The shock accretes mass at a rate
as determined
by the conditions in the core of the progenitor star
(see Sect. 4.4). In a stationary state, this rate
is equal to the rate at which matter is advected inward from the
shock to the neutrinosphere to be finally added into the neutron
star. The rate at which matter can be absorbed by the neutron star, however,
depends on the efficiency by which neutrinos are able to remove the energy
excess of the infalling material relative to the energy of the strongly bound
matter in the neutron star surface layers. For the
large accretion rates typical of the collapsed stellar core right after
bounce, the density is so high that the infalling matter becomes opaque
to neutrinos. In this case the efficiency of the energy loss is reduced.
When the gas is hotter, the neutrino opacity increases (because of the energy dependence of the
neutrino cross sections), and the neutrinosphere moves to a larger radius.
Due to this regulatory effect, the neutrinospheric temperature is a rather
inert quantity and, e.g., turns out to be very similar in different
numerical models. Therefore it is not a steady-state mass accretion rate which governs the
temperature at the base of the "atmosphere'' (as for accretion in optically
thin conditions), but the "surface'' of the nascent neutron star forms
where the temperature is sufficiently high for neutrino opaqueness to set in.
When neutrino cooling is not efficient enough, the advection of matter
through the neutrino cooling region is reduced compared to the accretion
into the shock, and matter piles up on top of the neutron star. Similarly,
strong neutrino heating in the gain region can reduce the inflow of matter.
The transition from accretion to an explosion is characterized by
an inversion of infall to outflow. For this reason the analysis of
the conditions for shock revival requires the inclusion of this sort of
time-dependence in the discussion. In the simplified model considered here,
the mass accretion rate is allowed to change between
and
.
Matter advected through
at a rate
determined by the efficiency of neutrino cooling is then assumed to be
added into the neutron star (compare Fig. 2).
Using Eqs. (2) and (6) and the definition
,
Eq. (4) can be rewritten in
the following form:
From Eq. (92) an approximation for
can be derived by
taking into account that
in the region between
and
,
where strong neutrino heating and cooling occurs.
Moreover, the integrand of the last term on the right hand
side of Eq. (92) is usually small, because
corresponds to about 8-9 MeV per nucleon for complete disintegration
of nuclei into free nucleons,
MeV per
nucleon, and
immediately above the shock, where the
infall velocity
is given by Eq. (43) and the
specific internal energy is typically much smaller than the specific
kinetic energy. For the same reason, the first term on the left hand
side of Eq. (92) is much smaller than the second term when
and
are of the same order.
With all this one gets
Such mass loss takes place during the later
phase of the neutrino-cooling evolution of the nascent neutron star, where a
baryonic wind, the so-called neutrino-driven wind, is blown off the
neutron star surface due to neutrino energy deposition just outside the
neutrinosphere (Qian & Woosley 1996). The transition from accretion
to mass outflow and the onset of mass loss can be discussed with
the formulae presented here. A description of the wind regime (where the
fluid velocity v approaches the local speed of sound), however, is beyond
the scope of the present work, because it requires retaining
the velocity gradient in the momentum equation, Eq. (3).
Assuming steady-state conditions, this leads to the well known set of
dynamic wind equations which can also be discussed by analytic means (see
Qian & Woosley 1996, and references therein). In contrast, the
toy model developed in this paper does not make use of
steady-state assumptions for the mass flow through the gain layer,
i.e., it is allowed that
in general.
The integral in Eq. (93) was evaluated in Sect. 6:
Copyright ESO 2001