mirror symmetry at the inner boundary. One of the detonators—the one on the +y side in our simulations—is set off 0.15 s (roughly half the time needed for the first detonation to reach the second detonator) after the first one.5 Shortly before converging, the helium detonation front assumes the shape defined by the intersection of two circles with different radii; see Figure 6. The same shape can be seen in the internal wave front on concentric spherical surfaces. Just like in the synchronous case (run 6), a dense hot spot forms when the internal wave fronts converge; see Figure 7 and the rightmost snapshot in Figure 6.
Figure 6. Helium shell detonation started by two asynchronous detonators with a 54° separation in the hottest helium layer (run 7). The gray, yellow, and green isosurfaces indicate the boundary of the CO core, the detonation front, and the internal compressional wave, respectively. The sketch next to the snapshot at t = 1.05 s (second from right) qualitatively mimics the shape of the converging detonation front as the intersection of two circles. The red isosurfaces indicate the hot spot that is generated when the internal wave converges (rightmost snapshot).
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Standard image High-resolution imageFigure 7. Snapshots of the temperature in a simulation with two asynchronous detonators at ±27° from the positive z-axis on the x = 0 plane (run 7). The x = 0 plane (right panels) contains the detonators and the center of the star, and the orthogonal y8 = 0.46 plane (left panels) contains a hot spot generated by converging internal waves. The detonator on the positive side of the y-axis is delayed by 0.15 s. The black contour lines represent, from the center outward, ρ = 2 × 107 g cm−3 (long dashed line), ρ = 107 g cm−3 (dotted line), XC = 0.49 (dashed line), ρ = 105 g cm−3 (dot-dashed line), and ρ = 104 g cm−3 (dot-dot-dot-dashed line). The snapshot at the bottom is taken when the internal wave fronts converge.
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Standard image High-resolution imageWith 120° separation and a delay of 0.30 s, run 9, there is no hot spot where the internal waves from the two detonators converge. As in the case with synchronous detonators at 90° discussed above, the waves from the two detonators pass through one another. The wave from the first detonator is the first to converge and trigger a core detonation.
3.2.5. Three Asynchronous Detonators
Unlike the above cases, a setup with three or more detonators is in general free of symmetries and requires a 3D simulation of the full star. In run 10, we again consider two detonators (A and B) with a separation of 120°, one of which (B) is delayed by 0.30 s, exactly as in run 9. In addition, a third detonator C, delayed by 0.20 s, is placed 90° from detonator A and 100° from detonator B on the positive x side. In this case, when the helium detonation converges toward the last patch of unburnt helium, it roughly has a triangular shape. The same shape is present in the internal wave on concentric spherical surfaces. There is a distinct hot spot when the internal waves converge. Shortly after, a secondary hot spot arises as the wave induced by the first detonator converges again with itself. Figure 8 shows snapshots of both hot spots (right-hand panels) and the converging wave fronts from which they originate (left-hand panels).
Figure 8. Snapshots of the temperature in a simulation with three detonators (run 10) on a concentric sphere inside the core which contains the hot spot from the three converging waves (upper right panel) and the hot spot from the wave induced by the first detonator alone (lower right panel).
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Standard image High-resolution image3.2.6. Light Helium Shells
Here we consider axisymmetric detonations (one detonator or two opposite detonators) for progenitor models other than A. A detonation in a 0.078 M☉ helium shell on top of a solar mass core (model E, run 14) is set off by a 25 km spherical detonator centered on the hottest helium layer. The sliding helium detonation yields a distinct hot spot where the internal wave converges at t ≈ 1.40 s. With carbon burning turned on from the time when the helium detonation converges (t ≈ 1.10 s), the core immediately detonates near its surface. This detonation is triggered by a thin, hot radial inflow of 56Ni. As shown in the upper panel of Figure 9, temperatures of 2–4 × 109 K and densities on the order of 107 g cm−3 are generated along this jet. In a simulation with two synchronous, opposite detonators, run 15, temperatures >109 K are generated neither when the wave fronts converge at the center, nor along the z-axis when the reflected waves collide (in contrast with model A, run 2). The only region hot enough to light the core in this case is located at the equatorial plane near the core's surface, where the collision of the internal waves begins. Although there is no hot inflow comparable to the case with one detonator (note that a radial inflow in this case is not a jet; see the lower panel in Figure 9) the core there ignites in the simulation.
Figure 9. Conditions near the core boundary as a function of distance from the center. Top panel: on the line (negative z-axis) where the helium detonation front converges in a run with one detonator (run 14). Bottom panel: on the helium collision plane (z = 0) in a run with two opposite synchronous detonators (run 15). The vertical lines mark the initial radius of the core–shell interface. The plots represent calculations where carbon burning is suppressed; otherwise, the core ignites at the earliest time (dot-dot-dot-dashed line) in both cases.
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Standard image High-resolution imageIt is difficult to set off a detonation in a 0.045 M☉ helium shell surrounding a one solar mass core (model D). We did not succeed with a spherical detonator centered on the hottest helium layer, whose density is 7.17 × 105 g cm−3. A detonation does not start even with a (perhaps unrealistically) strong initial detonator: a central temperature of 3 × 109 K, linearly decreasing to 1.5 × 109 K at the outer edge, a density three times that of the ambient medium, and a radius of 25 km (ending 1 km above the core–shell interface). Large shock velocities (we tried 1.6 × 109 cm s−1 instead of our usual 8 × 108 cm s−1) at the outer edge of the detonation spot did not help either.
A detonation in the 0.045 M☉ shell of model D can be set off, however, by a large spherical detonator of radius 50 km (which is about twice the distance between the core–shell interface and the hottest helium layer) centered 25 km above the hottest helium layer. The resulting detonation front is feebler than in all cases with heavier helium shells, blowing out at too coarse a resolution (≲2 km works, 6.5 km does not) and requiring the use of AMR in our simulated helium shell. However, once started, the detonation propagates around the star and converges after ≈1.40 s (run 16). The corresponding front velocity is ∼9.4 × 108 cm s−1 ≈ 4.3 times the sound speed in the hottest helium layer. When the internal wave induced by the helium detonation converges 0.40 s later, it forms a distinct hot spot. Without suppression of the carbon burning, the core detonates immediately after the convergence of the helium detonation, starting at the z-axis near the core–shell boundary. In a simulation with two synchronous, opposite detonators, run 17, no hot spot is formed in the core. With carbon burning turned on, the core does not detonate in the simulation.
3.3. Ignition in an Extended Region
As stated in the above paragraph, a spherical detonator in model D needs to be fairly large to set off a helium detonation. This, however, is not compatible with a runaway starting at the hottest layer in the helium shell. As an alternative, we here consider the possibility of a thermonuclear runaway starting in a (curved) sheet on an equipotential, instead of a single point. The size of convective cells in the helium shell is expected to be on the order of the pressure scale height, which is 366 km at the hottest helium layer in model D. The size of the region where the runaway starts could be a substantial fraction of this, but is probably not larger. As a toy model, we consider detonation spots in the form of spherical caps with a thickness of 50 km. Selected runs are listed in Table 5 and examples for a successful and an unsuccessful detonation are shown in Figure 10. As in most of our detonators, the temperature decreases linearly from 2 × 109 K at the center to 1.8 × 109 K at the outer edge (on all sides of the cap). The outer rims of the caps are half tori, imposed with a velocity that increases linearly from the torus center to the outer edge. An arc length of 50 km constitutes a limiting case in which the cap degenerates into a sphere with the same properties as our spherical detonators.
Figure 10. Successful (top) and unsuccessful (bottom) initiation of a detonation in the helium shell of model D with a detonator in the form of a spherical cap. The cases shown are the last two in Table 5. The color bar ranges from the minimum to the maximum temperature in each plot (note the decline of the maximum in case of failure). The gray contour line, at 49% 12C, marks the core–shell interface.
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Standard image High-resolution imageTable 5. Detonations Started in a Spherical Cap
Altitudea | Arc Length | Rim Density | Rim Velocity | Detonates |
---|---|---|---|---|
(km) | (km) | (108 cm s−1) | ||
0 | 141 | 2 × ambient | 8 | Yes |
0 | 96 | 2 × ambient | 8 | No |
0 | 233 | Ambient | 8 | Yes |
0 | 141 | Ambient | 8 | Yesb |
0 | 96 | Ambient | 8 | No |
0 | 415 | Ambient | 1 | Yes |
0 | 233 | Ambient | 1 | No |
0 | 415 | Ambient | 0.5 | No |
0 | 781 | Ambient | 0.5 | Yesb |
25 | 785 | Ambient | 1 | Yes |
25 | 418 | Ambient | 1 | No |
Notes. aRadial distance from the hottest helium layer to the center of the cap. bDetonation moves only inward at first and is then reflected back.
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The cap detonator is more powerful than a spherical one with the same radial (with respect to the center of the star) extent. Detonations can be initiated at ambient density with subsonic starter velocities. Smaller sizes require harsher starting conditions. Below a size of ∼100 km (roughly one-third pressure scale height), the initiation of a detonation appears impossible. For the given density of ∼7 × 105 g cm-3 near the temperature maximum of model D, this limit is in approximate agreement with the recent findings of Holcomb et al. (2013), who determined the critical sizes of helium detonation for a wide range of densities in a series of 1D simulations.
3.4. Complete Detonations
Table 6 lists the yields from helium shell detonations in different models, measured at the time when the helium detonation converges opposite the detonator (we only consider single detonators here, not expecting the yields from detonations started at multiple points to be much different). The lightweight helium shell in model D produces little 56Ni, only about 5% of what the heavier shell in model E produces, but the yields of isotopes with mass numbers between 36Ar and 52Fe are in total about twice as high as in model E.
Table 6. Nucleosynthesis Yields in the Helium Shell (M☉)
Model A | Model E | Model D | |
---|---|---|---|
12C | 8.00 × 10−4 | 5.24 × 10−4 | 7.02 × 10−4 |
14N | 1.11 × 10−10 | 2.83 × 10−14 | 4.24 × 10−13 |
16O | 3.19 × 10−4 | 1.93 × 10−4 | 2.46 × 10−5 |
20Ne | 4.78 × 10−5 | 2.72 × 10−5 | 1.95 × 10−5 |
24Mg | 9.40 × 10−5 | 5.30 × 10−5 | 3.00 × 10−5 |
28Si | 4.46 × 10−4 | 2.65 × 10−4 | 2.03 × 10−4 |
32S | 2.88 × 10−4 | 1.26 × 10−3 | 2.17 × 10−4 |
36Ar | 4.55 × 10−4 | 2.65 × 10−4 | 4.62 × 10−3 |
40Ca | 2.15 × 10−3 | 1.26 × 10−3 | 2.17 × 10−3 |
44Ti | 4.14 × 10−3 | 2.33 × 10−3 | 4.29 × 10−3 |
48Cr | 4.24 × 10−3 | 2.36 × 10−3 | 4.39 × 10−3 |
52Fe | 7.81 × 10−3 | 4.34 × 10−3 | 5.69 × 10−3 |
54Fe | 1.80 × 10−5 | 2.57 × 10−6 | 5.16 × 10−7 |
56Ni | 7.05 × 10−2 | 3.71 × 10−2 | 1.95 × 10−3 |
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We followed the detonation of the core and the expansion of the ejecta to scales of 106 km (about 200 times the size of the initial WD), at which time the expansion is homologous. The total nickel yields in models A, D, and E are 0.38 M☉, 0.52 M☉, and 0.66 M☉, respectively. Mass fractions of selected isotopes in models E and D are plotted in Figure 11. The inner parts of the core turn into almost pure 56Ni in both cases, whereas the outer parts yield mainly 28Si and 32S. The lighter helium shell produces large fractions of 40Ca, 44Ti, 48Cr, and 52Fe instead of 56Ni, which is the dominant product of the heavier shell.
Figure 11. Mass fractions of different isotopes along the equatorial plane (z = 0) in the ejecta of models E (top panel) and D (bottom panel) after complete shell and core detonations, as functions of radial velocity (which is approximately proportional to radius). In both panels, only isotopes with maximum fractions >10% are plotted, respectively.
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Standard image High-resolution image4. SUMMARY AND DISCUSSION
We studied the double detonation scenario for Type Ia supernovae by means of 2D and 3D simulations. Starting from the results of 1D stellar evolution simulations, we find that the helium detonation wave is halted at the core–shell interface if the detonation starts in the hottest layer, which in general is located at some altitude above the interface. If the detonation commences at higher altitude, the detonation may transcend into the core. For direct drive to be successful, the helium detonation must involve a critical mass which is sensitive to the density at the core–shell interface. A layer of mixed core–shell material does not facilitate the direct drive. In marginal cases, the detonation transcends the core–shell interface but then fragments, opening up the possibility of incomplete core detonations.
We confirm that the sliding helium detonation induces a mildly supersonic compressional wave inside the core which, if the detonation is set off at a single point in the helium shell, converges to produce an off-center spot that is sufficiently hot and dense to light the core as well. We tested the robustness of this model for non-symmetric initial conditions, considering a series of scenarios in which the helium detonation is started at two points and one scenario in which it is started at three points. We find that the secondary core detonation is quite robust, despite the lack of symmetry. In cases where detonators are widely separated (≳90°), the hot spot is produced by reflected waves or waves that have passed through other waves before converging with themselves, rather than the converging primary waves. Only in one extreme case—two antipolar, synchronous detonators in the helium shell of a (1.002 + 0.045) M☉ WD—do we find no hot spot and no core ignition.
The generation of a detonation-inducing hot spot is robust even in a completely non-symmetric setup with three asynchronous detonators. Geometric arguments suggest that it is even more robust than a setup with two detonators, where the helium detonation and the core waves converge in an elongated region. As the elongation increases with the smallest possible separation of the detonation fronts, the difference of having one, two, or three detonators might be larger at higher resolution. Although we have not run cases with more than three detonators, we expect that the core ignition would not be thwarted by additional detonators. A case with numerous detonators may be similar to a detonation in a spherical shell.
After the helium detonation has converged, the internal waves converge in the polar (latitudinal) direction at ever decreasing radii, beginning right beneath the core–shell interface. In addition, the collision of the helium detonation front can drive a jet of hot ash into the core. In any case, this region has high ignition potential. That is, the core may ignite at large radii before the "proper" hot spot forms deeper inside as the wave fronts converge also in the radial direction. The complete convergence of internal waves may only happen in cores that are difficult to ignite.
Our simulations suggest that it is very hard, perhaps impossible under realistic assumptions, to initiate a helium detonation at densities ≲ 106 g cm−3 (as observed in plane-parallel geometry by Townsley et al. 2012). On the other hand, the yields from WDs with thin helium shells are most compatible with observed Type Ia supernovae. Detonations in the helium are more easily started in an extended sheet rather than a point. Our simulations indicate that the size of such a sheet would have to be at least on the order of the size of a convective cell in the helium shell of a quasi-stationary WD. Whether detonation seeds of this kind are realistic can ultimately be answered only by suitable 3D convection simulations. Alternatively, a sufficiently large region may reach the conditions for helium detonations in the context of double-degenerate mergers (which are not directly considered in this work), by the interaction of an accretion stream with previously accreted helium (Guillochon et al. 2010) or during the merger itself (Raskin et al. 2012).
This research has been supported by the DOE SciDAC Program under contract DE-FC02-06ER41438, the National Science Foundation (AST 0909129), and the NASA Theory Program (NNX09AK36G). We acknowledge useful discussions with Haitao Ma concerning the implementation of detonation physics in CASTRO. We also thank John Bell and Ann Almgren for their major roles in developing the CASTRO code. R. Moll acknowledges support by the Alexander von Humboldt Foundation through the Feodor Lynen Research Fellowship program. This research used resources of the National Energy Research Scientific Computing Center, which is supported by the Office of Science of the U.S. Department of Energy under Contract No. DE-AC02-05CH11231. This research used resources of the Oak Ridge Leadership Computing Facility at the Oak Ridge National Laboratory, which is supported by the Office of Science of the U.S. Department of Energy under Contract No. DE-AC05-00OR22725.
Footnotes
- 1
The spheroidal detonation spot was constructed using the same temperature and velocity profiles with respect to the distance of the surface of the spot as for spherical detonators. However, this means that the energy contents (kinetic and thermal) are different. The distance to the core–shell interface may not be large enough for the detonation wave to lose all information of its (artificial) initiation besides curvature. This complicates the comparison. However, as the explosions induced by the spheroidal detonators are in general stronger (consistent with a higher energy content), we can still draw conclusions about the non-importance of curvature if direct drive with such a detonator fails.
- 2
Given that this displacement is becoming comparable to the size of the detonator itself, it is questionable whether or not direct drive will work for the most massive models. Also, the exact location of the hot layer is probably not known to this precision due to the 1D mixing length approximation used to treat convection. Multi-dimensional simulation of the convection during the preexplosive runaway might provide additional insight.
- 3
Whether a spontaneous detonation initiates depends not only on the density, the peak temperature, and the size of the region (or, equivalently, its mass), but also on the shape of the temperature profile (as emphasized by Seitenzahl et al. 2009). The conditions in the hottest zone are listed in Table 4. Since the grid zones in our simulations are usually larger than the critical masses for detonation, it is not possible to predict with certainty whether the conditions in one or a few zones lead to detonation.
- 4
For comparison, consider two merging detonations in a plane, starting from the x-axis at ±a. With r being the radius of an individual detonation, the height of the combined detonation on the y-axis is , asymptotically approaching r (and not r−a) at large radii. That is, the two initially separate detonations become indistinguishable when their size is much larger than the initial separation.
- 5
We implemented this in the code by suppressing the time-step update of the zones comprising the detonation spot for the said time.