CCD images and long-slit spectroscopy of the ring nebula around θ Mus     

Carlos Guillermo Giménez de Castro  & Virpi S. Niemela 《Monthly notices of the Royal Astronomical Society》1998,297(4):1060-1066

We present the first digital CCD images and long-slit spectroscopy of the optical ring nebula around the Wolf–Rayet star θ Mus. The CCD images obtained through narrow-band filters centred at [O  iii ] and Hα show that the nebula has a filamentary structure, similar to supernova remnants, mainly seen in [O  iii ]. A spatial detachment between [O  iii ] and Hα images suggests excitation stratification, or multiple rings. An analysis of the physical conditions in the nebula was performed by means of long-slit CCD spectra. The spectral images show that the nebula is of low density and medium excitation. By means of quotients of recombination and collisional spectral line fluxes we determine that the principal excitation mechanism is photoionization. We have determined the electronic temperature and density, and chemical abundances for the oxygen at different sites within the nebula. Nebular chemical abundances are found to be similar to the Galactic ISM, indicating that the nebula is mainly composed of swept up material.  相似文献   

The structure of galaxy clusters in various cosmologies     

Peter A. Thomas  Jörg M. Colberg  Hugh M. P. Couchman  George P. Efstathiou  Carlos S. Frenk  Adrian R. Jenkins  Alistair H. Nelson  Roger M. Hutchings  John A. Peacock  Frazer R. Pearce  & Simon D. M. White 《Monthly notices of the Royal Astronomical Society》1998,296(4):1061-1071

We investigate the internal structure of clusters of galaxies in high-resolution N -body simulations of four different cosmologies. There is a higher proportion of disordered clusters in critical-density than in low-density universes, although the structure of relaxed clusters is very similar in each case. Crude measures of substructure, such as the shift in the position of the centre-of-mass as the density threshold is varied, can distinguish the two in a sample of just 20 or so clusters; it is harder to differentiate between clusters in open and flat models with the same density parameter. Most clusters are in a quasi-steady state within the virial radius and are well-described by the density profile of Navarro, Frenk & White.  相似文献   

Geomorphological and sedimentological analysis of a catastrophic flash flood in the Arás drainage basin (Central Pyrenees, Spain)   总被引：1，自引：0，他引：1  

Francisco Gutirrez  Mateo Gutirrez  Carlos Sancho 《Geomorphology》1998,22(3-4)

On August 7th, 1996, an intense and short-duration convective storm occurred over the 18.6-km² Arás drainage basin (Central Pyrenees, Spain). This high relief basin is composed of three subbasins, Aso, Betés and La Selva, and feeds the Arás alluvial fan, in the Gállego river valley. This alluvial fan had been drained by an artificial channel (about 125 m³/s at bank-full capacity). More than 30 check dams in its feeder channel, the Arás barranco, had been previously filled by earlier sediments. The heaviest rain was over the Betés subbasin (total rainfall 178.4 mm; maximum rainfall intensity of 153 mm/h for a 10-min time interval was estimated). Most of the rainfall fell in a 70-min period. This storm resulted in high runoff, causing catastrophic damage and significant geomorphic changes in the drainage basin, especially in the Betés subbasin. The high discharge, concentrated in the Arás barranco, destroyed most of the check dams, flushing out a great amount of debris. Major channel trenching and widening occurred in this barranco. When the confined sediment-laden flash flood reached the basin mouth, it sheet-flooded the southern sector of the Arás fan depositing a massive amount of debris. On this fan 87 people lost their lives and the direct physical damage has been estimated at 55 million dollars. Two stages in the development of the flood have been differentiated from the sedimentological and morphological analysis of the flooded fan lobe. A first stage (peak discharge) of sheet-flooding deposited a coarse boulder lobe, burying the artificial channel at the fan head and causing a darnming effect on the water flood. During the second stage (discharge decline) the flood made its way through the fan head, incising the previous debris accumulation and splitting into two main flow paths.  相似文献   

If Quebec Goes . . . The ‘Exodus' Impact?     

Lucia Lo  Carlos Teixeira 《The Professional geographer》1998,50(4):481-498

In this paper, we explore migration aspects of the 1995 Quebec Sovereignty Referendum with data from a survey administered to non-francophones in Montreal two weeks prior to the Referendum. While the Quebec sovereignty issue has been around for some time and earlier exodus from the province, particularly among anglophones, is largely regarded as “forced” in some way, this study neither confirms the 1995 Sovereignty Referendum as a paramount factor in explaining outmigration from Quebec nor points to a real reluctance to leave Montreal. The decision to move is influenced by the interplay of a multitude of factors. The political influence is only an added factor to longstanding economic decline and cultural clash. Moreover, if there is any impulsion, the degree varies among different cultural and socioeconomic groups.  相似文献   

Advances in discrete element modelling of underground excavations   总被引：1，自引：1，他引：0  

Carlos Labra  Jerzy Rojek  Eugenio Oñate  Francisco Zarate 《Acta Geotechnica》2008,3(4):317-322

The paper presents advances in the discrete element modelling of underground excavation processes extending modelling possibilities as well as increasing computational efficiency. Efficient numerical models have been obtained using techniques of parallel computing and coupling the discrete element method with finite element method. The discrete element algorithm has been applied to simulation of different excavation processes, using different tools, TBMs and roadheaders. Numerical examples of tunnelling process are included in the paper, showing results in the form of rock failure, damage in the material, cutting forces and tool wear. Efficiency of the code for solving large scale geomechanical problems is also shown.  相似文献   

A Pulsed Laser Photolysis-Resonance Fluorescence Kinetic Study of the Atmospheric Cl Atom-Initiated Oxidation of Propene and a Series of 3-Halopropenes at Room Temperature     

José Albaladejo  Alberto Notario  Carlos A. Cuevas  Bernabé Ballesteros  Ernesto Martínez 《Journal of Atmospheric Chemistry》2003,45(1):35-50

Absolute rate coefficient measurements have been carried out for the reactions of Cl atoms with propene and a series of 3-halopropenes, at room temperature (298 ± 2) K using a newly constructed laser photolysis-resonance fluorescence (PLP-RF) system. The rate coefficients obtained (in units of cm³ molecule^–1 s^–1) are: propene (1.40± 0.24) ×10^–10, 3-fluoropropene (4.92 ± 0.42) ×10^–11, 3-chloropropene (7.47 ± 1.50) × 10^–11, 3-bromopropene (1.23± 0.14) ×10^–10 and 3-iodopropene (1.29± 0.15) ×10^–10. In order to test this new system, the reactions of Cl atoms with acetone and isoprene have also been studied and compared with data previously reported. The rate coefficients determined at room temperature for these last two reactions are (2.93 ± 0.20) ×10^–12 cm³ molecule^–1 s^{– 1} and (3.64± 0.20)×10^–10 cm³ molecule^–1 s^–1, respectively. The measured values were independent of pressure over the range 20–200 Torr. The influence of the different halogen atoms substituents on the reactivity of these alkenes with Cl atoms as well as the atmospheric implications of these measurements are studied and discussed for the first time in this work and compared with the reactivity with NO₃ and OH radicals.  相似文献   

Seismic Vulnerability of Historical Constructions: A Contribution   总被引：1，自引：0，他引：1  

Carlos Sousa Oliveira 《Bulletin of Earthquake Engineering》2003,1(1):37-82

Earthquakes are known to be natural hazards that have affected tremendously historical constructions. Unfortunately, as far as earthquake impacts are concerned, there are no world statistics to compare the suffering of populations or of the building stock and their evolution in time, with the damage inflicted to the stock of historical constructions. Lately, a great effort has been placed on engineering developments: (i) to better understand the seismic behaviour of historical construction and (ii) to assess the benefits of different techniques for reinforcing these structures. However, a great deal of discussion is still going on the type of reinforcement that should be applied, how effective it is and how much it costs. Research is needed for helping in these decisions, by providing a more precise framework in this field. The aim of this review is to make an overall insight on some of the available methods for assessing seismic vulnerability of historical constructions and on how to use them in the case of occurrence of an earthquake. Given this occurrence, the objective is to minimize the effects of aftershocks, avoid hurried demolition made under extreme pressure and help shore-up parts in risk of falling. The final aim is also to help in the definition of strategies for the repair of the damaged patrimony, or as a measure to prevent damage in future earthquakes for the most vulnerable cases. The paper is illustrated with the presentation of several examples published in the literature where the author participated. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   

3D imaging of a reservoir analogue in point bar deposits in the Ferron Sandstone, Utah, using ground-penetrating radar     

Xiaoxian Zeng  George A. McMechan  Janok P. Bhattacharya  Carlos L.V. Aiken  Xueming Xu  William S. Hammon III    Rucsandra M. Corbeanu 《Geophysical Prospecting》2004,52(3):151-163

Most existing reservoir models are based on 2D outcrop studies; 3D aspects are inferred from correlation between wells, and so are inadequately constrained for reservoir simulations. To overcome these deficiencies, we have initiated a multidimensional characterization of reservoir analogues in the Cretaceous Ferron Sandstone in Utah. Detailed sedimentary facies maps of cliff faces define the geometry and distribution of reservoir flow units, barriers and baffles at the outcrop. High‐resolution 2D and 3D ground‐penetrating radar (GPR) images extend these reservoir characteristics into 3D to allow the development of realistic 3D reservoir models. Models use geometric information from mapping and the GPR data, combined with petrophysical data from surface and cliff‐face outcrops, and laboratory analyses of outcrop and core samples. The site of the field work is Corbula Gulch, on the western flank of the San Rafael Swell, in east‐central Utah. The outcrop consists of an 8–17 m thick sandstone body which contains various sedimentary structures, such as cross‐bedding, inclined stratification and erosional surfaces, which range in scale from less than a metre to hundreds of metres. 3D depth migration of the common‐offset GPR data produces data volumes within which the inclined surfaces and erosional surfaces are visible. Correlation between fluid permeability, clay content, instantaneous frequency and instantaneous amplitude of the GPR data provides estimates of the 3D distribution of fluid permeability and clay content.  相似文献   

An overview of Calanus helgolandicus ecology in European waters     

Delphine Bonnet  Anthony Richardson  Andrew Hirst  Martin Edwards  Rabea Diekman  Luis Valdes  Juan Carlos Molinero  Wulf Greve  Aitor Albaina  Serena Fonda Umani  Antonina dos Santos  Susan Robinson 《Progress in Oceanography》2005,65(1):1-53

We review current knowledge and understanding of the biology and ecology of the calanoid copepod Calanus helgolandicus in European waters, as well as provide a collaborative synthesis of data from 18 laboratories and 26 sampling stations in areas distributed from the northern North Sea to the Aegean and Levantine Seas. This network of zooplankton time-series stations has enabled us to collect and synthesise seasonal and multi-annual data on abundance, body size, fecundity, hatching success and vertical distribution of C. helgolandicus. An aim was to enable comparison with its congener Calanus finmarchicus, which has been studied intensively as a key component of European and north east Atlantic marine ecosystems. C. finmarchicus is known to over-winter at depth, whereas the life-cycle of C. helgolandicus is less well understood. Overwintering populations of C. helgolandicus have been observed off the Atlantic coast between 400 and 800 m, while in the Mediterranean there is evidence of significant deep-water populations at depths as great as 4200 m. The biogeographical distribution of C. helgolandicus in European coastal waters covers a wide range of habitats, from open ocean to coastal environments, and its contribution to mesozooplankton biomass ranges from 6% to 93%. Highest abundances were recorded in the Adriatic and off the west coast of Spain. C. helgolandicus is generally found in 9-20 °C water, with maximum abundances from 13-17 °C. In contrast, C. finmarchicus is found in cooler water between 0 and 15 °C, with peak abundances from 0 to 9 °C. As water has warmed in the North Atlantic over recent decades, the range of C. helgolandicus and its abundance on the fringes of its expanding range have increased. This review will facilitate development of population models of C. helgolandicus. This will not only help answer remaining questions but will improve our ability to forecast future changes, in response to a warming climate, in the abundance and distribution of this important species.  相似文献   

Suspended-sediment response to pulses in river flow and semidiurnal and fortnightly tidal variations in a mesotidal estuary     

Carlos Vale  Carlota Corteso  Odete Castro  Ana M. Ferreira 《Marine Chemistry》1993,43(1-4)

The effects of the tidal regime and high river flows on the suspended sediment concentration field have been separated and the retention time of fluvial sediment has been determined. The study was carried out in the upper Sado estuary, Portugal, and included surveys at high and low tide in different semidiurnal tide ranges every month for 1 year, including contrasting freshwater discharge. DDT and its metabolites (DDD and DDE) were determined in the suspended sediment and in the whole soft tissues of oysters, and they have been used as tracers of the derived flood material in the upper estuary. The tide is responsible for the relatively slow relaxation time following a winter runoff event.  相似文献