A&A 450, 1037-1050 (2006)
DOI: 10.1051/0004-6361:20054626
L.-S. The 1 - D. D. Clayton1 - R. Diehl2 - D. H. Hartmann1 - A. F. Iyudin2,3 - M. D. Leising1 - B. S. Meyer1 - Y. Motizuki4 - V. Schönfelder2
1 - Department of Physics and Astronomy,
Clemson University, Clemson, SC 29634-0978, USA
2 -
Max-Planck-Institut für Extraterrestrische Physik,
Postfach 1312, 85741 Garching, Germany
3 -
Skobeltsyn Institute of Nuclear Physics, Moscow State University,
Vorob'evy Gory, 119992 Moscow, Russia
4 -
Cyclotron Center, RIKEN, Hirosawa 2-1, Wako 351-0198, Japan
Received 1 December 2005 / Accepted 15 December 2005
Abstract
According to standard models supernovae produce radioactive 44Ti,
which should be visible in gamma-rays following decay to 44Ca
for a few centuries.
44Ti production is believed to be the source of cosmic 44Ca, whose
abundance is well established.
Yet, gamma-ray telescopes have not seen the
expected young remnants of core collapse events. The 44Ti mean life of
89 y and the Galactic supernova rate of
3/100 y imply
several detectable 44Ti gamma-ray sources, but only one is clearly
seen, the 340-year-old Cas A SNR.
Furthermore, supernovae which produce much 44Ti are expected to occur primarily
in the inner part of the Galaxy, where young massive stars are
most abundant. Because the Galaxy is transparent to gamma-rays, this
should be the dominant location of expected gamma-ray sources.
Yet the Cas A SNR as the only one source is located far from
the inner Galaxy (at longitude 112
).
We evaluate the surprising absence of detectable supernovae from
the past three centuries.
We discuss whether our understanding of SN explosions, their
44Ti yields, their spatial distributions, and statistical arguments
can be stretched so that this apparent disagreement may be accommodated within
reasonable expectations, or if we have to revise
some or all of the above aspects to bring expectations in agreement with the
observations.
We conclude that either core collapse supernovae have been improbably
rare in the Galaxy during the past few centuries, or 44Ti-producing supernovae
are atypical supernovae.
We also present a new argument based on 44Ca/40Ca ratios
in mainstream SiC stardust grains that may cast doubt on
massive-He-cap type I supernovae as the source of most galactic 44Ca.
Key words: ISM: abundances - Galaxy: abundances - gamma rays: observations - ISM: supernova remnants - supernovae: general - dust, extinction
Supernovae are the agents that drive the evolution of gaseous regions of galaxies. As end points of the evolution of massive stars that have formed out of the interstellar gas, their explosions eject matter enriched with freshly formed isotopes and stir interstellar gas. However, the explosions themselves are still not understood (Janka et al. 2003; Burrows 2000). Parametric descriptions are used to describe the core collapses ("cc-SN'', supernovae of types II and Ib/c) (Woosley & Weaver 1995; Thielemann et al. 1996) as well as thermonuclear explosions of white dwarfs (supernovae of type Ia; Nomoto et al. 1997). A prominent issue in astrophysics is whether the supernova explosion itself is a well-regulated, robust physical process, or if intrinsic variability over a wider range of physical conditions are rather common.
Supernova homogeneity by type can be studied in different ways. One approach is to analyze the rate of supernovae of a specific type in different environments and over different time scales. In this work we do this by asking if the current rate of supernovae in our Galaxy which produce radioactive 44Ti is in line with expectations from other observables and from supernova theory.
44Ti decay offers a unique window to the study of supernova rates. Specific aspects of this window are:
Supernova rates in the Galaxy can be inferred from different observables. But observational incompleteness and bias requires that several assumptions are an essential part of such inferences. We compare here the observed 44Ti sky with expectations for the occurrences of young 44Ti emitting supernova remnants, as they result from astrophysical assessments of supernova characteristics for our Galaxy. We choose a time interval unit of 100 years for comparison of chemical history with supernova event rates. The extrapolation of the past history and yields of 44Ti-ejecting supernova events should give a production rate which can be compared with recent supernova rates, as no other source of 44Ca has yet been identified.
Have the 44Ca-producing supernovae been typical; is all of 44Ca produced through radioactive 44Ti; or do exceptional events contribute most of the 44Ti? Gamma-ray surveys for 44Ti sources, and presolar supernova grains provide ways to address this question.
In the following section we will then examine each of the critical assumptions in more detail.
For a 44Ti sky reference, we adopt the result from COMPTEL's survey in the 1.157 MeV band, which is the most complete survey to date (Dupraz et al. 1997; Iyudin et al. 1999). In this survey, one object has been clearly detected (340-year-old Cas A at a distance of 3.4 kpc), candidates at lower significance have been discussed (most prominently GRO J0852-4642 in the Vela region, Iyudin et al. 1999), and a weak signal from the Per OB2 association (Dupraz et al. 1997). Apparently, no bright young 44Ti emitting supernova remnants are found in the inner region of the Galaxy (see Fig. 1).
What do we expect the Galaxy to look like in 44Ti emission?
Supernova observations directly demonstrate
that these events are at the origin of 44Ti production:
the 1.157 MeV
-ray line following
44Ti decay has been detected in the 340-year old Galactic supernova remnant
Cas A (Iyudin et al. 1994; Vink et al. 2001).
Furthermore, SN1987A's late light curve, observed in unique detail
over more than 15 years, appears powered by
a similar amount of 44Ti (0.2-
),
from modeling of
radioactive energy deposition and photon transport
in the SNR (Fransson & Kozma 2002; Woosley et al. 1989).
Gamma-ray detection and proof of this interpretation
is still lacking, but INTEGRAL's
recent observations may prove sufficiently sensitive.
| |
Figure 1:
Maximum-entropy map of the Galactic plane
(within latitude |
| Open with DEXTER | |
Presolar grains have been identified in meteoritic samples through their unusual isotopic abundance patterns, and hold rich isotopic abundance detail for characterizing their condensation environments (e.g. Clayton & Nittler 2004; Zinner 1998). SiC grains of the X-type are attributed to core-collapse supernovae from their large excesses in characteristic isotopes (Nittler et al. 1996). 44Ti-produced overabundance of 44Ca is found in these SiC X grains, indicating presence of 44Ti at their time of condensation. Measured 44Ca/40Ca ratios are large (Nittler et al. 1996; Clayton et al. 1997a; Hoppe et al. 2000). This proves their supernova origin, on one hand, and likewise it proves that dust-producing supernovae may eject 44Ti in significant amounts. Their attribution to core collapse supernovae rather than supernovae of type Ia (Nittler et al. 1996) is plausible, if we believe that core collapse supernovae probably dominate 44Ti production and because there is no direct evidence of dust condensation in thermonuclear supernovae (Dwek 1998). It is likely that all of the observed X grains sample both different condensation environments and different production events. Therefore, their 44Ca abundances cannot be interpreted in absolute terms as a measure of the mass of 44Ti ejected per supernova.
The most plausible cosmic environment for production of 44Ti is
the
-rich freeze-out from high-temperature burning near
Nuclear Statistical Equilibrium
(e.g. Arnett 1996; Woosley et al. 1973).
The required high values for the entropy are found in core-collapse
supernovae.
Therefore the simplest plausible assumption is that
core-collapse supernovae are responsible
for any substantial sources of 44Ti.
It is likewise plausible that traditional SNIa do not add significantly to nucleosynthesis at mass A = 44, specifically no 44Ti, since their NSE freeze-out conditions will not be favorable for 44Ti production (Timmes et al. 1995). We consider the symbiotic-star scenario as a rare subclass of SNIa, even though their 44Ti yields may be large (Woosley & Weaver 1994); so they indeed would be rare outliers, rather than typical 44Ti producing supernovae. We will discuss uncertainties in each of these sites in more detail below (see Sect. 3.5).
Measurements of cosmic isotopic abundances can be converted into isotope production rates; however, for all long-lived isotopes models of chemical evolution have to be applied (e.g. Matteucci 2003; Timmes et al. 1995; Clayton 1988; Pagel 1997). How can we use these for predicting the shortlived 44Ti source appearance in gamma-rays? Its lifetime is too short for mean chemical evolution arguments.
Over the time scale of chemical evolution of the Galaxy, the cumulative and
averaging effects of different explosion types would integrate to a smooth
pattern of "standard abundances'',
as they are observed throughout the universe.
Evolutionary pathways for individual elements can be associated
with the evolution of metallicity and the rates of different supernova types.
The abundance of 44Ca in solar-system matter thus
can be translated through
models of chemical evolution into a current average production rate of
of 44Ti per 100 y
(Leising & Share 1990, see below).
Chemical evolution calculations (Timmes et al. 1995) using computed ejecta masses (Woosley & Weaver 1995) were shown to account reasonably for most solar abundances, including specifically 40Ca, but failing by a factor of three for 44Ca; this fact is also evident from the ratio of 44Ti to Fe in cc-SN models. But over short time scales where only a limited number of source events contribute, great variability among sources would present a significant difference of the present-day picture from the average. Therefore we may compare the expectations from long-term averaged 44Ti production to the present-day 44Ti source record imaged in gamma-rays, allowing for the short-term fluctuations with Monte-Carlo realizations of the sources.
The solar-system 44Ca abundance is rooted plausibly in
44Ti nucleosynthesis (Clayton 1982; Woosley et al. 1973),
and is a result of the
integrated Galactic nucleosynthesis prior to formation of the solar system.
Given a time-dependence of the production rate, it can be
normalized to the rate required to give precisely the measured solar
abundance 4.5 Gyr ago, which also fixes the long-term average
production rate today. Models of galactic chemical evolution,
constrained by a number of observables, provide us with that
time dependence, albeit subject to a number of assumptions and
parameter choices.
Adjusting the 44Ti yield in the aforementioned calculation
(Timmes et al. 1995)
upward by a factor of three to achieve the solar abundance,
we infer a production rate of
44Ca of about
yr-1.
Other considerations using different chemical evolution models
(see Appendix C) lead from the 44Ca abundance to a
current 44Ti production rate:
p(44Ti) =
yr-1, with full uncertainty
range 1.2-
yr-1 (see Appendix C).
Direct supernova rate measures have been made through correlations between
supernova activity and other tracers of the massive star content of a
galaxy.
van den Bergh (1991)
finds (
)
h1002 SN century-1. For
h100= 0.75, the rate is
SN century-1.
This rate is based on a
combined study of galactic supernova remnants, historical SNe, and novae
in M 31 and M 33. Cappellaro et al. (1993) refer to this rate as the
best estimate. van den Bergh & Tammann (1991)
find SNR = 4.0 SN century-1. The authors review supernova rates in external
galaxies and derive a specific supernova frequency, in units of
1 SNu = one SN per century per 1010
(B), for various galaxy types. If one
assumes that the Galaxy is intermediate between types Sab-Sb and types
Sbc-Sd, the specific rate is 3
h1002 SNu. For a Galactic blue-band
luminosity of L(B) =
(B) (their Table 11)
and
h100 = 0.75 we
infer SNR = 4.0 SN century-1. Their review paper also discusses estimates
from internal tracers in the Milky Way: from radio supernova remnant
(RSNR) statistics they infer SNR =
SN century-1. From the
historic record of nearby (<a few kpc) supernovae in the past millennium
they find SNR = 5.8
SN century-1.
The large extinction corrections in
the galactic plane make this small sample highly incomplete, which results
in large uncertainties in extrapolations to the full galactic disk. The
authors also review efforts based on the pulsar birth rate, but extensive
observational selection effects in combination with the strong and poorly
understood evolution of luminosity and beaming geometry
(see Lyne & Graham-Smith 1998; and Lorimer & Kramer 2004)
renders this method
impractical for estimating the galactic SNR. Continuing the studies of van den Bergh & Tammann,
Cappellaro et al. (1993)
find
SNR =
SN century-1,
when scaling to external galaxies of similar
type. The sample is obtained from surveys carried out at the Asiago and
Sternberg Observatories. The authors provide an extensive discussion of
the uncertainties of this method, which can exceed 200% for some late type
galaxies. More recently, van den Bergh & McClure (1994)
find SNR = (2.4-2.7) h752 events per century.
This
estimate is based on re-evaluation of the extra-galactic SN rates obtained
from Evans' 1980-1988 observations. This method depends on a somewhat
uncertain type of the Galaxy and the value of its blue-band luminosity,
while the uncertainty due to the Hubble constant is now very small. Given
the error analysis in the paper, the rate is uncertain by at least 30%.
van den Bergh & McClure (1994) in studying the supernova rates of local spiral galaxies of types Sab-Sd of Evans' observations estimated that 80%-90% of supernova in that galaxies are of types Ibc and II. Recently Cappellaro (2003) combining five SN searches to include 137 SNe in 9346 galaxies estimates the SN type ratios in the Galaxy to be Ia:Ib/c:II = 0.22:0.11:0.67. From these observations, one infers a ratio of core-collapse to thermonuclear supernova of R = (II+Ibc)/Ia = 3.5. However, note that the Galactic historical record in the last millennium shown in Table B.1 contains only two type Ia SNR out of six SNRs. An often used alternative distribution over types is Ia:Ib/c:II = 0.1:0.15:0.75 (Hatano et al. 1997; Dawson & Johnson 1994; Hartmann et al. 1993; Tammann et al. 1994), which implies a three times higher cc-SN fraction. In this work, we adopt this set of parameters, and note that the small 44Ti yield of type Ia renders our results insensitive to this ratio.
Over the last millennium, the historic record contains six events (see Appendix B.4), which implies a rather low rate at face value. However Galactic extinction at visible wavelengths and embedded supernovae will lead to large occultation bias, and with extinction models plus Monte Carlo simulations this historic record can be assessed to approximately agree with extragalactic rate determinations (see Sect. 3 and Appendix A.2). An often cited rate of galactic cc-SN of three per century is consistent both with astronomical arguments (van den Bergh & McClure 1990) and with the rate inferred by Timmes et al. (1995) from their chemical evolution model that produces solar abundances successfully. We adopt a supernova recurrence rate of 30 years as a baseline for our 44Ti sky expectations.
![]() |
Figure 2:
The expected Ti sky of 10 simulated galaxies of model A
where the supernova recurrence time is taken to be 30 years and
the supernovae ratio of Ia:Ib:II = 0.10:0.15:0.75.
Simulating a 105 galaxy sky,
a gamma-ray detector with a detection limit of
|
| Open with DEXTER | |
The 1.157 MeV
-ray line following
44Ti decay has been detected in the 340-year old Galactic supernova remnant
Cas A (Iyudin et al. 1994; Vink et al. 2001).
COMPTEL's survey (Dupraz et al. 1997; Iyudin et al. 1999)
has resulted in other candidate sources, such as the so-called
Vela junior SNR (Iyudin et al. 1998).
INTEGRAL's inner-Galaxy survey has been studied with IBIS Imager data,
which did not reveal a new source in this region
(Renaud et al. 2004).
The difficulties of MeV observations
have thus not led to convincing new 44Ti rich
supernova remnants, especially in the inner Galaxy region
(l = 0
30
)
where observations are deepest.
Yet, Cas A seems an established 44Ti detection in COMPTEL
(Schönfelder et al. 2000)
and Beppo-Sax (Vink et al. 2001)
and INTEGRAL/IBIS (Vink 2005) measurements,
while OSSE (The et al. 1996)
and RXTE (Rothschild & Lingenfelter 2003) measurements of Cas A
were not sufficiently sensitive.
There exist no well-understood supernova remnants other than Cas A
where the 44Ti production issue can be tested.
It is apparently the only supernova whose
yield, age, and nearness makes
44Ti visible in gammas.
Naturally we ask ourselves if Cas A is
a typical supernova or an anomalous case of a high-44Ti yield
supernova?
Current supernova models predict an amount of 44Ti which is of the same order than what these observations suggest, though generally slightly less. Can we take this as a satisfactory confirmation of our understanding of core collapse supernova 44Ti production? These two identified core collapse events and their association with 44Ti production appear to be in line with models which attribute 44Ti production to the more frequent standard core collapse events but not to standard thermonuclear supernovae. Is this correct?
If true, the location of 44Ti sources should match the locations
of young massive stars which have rather short lifetimes.
There is substantial evidence that massive star formation occurs in spiral
arms and predominantly in the inner Galaxy
(Kennicutt 1998; Elmegreen et al. 2003; Scoville et al. 2001).
Massive stars can be observed directly in the infrared
(e.g. Maeder & Conti 1994),
though extinction corrections are large in regions of dense clouds.
Possibly an even better (though more indirect) massive-star census
can be derived
from 26Al decay
-rays
(Prantzos & Diehl 1996; Knödlseder 2000; Diehl et al. 2005; Diehl et al. 1995).
26Al is understood to originate
predominantly from massive stars and
-rays
easily penetrate even dark clouds in star forming regions.
So, do we see the 44Ti sources in regions where we expect them to occur?
Or do other factors which are not yet understood conspire to make 44Ti
ejection a phenomenon of core collapse events occurring in special
regions and environments?
If we want to estimate how the 44Ti sky should appear in a gamma-ray survey, we need to follow a statistical approach, due to the rare occurrence of supernovae. We therefore apply a Monte Carlo approach of sampling plausible probability distributions for supernova rates, their 44Ti yields, and their Galactic distribution, thus calculating a large statistical sample of possible appearances of the 44Ti sky.
![]() |
Figure 3:
Cumulative 44Ti gamma-ray line flux distribution of
supernovae with
|
| Open with DEXTER | |
![]() |
Figure 4:
The longitude distribution of supernovae
for four 44Ti gamma-ray line flux bandwidths
in Model A of
Appendix A.2
with supernovae type ratio of Ia:Ib:II = 0.1:0.15:0.75.
The equal-bin width is 20 degrees in longitude.
Only the
|
| Open with DEXTER | |
It is immediately evident from Figs. 2
and 3 that expectations based on
such seemingly plausible assumptions look very different than
the observed 44Ti sky:
Fig. 2
shows
4-7 observable 44Ti sources in an area of the Galaxy that contained
none (see Fig. 1)
above the observable flux limit used for comparison. The brightest
source in that realization (large-filled circles)
has
10-4 cm-2 s-1,
which would have been seen as a
10
source by COMPTEL,
and would have been detected already in
INTEGRAL's inner-Galaxy survey (Vink 2004).
The majority of our calculated samples lead to this same type of conflict
(see Fig. 3).
The probability of having no sources within the
central galaxy is small for current surveys, as illustrated in
Fig. 4 (for model A):
for a survey down to
10-5 cm-2 s-1,
12% of supernovae appear within longitudes ![]()
,
whereas only 72% of supernovae is within that volume.
An interesting feature, however, is that the longitude
distribution for
cm-2 s-1
is dominated by sources from type Ia (the bulge) and farther away SNe,
while the distribution for
cm-2 s-1
is dominated by sources from type Ib and type II (disk) and nearby SNe.
This feature also can be seen in Fig. 3,
where around
cm-2 s-1the distribution changes its slope.
It is clear that something is wrong with at least one of these assumptions:
The 44Ti gamma-ray sky can be studied in lines from
the primary decay to 44Sc at 67.9 and 78.4 keV and
from the following decay to 44Ca at 1.157 MeV.
In this latter line, the COMPTEL imaging telescope had
reported the pioneering detection of 44Ti from Cas A
(Iyudin et al. 1994),
clearly showing a point source image at 1.157 MeV as well as the line in a
spectrum from this source.
This detection
had initially created some controversy because other gamma-ray
instruments apparently
did not see it (Rothschild et al. 1998; The et al. 1996).
We now believe that this is due to the high initially-reported
COMPTEL gamma-ray flux value, reduced later
with better statistical accuracy of the measurement
(Dupraz et al. 1997; Iyudin et al. 1999). The independent
detections with BeppoSax (Vink et al. 2001) and with
INTEGRAL/IBIS (Vink 2005)
in both lower-energy lines (Beppo-SAX) and in the 67.9 keV line (IBIS)
now consolidate the 44Ti detection from Cas A,
but also suggest that indeed the 44Ti gamma-ray flux of Cas A
is in a range between 0.8 and
ph cm-2 s-1; an "average'' of
(
)
10-5 ph cm-2 s-1 has been derived
(Vink 2005).
An upper limit from INTEGRAL/SPI reported from first studies
is consistent with this flux value, and may suggest that the 44Ti line
is broader than 1000 km s-1 (Vink 2005).
COMPTEL's sky survey allowed for mapping of the plane of the Galaxy in
the 44Ti line (Dupraz et al. 1996; Iyudin et al. 1999).
Secondary features in these COMPTEL 44Ti maps kept the discussion about
statistical significances and systematic uncertainties alive
(see Schönfelder et al. 2000, for a comparison of Cas A to RX J0852,
a promising second source candidate, Iyudin et al. 1998).
The COMPTEL point source detection algorithm
(de Boer et al. 1992) has been
tested with simulations
over the full sky: likelihood statistics has been verified to reproduce the
expected number of artificial sources for a full sky survey, as the noise
level is approached.
The problem is that in the range of all the 44Ti gamma-ray lines,
all gamma-ray telescopes suffer from a large background
from local radioactivity induced by cosmic-ray
bombardment of the instruments
(Weidenspointner et al. 2002; Gehrels & Michelson 1999).
Determination of this background is crucial.
For an imaging instrument, this can be done rather well by interpolation
of imaging signatures from adjacent energies.
But furthermore, for COMPTEL the 1.157 MeV
line of 44Ti is not far above its lower energy threshold, and in fact
imaging selections
strongly affect the sensitivity of the instrument up to
1.5 MeV.
Nevertheless, imaging analysis in adjacent energy bands should all experience
similar problems, and therefore differences between images in the 44Ti band and
in neighboring energy bands can be attributed to 44Ti rather than
continuum sources
or instrumental artifacts, once they are confirmed to be point-like sources
(instrumental background lines would in general spread over data space and
hence lead to extended or large-scale artifacts in the image, hence impact
on the flux measurement rather than on point source detection). Detailed
comparisons of results for different energy bands, data subsets,
and selections
have led to the more cautious report about the Vela-region source
(Schönfelder et al. 2000),
so that still no convincing second 44Ti source clearly above
the noise level is claimed.
The INTEGRAL limits for 44Ti lines from the Vela region source
are now close to the
reported COMPTEL flux value for this candidate source
(Renaud 2004; von Kienlin et al. 2004)
and we therefore consider only one single 44Ti source (Cas A) as being
detected down to
flux levels of 10-5 ph cm-2 s-1.
For the low-energy lines measured by other instruments, in addition to the instrumental background the underlying continuum (see The et al. 1999 for Cas A) presents a major source of uncertainty (see Vink & Laming 2003; Vink 2005; Vink et al. 2001). This becomes even more of a problem for recombination line features from 44Sc at 4.1 keV, which have been studied with ASCA (Iyudin et al. 2005; Tsunemi et al. 2000), yet without clear detections (though tantalizing hints have been discussed for the Vela-region source).
For our quantitative comparisons of the 44Ti supernova rate with the historical
record of supernovae in the last millennium
(see Appendix B.2),
we make use of the COMPTEL survey.
We avoid the regions where reduced exposure might eventually
lead to increased artifact levels, and concentrate on the inner Galaxy where
exposure for the COMPTEL sky survey is deep and homogeneous. We also avoid
using data after the second re-boost of the satellite, whereafter
the activation
level of 22Na had increased substantially
(Weidenspointner et al. 2002).
This leaves us with a dataset covering the sky range of
,
using
7 years of the 9-year sky survey. In these gamma-ray data, the 44Ti source
sensitivity should be rather well-behaved and useful for our study.
Note that the first inner-Galaxy survey from INTEGRAL
(longitudes of
20
around the GC)
(Renaud 2004)
is consistent with our dataset in that also there no source is found
to flux levels of 10-5 ph cm-2 s-1 (Renaud 2005).
Many determinations of the galactic star formation rate (SFR) and
supernova rate (SNR) have been made in past decades (see Diehl et al. 2005
for a compilation of estimates, and Stahler & Palla 2005 on general
astrophysical aspects of star formation). In this work we are concerned
with the 44Ti from supernovae, so we need the formation rate of
massive stars (above, say, 10
). The conversion between SNR and
SFR is a sensitive function of the Initial Mass Function (IMF),
and values given in the literature thus vary depending on the author's
chosen IMF. For a generic transformation equation, we use the
calibration from McKee & Williams (1997): SFR = 196 SNR, where the SFR
is measured in
yr-1 and the SNR in events per year. A
star formation rate of 4
yr-1 thus corresponds to a
supernova rate of two events per century. These rates only include core
collapse supernovae (type II and Ibc), but not SNIa.
Generally these supernova rates are averages over
time scales much longer than 44Ti decay.
Many papers discuss the star formation (rate) history (SFH) in relative
terms, or the star formation rate surface density
(
yr-1 kpc-2)
in the solar neighborhood and its radial dependence. None of
these papers is useful (for our purpose) without an absolute calibration,
based on a model of the galactic distribution of star formation.
Generically, the SFR is obtained from a tracer that can be corrected for observational selection effects and is understood well enough so that possible evolutionary effects can be taken into account. One either deals with a class of residual objects, such as pulsars or supernova remnants, or with reprocessed light, such as free-free, H-alpha, or IR emission that follows from the ionization and heating of interstellar gas and its dust content in the vicinity of the hot and luminous stars. One must be careful to include time-dependent effects, as the afterglow of an instantaneous starburst behaves differently than the steady state output from a region with continuous star formation. Here, we are concerned with an average star formation rate.
To set the stage, let us collect SFR values from the literature.
Smith et al. (1978)
concluded
SFR = 5.3
yr-1,
while Talbot (1980) finds a very low
value SFR = 0.8
yr-1, and Guesten & Mezger (1982)
report a very high value of SFR = 13.0
yr-1. Later papers
appear to converge on a median value: Turner (1984)
finds SFR = 3.0
yr-1, and Mezger (1987)
finds 5.1
yr-1. Measurements in the past
decade confirm this moderate rate: McKee (1989)
derives SFR = 3.6
yr-1
from the analysis of thermal radio emission
(free-free) from HII regions around massive stars. This emission is
directly proportional to the production rate of ionizing photons, which in
turn is directly proportional to the SFR. He pointed out that this method
is very sensitive to the slope of the high-mass IMF. We also note that the
method depends on stellar model atmospheres in conjunction with models for
massive stars, which change with treatments of mass loss, rotation, and
convection. This paper also briefly discusses the use of the far-IR
luminosity, due to warm dust heated by the absorption of photons from
massive stars. The author uses the measured IR luminosity of the Galaxy of
(from Mezger 1987)
to derive SFR = 2.4
yr-1.
We must convert between star formation rate (SFR) and supernova rate (SNR) (see above).
McKee & Williams (1997)
promote the value SFR = 4.0
yr-1,
and based on the
Scalo's IMF (Scalo 1986) convert this rate into a total number
rate of 7.9 stars per year. They assume that all stars above 8
become
supernovae, corresponding to a supernova fraction of
.
The
mean stellar mass is
.
The corresponding cc-SN rate is 2 per
century. This value is also supported by a completely independent method,
based on the production of radioactive 26Al in cc-SNe, which can be
traced though its gamma-ray line at 1.809 MeV.
Timmes et al. (1997)
use this method and conclude
SFR = (
)
yr-1, utilizing the 26Al line flux derived from COMPTEL.
The steady-state mass of 26Al obtained in their work is in the
range 0.7-2.8
,
consistent with the value presented in the
recent study by Diehl et al. (2005). Based on the Salpeter IMF in the
range 0.1-40
and the 26Al yields
from Woosley & Weaver (1995)
[which do not include contributions from the Wolf-Rayet wind
phase] the authors derive the above quoted SFR and an associated
cc-supernova rate of
per century. They neglect
hydrostatically produced 26Al that is injected into the ISM in massive
star winds, which causes their SFR to be overestimated. The large uncertainty is
mostly due to the steady-state mass of 26Al inferred from the COMPTEL flux.
INTEGRAL data presented by Diehl et al. (2005) have significantly reduced
the error in this key quantity, and with wind yields included the latter
study finds SNR =
supernovae per century, which corresponds
to SFR =
yr-1, similar to the value
given in McKee & Williams (1997). This SFR is very similar to the one
obtained for M 51 (Calzetti et al. 2005), and thus places the
Galaxy in the group of quiescently star-forming galaxies.
The most recent paper addressing this issue is by Reed (2005),
who does not derive the SFR, but states that
the galactic supernova rate is estimated as probably not less than 1
nor more than 2 per century. Using the conversion factors from
McKee & Williams (1997),
one infers that the SFR is in the range 2-4
yr-1. Reed
uses a sample of a little over 400 O3-B2 dwarfs within 1.5 kpc of the Sun
to determine the birthrate of stars more massive than 10
.
The galaxy
wide rate is derived from this local measurement by extrapolation based on
models for the spatial distribution of stars, a model for galactic
extinction (to accomplish corrections for stellar magnitudes), and a model
of stellar life times. Reed emphasizes various sources of errors, such as
lacking spectral classifications of some bright OB stars, the (poorly
known) inhomogeneous spatial structure of extinction as well as stellar
density, and non-unique connection between mass and spectral type.
Finally, Reed also draws attention to the fact that one would have to
include B3 dwarfs as well,
if the lower mass limit for supernovae is 8
and not 10
(see Heger et al. (2003) for comments on this mass limit). The
OB-star catalog of the author was used to perform a modified
test
to obtain a present-day star count as a function of absolute V-band
magnitude. From the stellar life times, and the assumption of steady
state, the local birthrate follows. A double exponential model (in
galactocentric radius and scale height above the plane) of the spatial
distribution of these stars (which includes an inner hole of radius
R =4.25 kpc) ultimately leads to a total birthrate of 1.14 OB stars per
century. Variations in the size of the hole change this number
significantly, which leads the author to finally claim a rate of 1-2 supernovae per century.
In the context of our interpretation of the 44Ti observations, we
would argue that
Supernova rates between one and three cc-SNe per century are
consistent with the large set of studies reviewed above. To solve the
44Ti Sky conflict with a choice of the SNR (or SFR), an extremely low
rate outside this range would of course explain the absence of 44Ti gamma-ray
line sources in the sky. However, chemical evolution arguments for
44Ca would then require correspondingly higher 44Ti yields which
are not supported by explosive nucleosynthesis studies (as discussed
below) and which in any case would lead to higher fluxes from supernova
remnants and thus again to a source count that exceeds the observed count
of
1. The observational constraints are on the product of rate and
yield. The natural solution to the problem may
be the very rare events with extremely high yields, which is discussed below.
In that case it is of course totally unclear what to use for the spatial
distribution of these events, and "unusual'' positions of a gamma-ray line
source on the sky (such as that of Cas A) would be hard to interpret.
But perhaps we have overlooked another option. We know that the galactic star formation process is strongly correlated in space and time (Elmegreen et al. 2003). Could it be that the Galaxy just had a brief hiatus in its SFR? It would not take too much of a pause (say a few centuries) to explain the absence of bright 44Ti sources if the past few centuries were very untypical with respect to the SFR (or SNR). This possibility is included in our Monte Carlo simulations, which show that this is not a likely solution when one simply considers Poisson fluctuations. This solution is thus not acceptable, unless one can point out a physical cause of the hiatus in the recent SFR.
Likewise, we may wonder about the possibility of very large
spatial fluctuations. Could it be that the recent Galaxy exhibits an
average star formation, rate-wise, but a lopsided distribution in space.
If the opposite side of the Galaxy currently forms stars, and regions in
the solar sector are relatively inactive (
),
we expect to detect fewer
gamma-ray line sources (because of their somewhat larger average
distances). But at the same time the supernovae would also suffer from
enhanced extinction, and matching the historic SN record would require a
much higher rate. We have simulated the effects of a lopsided profile
with a von Mises Distribution, the analog of a Gaussian distribution for
circular data (Mardia 1975; Fisher 1996).
This function allows us to change from an
axis-symmetric galactic distribution to a one-parameter distribution
(measured by a parameter k, where k=0 corresponds to the
uniform circular distribution) in a chosen direction
which we choose it to be the longitude
direction.
We re-simulated the
105 Galaxies sample as described in Sect. 2.5,
and find that the
detection probabilities
(stated in the caption of Fig. 2) change to
0.0042, 0.023, and 0.062 for parameter k=0.5 and
0.0068, 0.035, and 0.087 for parameter k=1.0, respectively.
The probability curves for 44Ti
-line source detection
(see Fig. B.4) are shifted towards higher rates, as expected, but the
overall likelihood of these models decreases. The constraint from the
historic record demands new rates that are even larger, as the
extinction correction affects the results more strongly than the D-2 distance
effect for the flux. The combination of these two constraints make
lopsided models less acceptable than axis-symmetric ones.
A lopsided model would also make Cas A even more special, regarding its
unexpected location on the sky. To alleviate this problem we simulated
lopsided star-forming galaxies in which the solar sector was the more
active.
The detection probabilities of 0, 1, and 2 44Ti sources of
this model are
0.0005, 0.003, and 0.012 for parameter k=1.0, respectively.
This shows that the number of
the most probable 44Ti
-line source detection
in the Galaxy is >2 detections
and the model is less probable than the model used for
Fig. 2 for consistency with the observed 44Ti sky.
Is it reasonable at all to consider one-sided star forming galaxies? That major merger events should be able to tidally induce a lopsided starburst activity is perhaps obvious, but the Galaxy is not undergoing such an event. However, Rudnick et al. (2000) have shown that even minor mergers (Ibata et al. 1995) generically termed "weak interactions'' may lead to a boost in the star formation rate correlated with their lopsidedness. Another mechanism for the creation of non-symmetric star formation patterns is the interaction between odd numbers of spiral density waves, as it may be at work in M 51 (Henry et al. 2003). We do not advocate such an asymmetry for our Galaxy, but just wanted to consider this real possibility as one of the potential fixes for the 44Ti sky problem. Our simulations indicate that even such an extreme solution does not work, as the various combined constraints operate against each other. While a lopsided Galaxy helps on the gamma-ray source count side, the historic record is harder to explain if recent supernovae are located preferentially on the far-side.
Analyzing the consistency of the supernova rates derived from the
Galactic historical record and the COMPTEL's gamma-ray map
(Appendix B.4),
the consistency would improve if the SN rate from historical record
is smaller. This could be realized if the true Galactic extinction map is
lower than the visual extinction map we used here.
Recently there are two published Galactic extinction maps that are
useful for the type of study of this paper.
The optical reddening model of Mendez & van Altena (1998),
which is based on Galactic dust distribution model,
makes use of the same
optical sky surveys implemented by Hakkila et al. (1997)
in addition to some other restricted surveys. However this extinction map is
reliable only for solar neighborhood within 6 kpc.
Another large scale three-dimensional model of Galactic extinction
based on the Galactic dust distribution of Drimmel et al. (2003)
has been shown to give a good agreement with the empirical extinction
derived from NIR color-magnitude diagrams within 0.05 mag and
furthermore it is reliable for a distance up to
8 kpc.
This extinction model gives a larger magnitude of
extinction than that of Hakkila et al. (1997) for
longitude
![]()
and
for most pointing directions from the Sun
for distance larger than 6 kpc. For distance less than 5 kpc,
the extinction of this map is smaller than that of
Hakkila et al. (1997) which could give a better agreement
between the SN rates of the historical record and
of the COMPTEL's gamma-ray map.
Although the lifetime of 44Ti measured in laboratories
had exhibited a
large uncertainty since its first measurement in 1965, a compilation of
five recent experiments
performed after 1998 gives an averaged lifetime
of
yr,
where the quoted error is of statistical
and of one standard deviation
(see, e.g., Fig. 5 of Hashimoto et al. 2001
and also Görres et al. 1998).
Apparently, this small uncertainty in the measured 44Ti lifetime does
not affect the discrepancy discussed here.
It is noted that the above-mentioned lifetime measured in laboratories is for neutral atoms. Since 44Ti is a pure orbital-electron-capture decay isotope, its lifetime depends on the electronic environment in the evolutional course of a supernova remnant. For example, a fully-ionized 44Ti is stable, and the lifetime of 44Ti in the Hydrogen-like ionization state becomes longer by a factor of 2.25 than that of the neutral 44Ti (see Motizuki & Kumagai 2004). Let us briefly consider the effect of 44Ti ionization on our problem.
In young supernova remnants, the reverse shock propagates inward through the ejecta and the resulting increase in temperature and density may lead to highly ionized ejecta material through thermal collisions with free electrons. A high-degree of ionization may then result in a longer lifetime of 44Ti, which would significantly alter the inferred 44Ti mass. In fact, H-like and He-like Fe ions have been observed in Cas A (see, e.g., Hwang et al. 2004). Because the electron binding energies of Ti are smaller than those of Fe, it is easier to ionize Ti than Fe. Accordingly, 44Ti atoms in Cas A may be expected to be in such high ionization states at least in part if they are accompanied by the highly ionized Fe (this is expected because 44Ti is synthesized at the same location as where 56Ni is also produced in the innermost region of a supernova).
Since the present-day radioactivity was entirely affected by the history
of various ionization stages and their duration time for which the 44Ti
has experienced through the evolution, detailed discussion requires
numerical simulations as was done by
Mochizuki et al. (1999) and Mochizuki (2001).
However, we can get a rough idea of the ionization effect on the
radioactivity by using the result of simple linear analysis, i.e.,
Eq. (7) of Motizuki & Kumagai (2004):
Note that
is always positive because the ionization always
increases its lifetime. As was pointed out by the above authors,
the sign of
is then determined by that of
the term in the parenthesis in the right-hand side of
Eq. (1).
This means that the flux is enhanced by the ionization
when a SNR is older than the 44Ti lifetime, and that
the flux is reduced when it is younger.
Our concern here is whether the effect of ionization on the lifetime
of 44Ti in SNRs can reduce the disagreement between the
observed 44Ti Galactic map and the model's map or not.
From the above arguments, we can easily understand that the
discrepancy may be diminished if the
-line fluxes in
Fig. 2 could be smaller
which may be realized if most of
the
-ray detected SNRs in Fig. 2
are younger than the 44Ti lifetime.
To get a rough idea, we performed a calculation
in which all parameters are the same as employed for
Fig. 2 except
1) the fluxes are multiplied by a factor 0.5 for SNRs with ages less
than 100 y,
and 2) the fluxes are multiplied by a factor 2 for SNRs with ages between 200
and 400 y. The selection of 200-400 years old SNRs as enhanced
targets here is because the effect of the ionization due to the reverse
shock is
considered to be distinguished for these ages and the further inclusion of
the enhanced-flux effect on SNRs older than 400 y only makes the discrepancy
larger (see Mochizuki et al. 1999 for details).
Simulating a 105 galaxy sky, we found that a
-ray detector with
a detection limit of
ph cm-2 s-1would have a probability of detecting 0, 1, 2 44Ti sources of 0.0012, 0.008,
and 0.026, respectively.
Therefore, from this simple analysis it is suggested that the disagreement
cannot be compensated by the ionization effect; in effect it becomes
worse in our simple calculations above than
the reference calculations of Fig. 2.
A more precise estimate requires the knowledge of the temperature and the density evolution of a supernova remnant, and the distribution of 44Ti in it. However, any detailed calculations taking into account the retardation of 44Ti decay due to ionization will not alter the situation better: in any case, the older SNRs whose fluxes may be enhanced always dominate in number the younger SNRs whose fluxes may be decreased.
Estimates of yields of 44Ti from nucleosynthesis in supernovae depend
crucially on key nuclear reaction rates, and uncertainties in these rates limit
our ability to constrain the supernova rate.
The et al. (1998)
studied the sensitivity of 44Ti yields in alpha-rich freezeouts to
uncertainties in nuclear reaction rates. They did this by computing the
alpha-rich freezeout with reference values for the reaction rates and then
comparing these results with ones from calculations with individual
rates varied
upwards and downwards by a factor of 100 from their reference values.
The results were that the production of 44Ti
was most sensitive to the rates for the following reactions:
44Ti
V,
C,
44Ti
Cr,
and 45V
Cr for matter with equal numbers of neutrons and
protons (
). For neutron excess
greater than zero,
the importance of the reaction 45V
Cr drops, but other
reactions become more important. In particular, these reactions are
12C
O, 40Ca
Ti,
27Al
P, and 30Si
S.
For our purposes, the relevant question is how much the 44Ti may vary
from current supernova models given these uncertainties. Motivated by the
work of The et al. (1998), Sonzogni et al. (2000) measured the
cross section for the 44Ti
V reaction at the
astrophysically relevant energies. They found that the experimental cross
section for this reaction was a factor of two larger than in the rate
compilation of Thielemann et al. (1987) used
in the The et al. (1998)
calculations. From this result, Sonzogni et al. (2000) inferred a 25% reduction in the amount of 44Ti produced in alpha-rich freezeouts
in supernovae. Other of the key reactions found by The et al. (1998)
had similar sensitivities of 44Ti yield to reaction rates; therefore,
if other experimental reaction rates are also a factor of
2 different
from the theoretical calculations, we can expect similar
effects
on the 44Ti yield. From these results, we might thus conservatively
expect the 44Ti yield to be uncertain by less than a factor of
2
due to reaction rate uncertainties.
Such a conclusion is supported by the study of the reaction rate sensitivity of
nucleosynthesis yields in core-collapse supernovae by
Hoffman et al. (1999).
These authors compared the yields from core-collapse supernova models using
two different reaction rate libraries. For the 15
stellar model
studied, the two calculations gave 44Ti yields that agreed to within 20%, in spite of the fact that many individual nuclear reaction rates differed
by a factor of two or more between the two rate compilations.
On the other hand, Nassar et al. (2005) have recently measured the
40Ca(
Ti reaction cross section in the energy range
for nucleosynthesis in supernovae. In that energy range, the authors find
that the reaction rate is 5-10 times larger than the previously
used theoretical rate calculated from a statistical model
(Rauscher et al. 2000). This large difference between
the experimental rate and the theoretical rate may be due to the fact that the
low level density in the 44Ti compound nucleus limits the applicability
of the statistical model for theoretical predictions for the rate of this
reaction. In any event, the larger rate increases the yield
of 44Ti by a factor of
in the stellar models
Nassar et al. (2005) explored. Such a large increase in the
40Ca
Ti reaction rate may allow normal core-collapse
supernovae to account for the solar system's supply of 44Ca; however,
this result would worsen the discrepancy between the observed
Galactic 44Ti gamma-ray flux and our predictions.
In core-collapse supernovae, 44Ti production occurs by the alpha-rich freezeout near the mass cut. The location of the mass cut in the star will then certainly affect the 44Ti yield. Also important is the question of whether the simple-minded notion of a mass cut at a single radial shell in the star even makes sense in more realistic models that account for large-scale fluid motions behind the stalled supernova shock prior to the explosion and for stellar rotation. These more realistic models suggest that the material ejected from near the mass cut will in fact be a mixture of parcels that arose from both inside and outside the mass cut. We can certainly expect variations in the entropies of those parcels, which, in turn will have attendant variations in the 44Ti yield (e.g., Pruet et al. 2005).
For our purposes, the important issue to consider is how much variation can
we expect in the 44Ti yield from differences in the mass cut and
multi-dimensional effects. One-dimensional models suggest that typically
half or more
of the 44Ti produced during the explosion might fall back on the remnant
(e.g, Nassar et al. 2005). Similar results are possible for
the multi-dimensional models. It is therefore quite conceivable that
yields of 44Ti from supernovae of the same mass
might vary by factors of
2 simply due to variations in the location
of the mass cut or multi-dimensional effects. Of course, if the supernova
forms a black hole with mass greater than
2 solar masses, it will
swallow up its innermost material and, thus, most or all of the 44Ti (and
56Ni) it produced. Such supernovae would be dim in both visible and
gamma radiation. Perhaps the Galactic 44Ti map is indicating that
supernovae over the last few hundred years have been predominantly of
this type.
Although often taken for granted, homogeneity among supernovae of a type
remains an open issue:
for thermonuclear supernovae, light curves have been found to be
fairly similar (Branch 1998).
Their successful empirical relative adjustment
through a light-curve-decline parameter apparently makes them
"standard candles'' over the full range of cosmic evolution
(this is the basis for the determination of cosmic expansion history,
see e.g. Dahlén et al. 2004).
The homogeneity of the r-process elemental abundance pattern
in low-metallicity stars suggests that the r-process, which is commonly
attributed to core collapse supernovae,
also presents a fairly well-regulated
nucleosynthesis environment (e.g. Thielemann et al. 2002).
On the other hand, the 56Ni masses ejected in supernovae
appear to scatter, within
30% for SNIa (Benetti et al. 2005),
and for
core collapse events over a wide range from 0.01 to 1
(Woosley et al. 1995; Woosley & Weaver 1995; Thielemann et al. 1996),
suggesting
more variability in the core collapse nucleosynthesis than in
thermonuclear explosions
(Nomoto et al. 1997; Thielemann et al. 2004). Still,
for supernovae of type Ia alternative model types are also discussed that
would produce quite distinctly different nucleosynthesis products than
central carbon ignition in Chandrasekhar-mass white dwarfs
(Nomoto 1982; Livne & Arnett 1995; Woosley & Weaver 1994).
In summary: supernovae of both types are quite homogeneous in some of their characteristics, but anomalies suggest a deeper study of physical regulations and their observational impact.
Nagataki et al. (1997)
in their explosive nucleosynthesis
calculations of 2-D axisymmetric type II supernova found that
materials engulfed by energetic shock waves along polar
directions undergo higher temperatures (or higher entropy per baryon,
Fryer & Heger 2000)
to produce a higher amount of 44Ti
than in spherical explosions.
Recently, Maeda & Nomoto (2003) also studied hydrodynamics
and explosive nucleosynthesis in bipolar supernova/hypernova explosions.
Their bipolar models produce a large amount
(>10-4
)
of 44Ti
and at the same time eject a relatively small amount
(
0.1-0.2
)
of 56Ni.
These features of 2D supernova models
inspire Prantzos (2004) to suggest that
the "missing 44Ti'' problem (to be in concordance with SN1987A and Cas A
observations and also to account for the 44Ca solar abundance)
could be solved by avoiding the overproduction of 56Ni.
More systematic studies are therefore required under
variety of progenitor masses, explosion energies, metallicities,
and other physical variables.
As this 2D effect could elude the discrepancy between the 44Ti production in
spherical supernova models and the amount
observed from Cas A SNR in gamma-line fluxes
and the amount deduced from 44Ca in solar abundance,
the axisymmetric explosion also seems to be the natural consequences
of rotation and magnetic field effects during pre-supernova phase
(Yamada & Sato 1994; Müller & Hillebrandt 1981)
and the neutrino-driven convection (Burrows et al. 1995)
for the core-collapse supernovae.
Furthermore, evidence to support the axisymmetric explosion
have been inferred from the measurements of
pulsar velocities (Hobbs et al. 2004; Burrows & Hayes 1996)
and from the jet features observed in radio and X-ray images from
several supernova remnants (Gaensler et al. 1998).
With various degrees of Rayleigh-Taylor instabilities
that may develop in core-collapse supernova
(either in 2-D or 3-D simulations),
we expect there would be
a wide distribution of 44Ti production in supernova events
as inferred indirectly by the pulsar velocity distribution.
Thereby the task is to find 44Ti distribution production
with supernovae synthesizing higher than typical amount of 44Ti produced in
a spherical model
(to explain the amount of 44Ca in solar abundance and Cas A SNR),
but also produces small amount of 44Ti for the most-recent supernova so their
gamma-line emissions are too weak to be detected.
For this, we have to wait until the explosive 3-D nucleosynthesis can
be performed within reasonable time.
The apparent deficit of 44Ti remnants from typical supernovae as the main
source of 44Ca
is explained if typical supernovae are not the main source. Some rare
type of event with a proportionately higher 44Ti yield could be the major
source
and not leave detectable remnants today
(e.g., Woosley & Pinto 1988). For example, these could be
He-triggered sub-Chandrasekhar-mass
thermonuclear supernovae (Woosley & Weaver 1994).
If their
recurrence time is several times the 44Ti lifetime, the Poisson
probability of having
none detectable now can be large. Woosley & Weaver (1994) find some
models with up to one hundred times higher 44Ti yields than the typical
supernova values discussed above. These need only occur now every one to
two thousand years to provide the necessary 44Ca synthesis. Such a
scenario, while potentially invisible to gamma-ray astronomy, would
imply inhomogeneities among the relative abundances of 44Ca and other
isotopes
(see Sect. D.3). A galactic survey at 6.9 keV could test this
scenario (Leising 2001). Another
-rich freezeout nucleus, 59Cu, decays to 59Ni
whose half-life is 75 000 years.
The nearest remnants of these rare objects from the past 105 years
could be easily detectable in the subsequent cobalt K
X-rays.
Mainstream SiC grains, however, argue against rare producers of large amounts of 44Ti being responsible for most of Galactic 44Ca, as the 44Ca/40Ca ratio in mainstream SiC grains does not vary much from grain to grain; here sample size is much larger than for X grains, so a more representative sampling may be assumed (see Appendix D).
We perform a simple simulation to test the viability of the rare-event scenario.
In this model, we take the model that produces Fig. B.4
(where the amount of 44Ti in supernovae are as produced by
the supernova models explained in Sect. 2.5)
but modify the 10% of core-collapse supernovae to produce 20
the 44Ti of the supernova models.
Therefore on average the amount of 44Ti in this model is about a factor 2.7
of the model shown in Fig. B.4 to account for
the 44Ca solar abundance.
This model gives a better agreement with the observed 44Ti sky
than the model used to produce Fig. 2 where
all supernovae produce 3
the amount of 44Ti of supernovae
models.
As shown in the caption of Fig. 2,
the probability of this model detecting 0, 1, and 2 44Ti sources are 0.012, 0.053,
and 0.12, respectively.
This results show that the model is more probable than the model
of Fig. 2 in explaining why COMPTEL and
INTEGRAL only detect one 44Ti source (less than expected).
For comparison, the supernovae recurrence rates of
the peak of the probability curve of
the 1.157 MeV
-line fluxes
that are consistent
with the COMPTEL observed fluxes (see Appendix B.2
and the dotted curve in Fig. B.4)
for the model of Fig. B.4, this model, and
the model of Fig. 2
are 36 yr (Fig. B.4), 40 yr, and 58 yr, respectively.
This result is encouraging that a set of supernovae models with
a rare type supernova that produces
most of the solar 44Ca
gives a closer recurrence rate to the one implied by the
historical supernova record (
17 yr)
than the model with 3
amount of 44Ti of
the calculated supernova models.
Still we have no good explanation for
why some small number of supernovae are so rich in 44Ti.
The observed distribution of pointlike sources of 44Ti in our Galaxy is inconsistent (at a probability near 10-3) with the combined current understanding of 44Ti production, specifically
A future survey with gamma-ray line sensitivity of 10
would be expected
to detect
10 sources (Fig. 2),
and so could rule out 44Ca production by frequent supernovae
at confidence
.
Regardless of specific assumptions,
the Cas A supernova remnant as
the brightest 44Ti remnant in the galaxy is a priori very unlikely.
That the brightest SNR should be found in
the outer galaxy or that it is over 300 years old are each improbable.
It suggests that yields higher
than suggested by many current calculations are possible,
which, of course, makes the lack of other detectable
remnants even more puzzling.
Acknowledgements
Part of this work was supported by NASA Grant NAG5-6892, NAG5-13565, NAG5-10764 to Clemson University and DOE's Scientific Discovery through Advanced Computing Program (grant DE-FC02-01ER41189). Research by DDC was supported by NASA's Origin of Solar Systems Program.
In generating supernova events of our Monte Carlo simulations,
we adopt the procedure shown by
Higdon & Fowler (1987); Mahoney et al. (1992); Hartmann et al. (1993).
A random number between 0 and 1000 is uniformly generated to represent
a supernova age between zero and 1000 y (
)
where
yr
(Ahmad et al. 1998; Görres et al. 1998; Norman et al. 1997)
is the mean life of 44Ti.
This range is large enough that a supernova age older than 1000 y does not
contribute to the Galactic 44Ti flux.
Another random number is generated to choose the type of the supernova event. Then, several random numbers are generated to give us the location of the supernova according to its spatial distribution. A detail procedure in generating the locations of supernova from a disk and spheroid populations of type Ia events can be found in the paper of Higdon & Fowler (1987); Mahoney et al. (1992). The distance of the supernova location to the Sun can be calculated easily.
A random number is generated from a Gaussian distribution to give us
the peak bolometric magnitude of the supernova following the distribution
given in Sect. A.2.
The apparent magnitude then can be calculated
knowing the location, the distance, extinction magnitude (from
Hakkilla et al.'s empirical model),
and the peak bolometric magnitude of the supernova.
We find in model A (Sect. A.2)
the fraction of SNe in the last millennium
brighter than
apparent magnitude 0 is
11%
(see Fig. B.3).
The amount of 44Ti of the supernova is given by a uniform distribution
of 44Ti according to its type as described in Sect. 2.5,
however note that the analysis in this appendix
does not use the multiplying factor of 3 that is used
in 2.5.
,
the 44Ti gamma-line flux at the Sun location,
then can be determined knowing
the location, the distance, the age, and the amount of 44Ti of
the supernova:
![]() |
Figure A.1: Same as Fig. 4 but for models B (left) and C (right). |
We generate 1 million supernovae according to the above prescription and
construct galaxies with numbers of supernovae between 1 and 300.
For each galaxy with a certain
number of supernovae,
the 44Ti gamma-line flux distribution
and the SN apparent magnitude distributed M(m,n) can be extracted.
For a galaxy with SN recurrence time of
or
average supernova rate,
/
(we only simulate
supernova events in the last millennium as described above),
the 44Ti gamma-line flux distribution,
can be obtained from
=
.
Supernova events as the source of Galactic 44Ti can either be type Ia, Ib/c, or II SNe. For this study, we choose a generally accepted (though uncertain) value of the type ratio, Ia:Ib/c:II = 0.1:0.15:0.75 (Hatano et al. 1997; Dawson & Johnson 1994). Yoshii et al. (1996) and Tsujimoto et al. (1995) using their chemical evolution model find that the ratio of the total number of type Ia to type II SNe of 0.12 gives a good agreement with the observed solar abundance. This is consistent with the observed Ia frequency which is as low as 10% of the total SNe occurrence (van den Bergh & Tammann 1991). Monte Carlo representations of type Ia SNe are generated using a nova distribution template that traces the blue light distribution in M 31 (Higdon & Fowler 1987). These populations form an axisymmetric disc and a spherically symmetric bulge. The spheroid density distribution follows:
Supernovae of types Ib & II are associated with massive stars whose
birth places are exponentially distributed in height above the plane
with a scale length of
100 pc.
Because the rate of core collapses is larger than the rate of
thermonuclear supernovae, we study several type II distributions to ensure
that our results do not depend significantly on this choice.
We consider three cases:
In order to produce a consistent picture of the recent Galactic supernova rate with the best known 44Ti supernova yields, supernovae types and spatial distribution, and Galactic extinction model we utilize our Monte Carlo simulation method to compare two observables of the same phenomenon (Higdon & Fowler 1987; The et al. 1999; Mahoney et al. 1992; Hartmann et al. 1993). We use the COMPTEL gamma-ray maps and the six historical Galactic supernova record of the last millennium to constrain the range of Galactic supernova rates.
Similar to the above determination of 44Ti flux distribution from
a simulated set of supernova
events, other distribution such as the apparent magnitude distribution
of supernovae
for a galaxy with an average supernova rate
can be constructed
(Sect. B.3).
From this distribution we can determine the probability of optical
detection for a certain detection-limiting apparent magnitude,
such as magnitude 0, for example.
In this way, we can use the same underlying assumptions about
supernova characteristics,
and compare two different observables, i.e. 44Ti gamma-ray versus optical
detections of the supernovae at the adopted rates. Varying the rates then
so that they conform to the observational constraints, we obtain a handle
on systematic differences in observed supernova rates through these two
observational windows.
For the 44Ti gamma-ray observations, we utilize the COMPTEL survey discussed above (Sects. 2.1 and 3.1). For the optical observations, we utilize the historical record summarized in Table B.1.
Table B.1: Recent galactic supernova record.
For comparison of the COMPTEL gamma-ray map with the results of Monte
Carlo simulations, due to our limited computational power, for the
purpose to reduce systematic effects from regions of low exposure, and
due to our limited ability to analyze the map, we perform two analysis.
In the flux dataspace (Sect. B.2) we
use the flux information exclusively, without using the observed location
of the gamma-ray source.
In the map dataspace analysis (Sect. B.1), we only use
the COMPTEL map of inner galaxy (
,
)
which does not include the locations of the detected 44Ti
-line
from Cas A and GRO J0852-4642.
In order to see how consistent the model with the Galactic supernova
record, we perform the historical record analysis below.
The historical supernova record covering the last millennium shows a total of only six Galactic SNe during that era (Table B.1). Of course, this small number is due to significant losses from extinction and incomplete monitoring of the sky, especially during the early centuries. In fitting this data, we count the fraction of galaxies that have six SNe brighter than magnitude 0. In this approach, we assume that historical SNe were detected if they were brighter than magnitude 0.
The peak absolute magnitudes of supernovae in the B-band are
approximated by Gaussian distributions.
For the mean values and the one standard deviation
we adopt for type Ia
MB = -19.4,
(Branch 1998),
for type Ib
MB = -18.2,
(Dawson & Johnson 1994), and
for type II
MB = -17.2,
(van den Bergh & Tammann 1991).
Their distribution is shown in Fig. B.1
Observed magnitudes of simulated SNe are obtained by convolving
absolute magnitudes through a Galactic extinction model of
(Hakkila et al. 1997).
In this extinction model, the total visual extinction
from the Sun's location to the Galactic Center is 11.64 mag
and the total visual extinction perpendicular to the Galactic plane at
Sun's location is
0.1 mag
(Fig. B.2).
The cumulative distribution of supernovae having blue peak apparent magnitude
brighter than mB in model A
is shown in Fig. B.3.
![]() |
Figure B.2: The Galactic visual extinction magnitude as a function of distance from the Sun to various direction according to empirical model of (Hakkila et al. 1997). |
![]() |
Figure B.3: The apparent magnitude of supernovae in model A according to empirical extinction model of Hakkila et al. (1997). |
The average fraction of the model that is consistent with six events brighter than magnitude 0 is shown in Figs. B.4, and B.5 as solid lines.
Our Galactic supernova record analysis leads to a most probable
Galactic supernova recurrence time of
17,
16, and
13 y
based on models A, B, and C, respectively.
This implies a larger rate than given by previous
investigations based on the historical record.
For example, Dawson & Johnson (1994) estimated
3 SNe per century as also obtained by
Tammann et al. (1994).
The rate is smaller than ours because
Dawson & Johnson (1994)
considered 7 observed SNe within the last 2000 yr and
assumed that the historical record
is 80% complete.
A higher SNe rate of 5 SNe per century was obtained by
Hatano et al. (1997)
who include a
population of "ultradim'' SNe in addition to 4 observed Galactic SNe
having V<0 and 80% completeness within the last millenium.
The map and flux methods of estimating supernova rates based on
-ray
data appear to be significantly different, but they are statistically
consistent with each other for a wide range of supernova rates.
The imaging analysis gives a smaller rate than the flux analysis,
because the data used in the map analysis do not include
the Cas A and GRO J0852-4642
-line detections.
However, the probability estimate from the flux analysis
is a somewhat coarser estimate because the size of independent FOVs
used in determining the probability is not known exactly.
Ignoring the spatial information begs the question as to why the
two brightest SN are in the outer Galaxy rather than in the inner
Galaxy where we expected them.
![]() |
Figure B.5: Same as Fig. B.4 but for models B ( left) and C ( right). |
In the flux dataspace analysis, where we ignore the expected spatial
distribution of 44Ti remnants and consider only the measured
flux distribution, we find a most probable supernova rate that is
more compatible with standard values (such as the rate inferred by
the historical record), even for standard 44Ti yields.
However, the COMPTEL map data indicate a lower SN rate
(
1 SN/36 yr) than that suggested by
the historical record (
1 SN/17 yr).
However model A which does not have a supernova event in
the inner 3 kpc radius has better agreement between the map
analysis and the historical record analysis.
This suggests that a model with less concentrated supernova
near the Galactic center than the model used here could give
a better agreement than we obtained here.
Also, an extinction model with smaller extinction
toward the Galactic center than Hakkilla et al.'s model
could give a better agreement than what we present here.
Based on chemical evolution studies,
Timmes et al. (1996)
estimated that only
1/3 of the solar 44Ca abundance is accounted for.
Models with a SN rate of
3 SNe per century
and standard 44Ti yields
fail to produce the solar 44Ca abundance.
This rate, when confronted with the gamma-ray data (dashed line in
Figs. B.4
and B.5)
is too large:
the COMPTEL gamma-ray data worsen an already serious
problem. Timmes et al. (1996)
suggest 3 possibilities:
![]() |
(C.1) |
The SiC X grains probably originated in core-collapse SNII. Within them the pure alpha-rich freezeout (Woosley et al. 1973, Sect. VII), which produces the bulk of 44Ti ejected from SNII, has production ratio near P(44Ti)/P(48Ti) = 1-2 (see Fig. 23 of The et al. 1998; Woosley et al. 1973, Sect. 3); so no X grain is pure alpha-rich freezeout material, although some of them must contain a significant fraction of their Ti from the alpha-rich freezeout. On the other hand, the production ratio during normal silicon burning is very much smaller, near P(44Ti)/P(48Ti) = 0.01 (Woosley et al. 1973, Fig. 19). Therefore, X grains having 44Ti/48Ti near 0.01 or less may contain no alpha-rich freezeout material at all, but instead condense from Si-burning ejecta rich in 28Si.
In their study of 99 SiC X grains from the Murchison meteorite, Hoppe et al. (2000) found that 25 contained enough Ti and Ca for isotopic analysis with the CAMECA IMS3f ion microprobe in Bern. Now that the new nano-SIMS ion microprobe is functional, we may hope for even more complete future surveys with its higher sensitivity. Of the 25 having enough Ti and Ca, 5 revealed large and easily resolved 44Ca excesses, corresponding to P(44Ti)/P(48Ti) > 0.01. Although the chemistry of condensation of SiC in supernovae has not been solved, initial studies (Deneault et al. 2003) of the location of C and Si suggest that no more than 20% of SiC X grains should be expected to contain P(44Ti)/P(48Ti) ratios in excess of those available during normal O and Si burning. That is, a majority of the X grains should contain no alpha-rich matter even if each supernova ejects such matter. If this be taken as so, the data suggest that the parent supernova population responsible for the 100s of X grains that have been studied did eject alpha-rich freezeout material in addition to its Si-burning matter. If ejection of alpha-rich freezeout matter were instead rare, we expect that the number of SiC grains having large P(44Ti)/P(48Ti) ratios would be significantly less than 20%. Without more detailed understanding of the origin of the X grains it seems plausible to take their evidence to suggest that all SNII eject alpha-rich-freezeout matter.
If the SiC X grains do originate in SNII, their frequent 44Ca excesses demonstrate that either the X grains all originated in a single nearly supernova that did eject 44Ti or originated in many presolar SNII that mostly ejected 44Ti (although not necessarily always). The properties of the "mainstream SiC grains'' enable us to argue against the possibility of a single supernova as origin of the X grains. The much more abundant mainstream grains, which are thought to have originated in presolar carbon stars, have been argued on the basis of their Si isotopes to have been the result of a great many C stars. Their Si isotopic compositions represent approximately the initial Si isotopic compositions from which the intermediate-mass stars formed, and their correlation between excess 29Si and 30Si is explained by galactic chemical evolution effects that have produced a wide range of Si isotopic compositions in a large number of C stars (Timmes & Clayton 1996; Clayton 2003). Because the mainstream grains comprise about 10-4 of all interstellar Si, much of which is quite old, and because the condensed SiC from the C-star phase is but a small fraction of all Si ejected from stars, it seems that the lifetime of SiC grains in the ISM is not short. If this be so, the lifetime of X SiC grains is also not short, suggesting a substantial number of contributing supernovae to the matter gathered into any cloud in the ISM.
For the question of 44Ti gamma-ray hotspots the issue arises whether the SiC X grains may instead have arisen from exploding SNIa. After all, the high expectation for seeing 44Ti supernova remnants shown in Fig. 1 came from the assumption that type II are the sources of 44Ti nucleosynthesis and therefore also of the solar 44Ca abundance. The absence of such sources could be explained if rare type I events produced much larger yields than are expected from type II. Do the supernova grains offer any guidance? Clayton et al. (1997b) showed that isotopically good fits to X grains might originate within He caps on exploding C,O white dwarfs. Huge production ratios, up to P(44Ti)/P(48Ti) = 100, occur in those He shell zones having peak T9>1 (see their Fig. 6). These are too great for existing observations of X grains, suggesting that SNIa are not their sources. However, Clayton et al. (1997b) showed that good fits to all isotopes require that the He caps undergo considerable post-explosive mixing prior to condensation of the X grains. Their Table 2 shows production ratios as small as 0.01 in an average of zones 1-8 (the coolest eight zones) and near 10 in an average over all sixteen zones. (The reader must note that much 48Ti production is listed by them under 48Cr, its radioactive progenitor.) The isotopic possibility must therefore be addressed that the 44Ti-rich X grains are from SNIa He caps rather than from SNII. The discovery of even a single X-type SiC grain containing an initial ratio 44Ti/48Ti = 5 or greater would demonstrate that the He-cap SNIa do exist and that they can condense SiC. This would amount to an existence proof for these rare 44Ti producers. But no such grain has yet been detected.
Clayton et al. (1997b) pointed out that if the SNIa are near the
Chandrasekhar mass, the He cap can be no more than 0.01
so that
less than 10-5
of 44Ti is ejected. Such events would be both
rare and dim in 44Ti lines. However, a much larger He cap is involved if
the white dwarf is sub-Chandrasekhar (larger) and the detonation begins
in a massive He cap. Large amounts of 44Ti are ejected from such models
(Woosley & Weaver 1994),
so that the rates of such events are limited by the
requirement that they not overproduce the galactic 44Ca
abundance. If this occurs, the rarity of these events in time could
account for their absence in the COMPTEL data (see also the
Discussion). The relevance of the X grains derives from the physical
unlikelihood of condensation of X grains in such He caps. Their
expansion is very fast, and the radiation environment intense, so that
even the formation of molecules seems unlikely until the density has
become too low for the growth of a 1-micrometer grain of SiC.
Clayton et al. (1997b)
note that even the possibility of grain condensation would
seem to require 3-D explosive modeling in order that some of the He cap
can remain at low velocity ("slow He''). This entire problem will
require more study before plausibility of SiC X grains from SNIa can be
admitted. We therefore conclude that the 44Ti-bearing X grains
have arisen in SNII.
We turn now to non-supernova Stardust whose 44Ca ratios reflect the initial compositions of their donor stars. The supernova X grains seem to support the assumptions that led to the conflict between the COMPTEL map (Fig. 1) and the expected hotspots (Fig. 2); namely, that X grains condensed within SNII, that the number of contributing SNII was large, and that most ejected alpha-rich freezeout matter. However, X grains do not demonstrate that the bulk ejecta of SNII contain sufficient mass of 44Ti to account for the natural 44Ca abundance. To test for the presence of rare large 44Ti producers (Woosley & Weaver 1994) responsible for making good the shortfall from SNII we turn to the mainstream SiC grains with the following original argument. Rare SNIa responsible for roughly 2/3 of galactic 44Ca plausibly result in Galactic inhomogeneities in the interstellar 44Ca/40Ca ratio that should be larger than those seen by astronomers for elemental-ratio variations attributed to inhomogeneous incorporation of SNII ejecta. It must be slower to homogenize the ISM if SNIa occurring every 3000 yr contribute 2/3 of 44Ca abundance than for homogenizing ISM from SNII occurring every 30 yr and making but 1/3 of the 44Ca abundance. ISM regions temporarily enriched in the rare SNIa ejecta may make stars having larger 44Ca/40Ca initial ratios. The mainstream SiC grains reflect the interstellar composition from which the carbon stars formed. That is, factor of two or more variations in 44Ca/40Ca ratio should be present in the initial compositions of stars.
It is this expectation that the mainstream grains may speak against. Hoppe et al. (2000) measured Ca isotopes in 28 mainstream SiC grains (see their Fig. 8) and found their 44Ca/40Ca ratios to be indistinguishable from solar despite large Si isotope variations in the same stars demonstrating that the grains come from different AGB C stars having distinct chemical evolution histories for their initial compositions (Timmes & Clayton 1996). Each mainstream grain was consistent with solar 44Ca/40Ca ratio and their average was enriched 3.8% in 44Ca, as expected for modest s-process enrichments of AGB atmospheres by the third dredge ups. Because of the small numbers of Ca atoms in mainstream grains, however, individual grain ratios were uncertain by at least 20%. Even so, 20% is a small inhomogeneity for rare events producing 2/3 of the bulk 44Ca. To improve this data base we call for high precision measurements of the 44Ca/40Ca ratio in a sample of mainstream grains with the new nanoSIMS ion microprobes. Such a survey could reveal more precisely any variations in initial 44Ca/40Ca ratios in intermediate-mass stars expected if the 44Ti synthesis has instead been the result of a few rare events of very large 44Ti yield. The present data speak against that. The new arguments that we have presented here can all be improved dramatically in the next few years. Although their message today is not statistically certain, their sense is to support the original conflict that we have displayed in Fig. 2. Because the 44Ca/40Ca ratio in mainstream grains from many AGB stars is very near to the solar ratio, we point out that it is no longer possible to entertain the idea that the sun may itself contain an anomalous 44Ca/40Ca ratio. One can not blame the inability of standard models of the chemical evolution of the galaxy to produce enough 44Ca by speculating that the sun is abnormally rich in its 44Ca content.
It should be noted that a thorough study of stardust isotopic
inhomogeneity within the context of inhomogeneous galactic chemical
evolution has been presented by
Nittler (2005).
He shows in particular
that correlations between Si and Ti isotopic compositions found in
stardust can not be accounted for by inhomogeneous GCE. He does not,
however, discuss the variations in 44Ca/40Ca
that are generated by his
model owing to the He-cap SNIa. On the other hand, his calculations may
not be ideal for this problem because his model admixes into a homogeneous
ISM the same fraction for each supernova's ejecta
(a =
)
after Monte Carlo sampling
to obtain N=70 supernovae. Nonetheless, that paper shows
the potential power of stardust to delimit GCE inhomogeneities in general.
This approach should be reconsidered carefully when a good data set for
initial 44Ca/40Ca in stardust is available.
Mainstream SiC grains are probably not the best grains with which to measure initial stellar 44Ca/40Ca abundance ratios. The mainstream SiC grains contain very little Ca because Ca is much less favored chemically than is Ti within thermally condensing SiC grains. The hibonite Stardust grains described by Nittler et al. (2005), on the other hand, contain much more Ca because Ca is an essential ingredient of the hibonite crystal structure. Therefore, accurate measurements of 44Ca/40C in hibonite grains could reveal better information relevant to ISM inhomogeneity of the 44Ca/40Ca ratio.