641 research outputs found
Quantum group invariant, nonextensive quantum statistical mechanics
We study the consequences of introducing quantum group invariance in the
formalism of nonextensive quantum statistical mechanics.
We find that the corresponding thermodynamical system is equivalent to a
Bose-Einstein gas in the Boltzmann-Gibbs formalism with a higher critical
temperature than the standard Bose-Einstein case.Comment: Revtex file, 6 pages, one figure. The original article has been
expanded to include some additional comments, one figure and a discussion
regarding the critical temperature. One reference adde
Compatibility of Gauss maps with metrics
We give necessary and sufficient conditions on a smooth local map of a
Riemannian manifold into the sphere to be the Gauss map of an
isometric immersion , . We briefly discuss the case of
general as wellComment: 14 pages, no figure
The promoter from SlREO, a highly-expressed, root-specific Solanum lycopersicum gene, directs expression to cortex of mature roots
Root-specific promoters are valuable tools for targeting transgene expression, but many of those already described have limitations to their general applicability. We present the expression characteristics of SlREO, a novel gene isolated from tomato (Solanum lycopersicum L.). This gene was highly expressed in roots but had a very low level of expression in aerial plant organs. A 2.4-kb region representing the SlREO promoter sequence was cloned upstream of the uidA GUS reporter gene and shown to direct expression in the root cortex. In mature, glasshouse-grown plants this strict root specificity was maintained. Furthermore, promoter activity was unaffected by dehydration or wounding stress but was somewhat suppressed by exposure to NaCl, salicylic acid and jasmonic acid. The predicted protein sequence of SlREO contains a domain found in enzymes of the 2-oxoglutarate and Fe(II)-dependent dioxygenase superfamily. The novel SlREO promoter has properties ideal for applications requiring strong and specific gene expression in the bulk of tomato root tissue growing in soil, and is also likely to be useful in other Solanaceous crop
Effect of Re-impacting Debris on the Solidification of the Lunar Magma Ocean
Anorthosites that comprise the bulk of the lunar crust are believed to have
formed during solidification of a Lunar Magma Ocean (LMO) in which these rocks
would have floated to the surface. This early flotation crust would have formed
a thermal blanket over the remaining LMO, prolonging solidification.
Geochronology of lunar anorthosites indicates a long timescale of LMO cooling,
or re-melting and re-crystallization in one or more late events. To better
interpret this geochronology, we model LMO solidification in a scenario where
the Moon is being continuously bombarded by returning projectiles released from
the Moon-forming giant impact. More than one lunar mass of material escaped the
Earth-Moon system onto heliocentric orbits following the giant impact, much of
it to come back on returning orbits for a period of 100 Myr. If large enough,
these projectiles would have punctured holes in the nascent floatation crust of
the Moon, exposing the LMO to space and causing more rapid cooling. We model
these scenarios using a thermal evolution model of the Moon that allows for
production (by cratering) and evolution (solidification and infill) of holes in
the flotation crust that insulates the LMO. For effective hole production,
solidification of the magma ocean can be significantly expedited, decreasing
the cooling time by more than a factor of 5. If hole production is inefficient,
but shock conversion of projectile kinetic energy to thermal energy is
efficient, then LMO solidification can be somewhat prolonged, lengthening the
cooling time by 50% or more
High-Resolution Submillimeter and Near-Infrared Studies of the Transition Disk around Sz 91
To reveal the structures of a transition disk around a young stellar object
in Lupus, Sz 91, we have performed aperture synthesis 345 GHz continuum and
CO(3--2) observations with the Submillimeter Array (\sim1\arcsec--3\arcsec
resolution), and high-resolution imaging of polarized intensity at the
-band by using the HiCIAO instrument on the Subaru Telescope (0\farcs25
resolution). Our observations successfully resolved the inner and outer radii
of the dust disk to be 65 AU and 170 AU, respectively, which indicates that Sz
91 is a transition disk source with one of the largest known inner holes. The
model fitting analysis of the spectral energy distribution reveals an H
mass of M_\sun in the cold (30 K) outer part at
AU by assuming a canonical gas-to-dust mass ratio of 100, although a
small amount ( M_\sun) of hot (180 K) dust possibly
remains inside the inner hole of the disk. The structure of the hot component
could be interpreted as either an unresolved self-luminous companion body (not
directly detected in our observations) or a narrow ring inside the inner hole.
Significant CO(3--2) emission with a velocity gradient along the major axis of
the dust disk is concentrated on the Sz 91 position, suggesting a rotating gas
disk with a radius of 420 AU. The Sz 91 disk is possibly a rare disk in an
evolutionary stage immediately after the formation of protoplanets because of
the large inner hole and the lower disk mass than other transition disks
studied thus far
High-Contrast NIR Polarization Imaging of MWC480
One of the key predictions of modeling from the IR excess of Herbig Ae stars
is that for protoplanetary disks, where significant grain growth and settling
has occurred, the dust disk has flattened to the point that it can be partially
or largely shadowed by the innermost material at or near the dust sublimation
radius. When the self-shadowing has already started, the outer disk is expected
to be detected in scattered light only in the exceptional cases that the scale
height of the dust disk at the sublimation radius is smaller than usual.
High-contrast imaging combined with the IR spectral energy distribution allow
us to measure the degree of flattening of the disk, as well as to determine the
properties of the outer disk. We present polarimetric differential imaging in
band obtained with Subaru/HiCIAO of one such system, MWC 480. The HiCIAO
data were obtained at a historic minimum of the NIR excess. The disk is
detected in scattered light from 0\farcs2-1\farcs0 (27.4-137AU). Together with
the marginal detection of the disk from 1998 February 24 by HST/NICMOS, our
data constrain the opening half angle for the disk to lie between
1.3. When compared with similar measures in CO for
the gas disk from the literature, the dust disk subtends only 30% of the
gas disk scale height (H/R0.03). Such a dust disk is a factor of 5-7
flatter than transitional disks, which have structural signatures that giant
planets have formed.Comment: 21 pages, 6 figures, 1 table, ApJ accepted 2012-05-0
The effect of slip variability on earthquake slip-length scaling
There has been debate on whether average slip D in long ruptures should scale with rupture length L, or with rupture width W. This scaling discussion is equivalent to asking whether average stress drop Δσ, which is sometimes considered an intrinsic frictional property of a fault, is approximately constant over a wide range of earthquake sizes. In this paper, we examine slip-length scaling relations using a simplified 1-D model of spatially heterogeneous slip. The spatially heterogeneous slip is characterized by a stochastic function with a Fourier spectrum that decays as k^(−α), where k is the wavenumber and α is a parameter that describes the spatial smoothness of slip. We adopt the simple rule that an individual earthquake rupture consists of only one spatially continuous segment of slip (i.e. earthquakes are not generally separable into multiple disconnected segments of slip). In this model, the slip-length scaling relation is intimately related to the spatial heterogeneity of the slip; linear scaling of average slip with rupture length only occurs when α is about 1.5, which is a relatively smooth spatial distribution of slip. We investigate suites of simulated ruptures with different smoothness, and we show that faults with large slip heterogeneity tend to have higher D/L ratios than those with spatially smooth slip. The model also predicts that rougher faults tend to generate larger numbers of small earthquakes, whereas smooth faults may have a uniform size distribution of earthquakes. This simple 1-D fault model suggests that some aspects of stress drop scaling are a consequence of whatever is responsible for the spatial heterogeneity of slip in earthquakes
Zds1/Zds2-PP2ACdc55 complex specifies signaling output from Rho1 GTPase
Acknowledgments We thank David Pellman, John Pringle, Daniel Lew, Masaki Mizunuma, Kenji Irie, and the Yeast Genome Resource Center for yeast strains and plasmids and members of Yoshida Laboratory and Keiko Kono for their support. Multicopy suppressor screening for gef∆ was initiated in the Pellman Laboratory with the help of Didem Ilter. This research was supported by Sprout grant from Brandeis University (E.M. Jonasson and S. Yoshida), an American-Italian Cancer Foundation Postdoctoral fellowship (V. Rossio), and a Massachusetts Life Sciences Center grant (S. Yoshida).Peer reviewedPublisher PD
Thermostatistics of deformed bosons and fermions
Based on the q-deformed oscillator algebra, we study the behavior of the mean
occupation number and its analogies with intermediate statistics and we obtain
an expression in terms of an infinite continued fraction, thus clarifying
successive approximations. In this framework, we study the thermostatistics of
q-deformed bosons and fermions and show that thermodynamics can be built on the
formalism of q-calculus. The entire structure of thermodynamics is preserved if
ordinary derivatives are replaced by the use of an appropriate Jackson
derivative and q-integral. Moreover, we derive the most important thermodynamic
functions and we study the q-boson and q-fermion ideal gas in the thermodynamic
limit.Comment: 14 pages, 2 figure
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