11,849 research outputs found
Abelian extensions of semisimple graded CR algebras
In this paper we take up the problem of describing the CR vector bundles M
over compact standard CR manifolds S, which are themselves standard CR
manifolds. They are associated to special graded Abelian extensions of
semisimple graded CR algebras.Comment: 25 pages, 5 figure
Weyl states and Fermi arcs in parabolic bands
Weyl fermions are shown to exist inside a parabolic band, where the kinetic
energy of carriers is given by the non-relativistic Schroedinger equation.
There are Fermi arcs as a direct consequence of the folding of a ring shaped
Fermi surface inside the first Brillouin zone. Our results stem from the
decomposition of the kinetic energy into the sum of the square of the Weyl
state, the coupling to the local magnetic field and the Rashba interaction. The
Weyl fermions break the time and reflection symmetries present in the kinetic
energy, thus allowing for the onset of a weak three-dimensional magnetic field
around the layer. This field brings topological stability to the current
carrying states through a Chern number. In the special limit that the Weyl
state becomes gapless this magnetic interaction is shown to be purely
attractive, thus suggesting the onset of a superconducting condensate of zero
helicity states
Mapping the spatial variation of soil moisture at the large scale using GPR for pavement applications
The characterization of shallow soil moisture spatial variability at the large scale is a crucial issue in many research studies and fields of application ranging from agriculture and geology to civil and environmental engineering. In this framework, this work contributes to the research in the area of pavement engineering for preventing damages and planning effective management. High spatial variations of subsurface water content can lead to unexpected damage of the load-bearing layers; accordingly, both safety and operability of roads become lower, thereby affecting an increase in expected accidents.
A pulsed ground-penetrating radar system with ground-coupled antennas, i.e., 600-MHz and 1600-MHz center frequencies of investigation, was used to collect data in a 16 m Ă 16 m study site in the Po Valley area in northern Italy. Two ground-penetrating radar techniques were employed to non-destructively retrieve the subsurface moisture spatial profile. The first technique is based on the evaluÂŹation of the dielectric permittivity from the attenuation of signal amplitudes. Therefore, dielectrics were converted into moisture values using soil-specific coefficients from Toppâs relationship. Ground-penetrating-radar-derived values of soil moisture were then compared with measurements from eight capacitance probes. The second technique is based on the Rayleigh scattering of the signal from the Fresnel theory, wherein the shifts of the peaks of frequency spectra are assumed comprehensive indiÂŹcators for characterizing the spatial variability of moisture. Both ground-penetrating radar methods have shown great promise for mapping the spatial variability of soil moisture at the large scale
Facies, architecture and genetic controls of carbonate ramp aprons development
Cool-water Carbonate Ramp Aprons (CRA) are depositional systems in which skeletal sand and gravel are redistributed basinwards on a ramp, off a shallow carbonate platform by tractive currents as a result of flow funnelling in between topographic highs. These deposits are different and should not be confused with the carbonate apron models proposed by of Mullins and Cook (1986) who describe either carbonate deep water turbiditic systems accumulated at the base of the slope or talus cones formed at the margins of carbonate build ups.
A key example of CRA facies assemblages is represented by the Early Pleistocene, Favignana Calcarenite where bimodal depositional processes, occurring in a water depth range estimated between 5 and 80 m, typical of this depositional environment, resulted in the accumulation of distinct and alternating sedimentary packages: a low- energy sedimentary assemblage formed by typical subaqueous dunes consisting of tabular cross bedded grainstones and packstones often bioturbated is coupled with a heterogeneous facies assemblage where, coarse-grain filled erosional depressions, largely variable in size, formed by downslope confined flows generating elongated scours are associated with low- angle cross bedded grainstones formed in supercritical conditions (backset bedded, antidunes etc).
Based on outcrop examination and 2D seismic line interpretation CRA deposits have a triangular shape which form a series of coalescent fans forming an overall apron connecting the shallow carbonate platform/ inner ramp setting (factory) to the deeper basin through a steep ramp. The seismic data in particular allow the deciphering of the internal architecture and understanding the modality of progradation and aggradation and lateral shift of these sedimentary bodies. In the sedimentary record the carbonate ramp aprons develops a wedge-like geometry composed by discrete superposed and laterally stacked lenticular bodies often separated by erosional surfaces marked by reflector discontinuities. The frequency of erosional/reactivation surfaces attest for frequent high-energy events which, in the basis of sedimentary facies present in outcrops, demonstrate the important role plaid by high-energy storms and possibly tsunamis in building these deposits.
Similarly to what has been described for the Favignana Calcarenites, CRA deposits can represent an important part of ancient sedimentary record of intrashelf carbonate successions such as the Oligocene/Miocene carbonate successions in the Gulf of Venezuela. There, well-sorted calcarenite drift deposits forming similar well-sorted calcarenite drift apron-shaped deposits, similar to the ones described in Favignana are visible in the topographic lows, next to steep platform margins
The CR structure of minimal orbits in complex flag manifolds
Let \^G be a complex semisimple Lie group, Q a parabolic subgroup and G a
real form of \^G. The flag manifold \^G/Q decomposes into finitely many
G-orbits; among them there is exactly one orbit of minimal dimension, which is
compact. We study these minimal orbits from the point of view of CR geometry.
In particular we characterize those minimal orbits that are of finite type and
satisfy various nondegeneracy conditions, compute their fundamental group and
describe the space of their global CR functions. Our main tool are parabolic CR
algebras, which give an infinitesimal description of the CR structure of
minimal orbits.Comment: AMS-TeX, 44 pages v2: minor revisio
How Do Output Growth Rate Distributions Look Like? Some Time-Series Evidence on OECD Countries
This paper investigates the statistical properties of within-country GDP and
industrial production (IP) growth rate distributions. Many empirical
contributions have recently pointed out that cross-section growth rates of
firms, industries and countries all follow Laplace distributions. In this work,
we test whether also within-country, time-series GDP and IP growth rates can be
approximated by tent-shaped distributions. We fit output growth rates with the
exponential-power (Subbotin) family of densities, which includes as particular
cases both the Gaussian and the Laplace distributions. We find that, for a
large number of OECD countries including the U.S., both GDP and IP growth rates
are Laplace distributed. Moreover, we show that fat-tailed distributions
robustly emerge even after controlling for outliers, autocorrelation and
heteroscedasticity
Mesoscopic simulation study of wall roughness effects in micro-channel flows of dense emulsions
We study the Poiseuille flow of a soft-glassy material above the jamming
point, where the material flows like a complex fluid with Herschel- Bulkley
rheology. Microscopic plastic rearrangements and the emergence of their spatial
correlations induce cooperativity flow behavior whose effect is pronounced in
presence of confinement. With the help of lattice Boltzmann numerical
simulations of confined dense emulsions, we explore the role of geometrical
roughness in providing activation of plastic events close to the boundaries. We
probe also the spatial configuration of the fluidity field, a continuum
quantity which can be related to the rate of plastic events, thereby allowing
us to establish a link between the mesoscopic plastic dynamics of the jammed
material and the macroscopic flow behaviour
On the topology of minimal orbits in complex flag manifolds
We compute the Euler-Poincar\'e characteristic of the homogeneous compact
manifolds that can be described as minimal orbits for the action of a real form
in a complex flag manifold.Comment: 21 pages v2: Major revisio
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