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- Light-element
depletion in contracting pre-main-sequence stars and brown dwarfs
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Starting with an analytical calculation of the thermonuclear depletion
of lithium, beryllium, and boron in contracting, fully convective,
pre-main-sequence stars less massive than about 0.5 solar masses, we
demonstrated the robustness of using the lithium abundance for
constraining cluster ages. Because these low mass stars are fully
convective, we can accurately model them as fully mixed polytropes
(index 3/2) with the assumption that the effective temperature is fixed.
The destruction rate of lithium, beryllium, and boron are strong
functions of central temperature, and so the transition from the star
having an abundance of these elements to having a deficit is rapid.
This is fortunate, as it is easy to determine if a star is depleted, but
difficult to determine by how much.
Although our calculation assumes a fixed effective temperature, it does not
constrain its value. Our technique then accurately determines the radius,
age, and luminosity of the pre-main-sequence star as a function of two
observables, elemental abundance and effective temperature. Lithium
abundance observations also provide a useful discriminant between stars and
brown dwarfs, as the latter do not reach central temperatures hot enough to
destroy lithium. By comparing pairs of cluster stars, one with lithium and
one without, we determined a minimum age (60 Myr) for α Persei and the
Pleiades (105 Myr), in confirmation of that found by Basri et al.
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A possible sub-threshold resonance in beryllium
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While fitting the reactions, I became interested in the possible effect of
a sub-threshold (25.7 keV) resonance in the reaction
9Be(p,α)6Li. Experiments had been unable to
accurately determine the spin and parity of the intermediate state; one of
the possible (spin, parity) combinations would allow this reaction to
proceed via a level in the compound nucleus 10B with an
s-wave entrance channel. In principle this resonance could be
tested by observations of beryllium abundances in sub-solar mass stars.
- Carbon burning on
accreting neutron stars
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Many accreting neutron stars exihibit X-ray bursts (called type I) which
canonically appear as a rapid brightening on a timescale of order 1 s,
followed by a roughly exponential decay. The recurrence times,
energetics, and spectral properties of these bursts are consistent with
them being due to unstable burning of accreted H/He.
For neutron stars rapidly accreting pure He (such as on the polar cap of
an accretion-powered pulsar), there is a possibility of detecting
unstable carbon burning. At super-Eddington local accretion rates, the
recurrence times are short enough (hours to days) to make this burning
observable.
Recently, large super bursts have been observed from several weakly
magnetized neutron stars. One example of which is 4U 1820-30,
which accretes pure He from its companion. For this object, the
identification of the superburst with a thermonuclear instability in a
carbon-rich layer seems secure; there remain many interesting questions
about the energetics and evolution of the burst.
- Thermal
structure of accreting neutron stars
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Accretion at near-Eddington rates heats the outer atmosphere to
temperatures greater than 5 108 K. At this temperature,
neutrino emissions from the deep crust (densities greater than neutron
drip) and core become important. These rates are relevant for the
brightest low-mass X-ray binaries, the Z sources. As the material in the
crust is pushed ever deeper by the accumulation of material in overlying
layers, a series of compression-induced reactions (electron captures,
neutron emissions, and pycnonuclear reactions) release about 1 MeV per
accreted baryon (Haensel 1990); this heat is deposited in the region about
neutron drip. This heat is then conducted into the deep crust and core and
re-emitted as neutrinos. The temperature in the inner crust and core
therefore depends on the method of neutrino emission (i.e., modified Urca
vs. accelerated mechanisms) and also the degree to which proton and neutron
superfluidity suppress that emission.
For low-mass X-ray binaries, accretion over the lifetime of the binary
(∼ 109 yr) can replace the entire crust. This crust
will differ in composition from the original, which is approximately in
nuclear statistical equilibrium. The impurities can drastically reduce the
thermal conductivity, which leads to a decrease in the timescale for ohmic
decay of crustal magnetic fields.
- Magnetic
confinement of accreted material
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This work began with a study of how deep the strong magnetic fields of
accreting X-ray pulsars could confine the accretion flow, and the
consequences for unstable hydrogen/helium burning on the accreting pulsar
(2.14 Hz) GRO J1744-28 and unstable carbon burning on more strongly
magnetized X-ray pulsars. Following Hameury et al., L. Bildsten & I
performed a magnetostatic calculation and found that the magnetic field
lines are strongly distorted from vertical (i.e., the mound spreads) when
the pressure at its base is greater than about R/H times the magnetic
pressure B2/8 π, where R is the radius of the polar cap and H
is the thickness of the atmosphere. We applied this to GRO J1744-28
and found that the inferred magnetic field could confine the accretion flow
enough to make the burning of hydrogen and helium stable. This would
explain the absence of type I X-ray bursts. We expected that as the
outburst faded and the accretion rate declined, the local accretion rate
would eventually become sub-Eddington and allow unstable burning to begin.
The absence of unstable burning (either in the form of type I X-ray bursts
or slow flares) raises intriguing questions about the geometry of the polar
cap and the ability of the magnetic field to halt a convective burning
front.
A more refined calculation of the stability of the accreted material was
done my C Litwin, myself, and R Rosner. We found that line-tying to the
crust stabilizes short-wavelength ballooning modes until the
overpressure at the top of the neutron star crust exceeds the magnetic
pressure by a factor ∼8(a/h), where a and h
are, respectively, the lateral extent of the accretion region and the
density scale height. The most unstable modes are localized within a
density scale height above the crust.
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