1,499 research outputs found
Graphs of bounded degree and the -harmonic boundary
Let be a real number greater than one and let be a connected graph of
bounded degree. In this paper we introduce the -harmonic boundary of . We
use this boundary to characterize the graphs for which the constant
functions are the only -harmonic functions on . It is shown that any
continuous function on the -harmonic boundary of can be extended to a
function that is -harmonic on . Some properties of this boundary that are
preserved under rough-isometries are also given. Now let be a finitely
generated group. As an application of our results we characterize the vanishing
of the first reduced -cohomology of in terms of the
cardinality of its -harmonic boundary. We also study the relationship
between translation invariant linear functionals on a certain difference space
of functions on , the -harmonic boundary of with the first
reduced -cohomology of .Comment: Give a new proof for theorem 4.7. Change the style of the text in the
first two section
The first -cohomology of some finitely generated groups and -harmonic functions
Let be a finitely generated infinite group and let . In this paper
we make a connection between the first -cohomology space of and
-harmonic functions on . We also describe the elements in the first
-cohomology space of groups with polynomial growth, and we give an
inclusion result for nonamenable groups
Atmospheric NLTE-models for the spectroscopic analysis of blue stars with winds. IV. Porosity in physical and velocity space
[Abridged] Clumping in the radiation-driven winds of hot, massive stars
affects the derivation of synthetic observables across the electromagnetic
spectrum. We implement a formalism for treating wind clumping - in particular
the light-leakage effects associated with a medium that is porous in physical
and velocity space - into the global (photosphere+wind) NLTE model atmosphere
code FASTWIND. We assume a stochastic, two-component wind consisting of a
mixture of optically thick and thin clumps embedded in a rarefied inter-clump
medium. We account fully for the reductions in opacity associated with porosity
in physical and velocity-space, and for the well-known effect that opacities
depending on rho^2 are higher in clumpy winds than in smooth ones of equal
mass-loss rate. By formulating our method in terms of suitable mean and
effective opacities for the clumpy wind, we are able to compute models with the
same speed (~15 min. on a modern laptop) as in previous code-generations. Some
first, generic results of the new models include: i) Confirming earlier results
that velocity-space porosity is critical for analysis of UV wind lines in
O-stars; ii) for the optical Halpha line, optically thick clumping effects are
small for O-stars, but potentially very important for late B and A-supergiants;
iii) spatial porosity is a marginal effect for absorption of high-energy X-rays
in O-stars, as long as the mean-free path between clumps are kept at realistic
values; iv) porosity is negligible at typical O-star radio-photosphere radii;
v) regarding the wind ionization balance, a general trend is that increased
rates of recombination in simulations with optically thin clumps lead to
overall lower degrees of ionization than in corresponding smooth models, but
that this effect now is counteracted by the increased levels of light-leakage
associated with porosity in physical and velocity space.Comment: 12 pages, 5 figures, accepted for publication in Astronomy &
Astrophysic
2D wind clumping in hot, massive stars from hydrodynamical line-driven instability simulations using a pseudo-planar approach
Context: Clumping in the radiation-driven winds of hot, massive stars arises
naturally due to the strong, intrinsic instability of line-driving (the `LDI').
But LDI wind models have so far mostly been limited to 1D, mainly because of
severe computational challenges regarding calculation of the multi-dimensional
radiation force. Aims: To simulate and examine the dynamics and
multi-dimensional nature of wind structure resulting from the LDI. Methods: We
introduce a `pseudo-planar', `box-in-a-wind' method that allows us to
efficiently compute the line-force in the radial and lateral directions, and
then use this approach to carry out 2D radiation-hydrodynamical simulations of
the time-dependent wind. Results: Our 2D simulations show that the LDI first
manifests itself by mimicking the typical shell-structure seen in 1D models,
but how these shells then quickly break up into complex 2D density and velocity
structures, characterized by small-scale density `clumps' embedded in larger
regions of fast and rarefied gas. Key results of the simulations are that
density-variations in the well-developed wind statistically are quite isotropic
and that characteristic length-scales are small; a typical clump size is ~0.01R
at 2R, thus resulting also in rather low typical clump-masses ~10^17 g.
Overall, our results agree well with the theoretical expectation that the
characteristic scale for LDI-generated wind-structure is of order the Sobolev
length. We further confirm some earlier results that lateral `filling-in' of
radially compressed gas leads to somewhat lower clumping factors in 2D
simulations than in comparable 1D models. We conclude by discussing an
extension of our method toward rotating LDI wind models that exhibit an
intriguing combination of large- and small-scale structure extending down to
the wind base.Comment: 9 pages, 7 figures + 1 Appendix with 1 figure. Recommended for
publication in A&
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