Comments on “Geostatistics: Models and tools for the earth sciences” by A. G. Journel     

Jean Serra 《Mathematical Geosciences》1987,19(4):349-355

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Cinq années de sondages ozone sur Cagliari (Sardaigne)     

Mattna  N.  Porra'  G. P.  Serra  A. 《Pure and Applied Geophysics》1973,106(1):1169-1179

Resumé Pendant la période Février 1967-Février 1972 ont été accomplies, à l'Observatoire de Meteorologie Aéronautique de Cagliari,²) 157 sondages ozone par des sondes électrochimiques type Brewer.On présente un résumé des resultats des mesures et on décrit les caracteristiques principales de la répartition de l'ozone sur la verticale de Cagliari et ses variations saisonniéres.  相似文献   

Arome,a balloon-borne instrument for astronomical near-infrared spectrophotometry     

N. Sales  M. Giard  B. Brockman  J. P. Chabaud  J. P. Clavier  P. Coupiac  J. P. Crussaire  J. M. Lamarre  J. Narbonne  M. Nexon  F. Pajot  R. Korczak  D. Rouan  G. Serra 《Experimental Astronomy》1991,2(1):1-26

We present here the French balloon-borne experiment named AROME. This astronomical instrument is specifically designed for the detection of near infrared emission bands (=3–12m) from extended sources of low surface brightness with an angular resolution of 0.5°. The rms sensitivity achieved is of the order of 10^-8 Wm^-2sr^-1, in terms of the power radiated in the 3.3m band. We recall that this program led to the first detection of the 3.3m feature in the spectrum of the diffuse galactic emission. The scientific results were presented and interpreted in Paper I, Giard et al., 1989. Future work will include both the observation of fainter objects at 3.3m and the detection of other emission bands at 6.2 and 11.3m.  相似文献   

A possible impact crater for the 1908 Tunguska Event     

L. Gasperini  F. Alvisi  G. Biasini  E. Bonatti  G. Longo  M. Pipan  M. Ravaioli  R. Serra 《地学学报》2007,19(4):245-251

The so‐called ‘Tunguska Event’ refers to a major explosion that occurred on 30 June 1908 in the Tunguska region of Siberia, causing the destruction of over 2000 km² of taiga, globally detected pressure and seismic waves, and bright luminescence in the night skies of Europe and Central Asia, combined with other unusual phenomena. The ‘Tunguska Event’ may be related to the impact with the Earth of a cosmic body that exploded about 5–10 km above ground, releasing in the atmosphere 10–15 Mton of energy. Fragments of the impacting body have never been found, and its nature (comet or asteroid) is still a matter of debate. We report results from the investigation of Lake Cheko, located ∼8 km NNW of the inferred explosion epicenter. Its funnel‐like bottom morphology and the structure of its sedimentary deposits, revealed by acoustic imagery and direct sampling, all suggest that the lake fills an impact crater. Lake Cheko may have formed due to a secondary impact onto alluvial swampy ground; the size and shape of the crater may have been affected by the nature of the ground and by impact‐related melting and degassing of a permafrost layer.  相似文献   

Shaking table testing of an existing masonry building: assessment and improvement of the seismic performance          下载免费PDF全文

Nuno Mendes  Paulo B. Lourenço  Alfredo Campos‐Costa 《地震工程与结构动力学》2014,43(2):247-266

This paper aims to assess and improve the seismic performance of an existing masonry building with flexible floors, representative of a Portuguese building typology—‘gaioleiro’ buildings. The study involved seismic tests and dynamic identification tests of two models (nonstrengthened and strengthened) in the shaking table. Each model was subjected to several seismic tests with increasing amplitude. Before the first test and after each seismic test, the dynamic identification of the model was carried out, aiming at obtaining their seismic vulnerability curves based on a damage indicator obtained from the decrease of the frequencies of the modes. In the strengthened model, steel elements were used to improve the connection between walls and floors, together with ties in the upper stories. The results show that adopted strengthening technique is effective for reducing the seismic vulnerability of ‘gaioleiro’ buildings, namely for improving the out‐of‐plane behavior of the facades. Copyright © 2013 John Wiley & Sons, Ltd.  相似文献   

Shaking table testing for masonry infill walls: unreinforced versus reinforced solutions          下载免费PDF全文

Paulo B. Lourenço  João M. Leite  Manuel F. Paulo‐Pereira  A. Campos‐Costa  P. X. Candeias  Nuno Mendes 《地震工程与结构动力学》2016,45(14):2241-2260

Several factors influence the behaviour of infilled frames, which have been a subject of research in the past with moderate success. The new generation of European design standards imposes the need to prevent brittle collapse of the infills and makes the structural engineer accountable for this requirement, yet it fails to provide sufficient information for masonry infills design. Therefore, the present work aims at understanding the seismic behaviour of masonry infill walls within reinforced concrete frames, using both unreinforced and reinforced solutions (bed joint reinforcement and reinforced plaster). For this purpose, three reinforced concrete buildings with different infill solutions were constructed at a scale of 1:1.5, all with the same geometry, and were tested on the shaking table of the National Laboratory for Civil Engineering, Portugal. All solutions performed adequately for the design earthquake, with no visible damage. Still, the experimental tests show that the double‐leaf‐unreinforced infill walls underperformed during a large earthquake, collapsing out of plane by rotating as rigid bodies with multiple configurations. Also the reinforced concrete buildings collapsed, because of the adverse interaction with the infill walls. The infill walls with bed joint reinforcement and reinforced plaster did not collapse out of plane, because of their connection to the concrete frame, which is an essential requirement. Copyright © 2016 John Wiley & Sons, Ltd.  相似文献   

Localized algal blooms induced by river inflows in a canyon type reservoir     

Vidal  Javier  Marcé  Rafael  Serra  Teresa  Colomer  Jordi  Rueda  Francisco  Casamitjana  Xavier 《Aquatic Sciences - Research Across Boundaries》2012,74(2):315-327

The local response of the phytoplankton community to river inflow processes was investigated with modeling and field analyses in a long and narrow, stratified reservoir in mid-summer. The river water had high concentrations of phosphorus and nitrogen (ammonium and nitrate) and temperature had large variations at diurnal scales. As a consequence of the large variation in river temperature, the level of neutral buoyancy (the depth where the river water spreads laterally in the reservoir) oscillated between the surface (overflows) during the day, and the depth of the metalimnion (interflows) during the night. The reservoir remained strongly stratified, which favoured the presence of cyanobacteria. It is shown that under these conditions, nutrient-rich river water injected during overflows into the surface layers promoted the occurrence of localized algal blooms in the zones where the overflow mixed with the quiescent water of the reservoir. A series of hydrodynamic simulations of the reservoir were conducted both with synthetic and realistic forcing to assess the importance of river temperatures and wind-driven hydrodynamics for algal blooms. The simulations confirmed that the river inflow was the main forcing mechanism generating the localized bloom.  相似文献   

Three-dimensional modelling of a tidal channel: The Espinheiro Channel (Portugal)     

Nuno Vaz  João Miguel Dias  Paulo Chambel Leitão 《Continental Shelf Research》2009

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Effect of submerged aquatic vegetation on turbulence induced by an oscillating grid   总被引：1，自引：0，他引：1  

Dolors Pujol  Jordi ColomerTeresa Serra  Xavier Casamitjana 《Continental Shelf Research》2010

In wetlands wind-induced turbulence significantly affects the bottom boundary, and the interaction between turbulence and plant canopies is therefore particularly important. The aim of this study is to advance understanding of the impact of this interaction in submerged aquatic vegetation (SAV)¹ on vertical mixing in a fluid dominated by turbulence. Wind-generated turbulence was simulated in the laboratory using an oscillating grid. We quantify the vertical distribution of turbulent kinetic energy (TKE)² above and within different types of vegetation, measured by an acoustic Doppler velocimeter. Experimental conditions are analysed in two canopy models (rigid and semi-rigid) with seven solid plant fractions (SPFs)³, three stem diameters (d)⁴ and three oscillation grid frequencies (f)⁵ and four natural SAVs (Cladium mariscus, Potamogeton nodosus, Myriophyllum verticillatum and Ruppia maritima).  相似文献   

Observations of Centaur 8405 Asbolus: Searching for Water Ice     

Jennifer Romon-MartinMaria A. Barucci  Catherine de BerghAlain Doressoundiram  Nuno Peixinho  François Poulet 《Icarus》2002,160(1):59-65

Near-infrared spectra of Centaur 8405 Asbolus have been obtained, covering the whole rotational period. Complementary photometry and visible spectroscopy have also been performed. The aim of this project was to confirm or refute the water ice detection on one side of Asbolus reported by Kern et al. (2000 Astrophys. J.542, L155-L159). We found no absorption feature at any rotational phase of Asbolus. Our study is the first in-depth investigation of a centaur over a complete rotational period. Our results seem also to indicate that a change in the slope from 0.8 to 1.0 μm may occur in Asbolus spectrum.  相似文献