4,031 research outputs found
Self-gravitational corrections to the Cardy-Verlinde formula of charged BTZ black hole
The entropy of the charged BTZ black hole horizon is described by the
Cardy-Verlinde formula. We then compute the self-gravitational corrections to
the Cardy-Verlinde formula of the charged BTZ black hole in the context of
Keski-Vakkuri, Kraus and Wilczek (KKW) analysis. The self-gravitational
corrections to the entropy as given by the Cardy-Verlinde formula are found to
be positive. This result provides evidence in support of the claim that the
holographic bound is not universal in the framework of two-dimensional gravity
models.Comment: 12 pages, minor revision, accepted for publication in MPL
Anderson Transition in Disordered Bilayer Graphene
Employing the Kernel Polynomial method (KPM), we study the electronic
properties of the graphene bilayers in the presence of diagonal disorder,
within the tight-binding approximation. The KPM method enables us to calculate
local density of states (LDOS) without need to exactly diagonalize the
Hamiltonian. We use the geometrical averaging of the LDOS's at different
lattice sites as a criterion to distinguish the localized states from extended
ones. We find that bilayer graphene undergoes Anderson metal-insulator
transition at a critical value of disorder strength
A Model of the EGRET Source at the Galactic Center: Inverse Compton Scattering Within Sgr A East and its Halo
Continuum low-frequency radio observations of the Galactic Center reveal the
presence of two prominent radio sources, Sgr A East and its surrounding Halo,
containing non-thermal particle distributions with power-law indices around
2.5-3.3 and 2.4, respectively. The central 1-2 pc region is also a source of
intense (stellar) UV and (dust-reprocessed) far-IR radiation that bathes these
extended synchrotron-emitting structures. A recent detection of gamma-rays
(2EGJ1746-2852) from within around 1 degree of the Galactic Center by EGRET
onboard the Compton GRO shows that the emission from this environment extends
to very high energies.
We suggest that inverse Compton scatterings between the power-law electrons
inferred from the radio properties of Sgr A East and its Halo, and the UV and
IR photons from the nucleus, may account for the possibly diffuse gamma-ray
source as well. We show that both particle distributions may be contributing to
the gamma-ray emission, though their relevant strength depends on the actual
physical properties (such as the magnetic field intensity) in each source. If
this picture is correct, the high-energy source at the Galactic Center is
extended over several arcminutes, which can be tested with thenext generation
of gamma-ray and hard X-ray missions.Comment: latex, 14 pages, 3 figures (accepted for publication in ApJ
Equivalence of a one-dimensional driven-diffusive system and an equilibrium two-dimensional walk model
It is known that a single product shock measure in some of one-dimensional
driven-diffusive systems with nearest-neighbor interactions might evolve in
time quite similar to a random walker moving on a one-dimensional lattice with
reflecting boundaries. The non-equilibrium steady-state of the system in this
case can be written in terms of a linear superposition of such uncorrelated
shocks. Equivalently, one can write the steady-state of this system using a
matrix-product approach with two-dimensional matrices. In this paper we
introduce an equilibrium two-dimensional one-transit walk model and find its
partition function using a transfer matrix method. We will show that there is a
direct connection between the partition functions of these two systems. We will
explicitly show that in the steady-state the transfer matrix of the one-transit
walk model is related to the matrix representation of the algebra of the
driven-diffusive model through a similarity transformation. The physical
quantities are also related through the same transformation.Comment: 5 pages, 2 figures, Revte
Numerical fault simulation in Himalayas with 2 D finite element method
The nature of the stress field in the Himalaya is examined by the 2D finite element method where linear elastic rheology and plain strain condition are assumed. The Mohr-Coulomb failure criterion has been adopted to analyze the relationship between stress distribution and fault formation.Two profile models are prepared and convergent displacement is imposed on them along the NE-SW horizontal direction.The convergent displacement and physical properties of the rock layer control the distribution,orientation,magnitude and intensity of the stress and fault development.According to the calculated stress pattern,thrust faults are expected to develop in the central Himalaya (model A).Normal and some thrust faults take place in the north-western Himalaya (model B).The results from our numerical experiment are in agreement with those from the seismicity and focal mechanism solution of earthquakes and also with those of M.M.Alam and D.Hayashi (Bull.Fac.Sci.Univ. Ryukyus, 73, 15, 2002) in the central Himalaya
Rapid Cycling and Exceptional Yield in a Metal-Organic Framework Water Harvester.
Sorbent-assisted water harvesting from air represents an attractive way to address water scarcity in arid climates. Hitherto, sorbents developed for this technology have exclusively been designed to perform one water harvesting cycle (WHC) per day, but the productivities attained with this approach cannot reasonably meet the rising demand for drinking water. This work shows that a microporous aluminum-based metal-organic framework, MOF-303, can perform an adsorption-desorption cycle within minutes under a mild temperature swing, which opens the way for high-productivity water harvesting through rapid, continuous WHCs. Additionally, the favorable dynamic water sorption properties of MOF-303 allow it to outperform other commercial sorbents displaying excellent steady-state characteristics under similar experimental conditions. Finally, these findings are implemented in a new water harvester capable of generating 1.3 L kgMOF -1 day-1 in an indoor arid environment (32% relative humidity, 27 °C) and 0.7 L kgMOF -1 day-1 in the Mojave Desert (in conditions as extreme as 10% RH, 27 °C), representing an improvement by 1 order of magnitude over previously reported devices. This study demonstrates that creating sorbents capable of rapid water sorption dynamics, rather than merely focusing on high water capacities, is crucial to reach water production on a scale matching human consumption
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