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61.
62.
Enrique Pérez Rosa González Delgado José M. Vílchez 《Astrophysics and Space Science》2001,277(1):83-86
We perform a detailed measurement of the electron density along two slit position angles in the bright, low metallicity extragalactic HII region NGC 2363. A comparison of the density structures obtained with the two independent diagnostics given by [AIV]4711/4740 and [SII]6716/6731, show that they present both different absolute values and different radial dependencies, with the [AIV] densities reaching up to 1000 cm-3. We explore the implications for the computation of the He abundance. 相似文献
63.
The Baza Fault: a major active extensional fault in the central Betic Cordillera (south Spain) 总被引:2,自引:0,他引:2
P. Alfaro J. Delgado C. Sanz de Galdeano J. Galindo-Zaldívar F. J. García-Tortosa A. C. López-Garrido C. López-Casado C. Marín-Lechado A. Gil M. J. Borque 《International Journal of Earth Sciences》2008,97(6):1353-1365
In the Guadix-Baza Basin (Betic Cordillera) lies the Baza Fault, a structure that will be described for the first time in
this paper. Eight gravity profiles and a seismic reflection profile, coupled with surface studies, indicate the existence
of a NE-dipping normal fault with a variable strike with N-S and NW-SE segments. This 37-km long fault divides the basin into
two sectors: Guadix to the West and Baza to the East. Since the Late Miocene, the activity of this fault has created a half-graben
in its hanging wall. The seismic reflection profile shows that the fill of this 2,000–3,000 m thick asymmetric basin is syntectonic.
The fault has associated seismicity, the most important of which is the 1531 Baza earthquake. Since the Late Tortonian to
the present, i.e. over approximately the last 8 million years, extension rates obtained vary between 0.12 and 0.33 mm/year
for the Baza Fault, being one of the major active normal faults to accommodate the current ENE–WSW extension produced in the
central Betic Cordillera. The existence of this fault and other normal faults in the central Betic Cordillera enhanced the
extension in the upper crust from the Late Miocene to the present in this regional compressive setting. 相似文献
64.
Xavier Romão João Guedes Aníbal Costa Raimundo Delgado 《Bulletin of Earthquake Engineering》2008,6(2):309-333
Probabilistic seismic assessment requires extensive computational effort resulting from variability both in input ground motions
and mechanical properties. Nonetheless, such methodologies are of considerable importance, namely for pre-earthquake disaster
planning or development of retrofitting programs. A framework for the analytical definition of closed form expressions for
exceedance probabilities of structural component limit states, defined by limit values of structural response parameters,
is proposed herein. The definition of these expressions is based on the probabilistic representation of the ground motion
intensity and on the establishment of suitable expressions characterizing the evolution of structural demand with increasing
earthquake intensity. Distinction is made between deformation-based and force-based structural parameters in the definition
of such relations. Within the proposed framework, the limit states are defined by single deterministic thresholds of structural
response quantities at the component level, as defined in structural codes. Different approaches are also discussed to account
for the randomness of the mechanical properties and ground motion input within the proposed methodology. An application of
the assessment of different limit state probabilities of members from a reinforced concrete building is presented, for which
limit states and limit state capacities are defined according to the upcoming Part 3 of the Eurocode 8. Although the presented
application only deals with member chord rotation and shear force limit state probabilities, the proposed methodology can
be generalized to other deformation-based and force-based structural parameters. 相似文献
65.
Sedimentation in the floodplains of the Mekong Delta,Vietnam Part II: deposition and erosion
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Nguyen Nghia Hung José Miguel Delgado Andreas Güntner Bruno Merz András Bárdossy Heiko Apel 《水文研究》2014,28(7):3145-3160
Deposition and erosion play a key role in the determination of the sediment budget of a river basin, as well as for floodplain sedimentation. Floodplain sedimentation, in turn, is a relevant factor for the design of flood protection measures, productivity of agro‐ecosystems, and for ecological rehabilitation plans. In the Mekong Delta, erosion and deposition are important factors for geomorphological processes like the compensation of deltaic subsidence as well as for agricultural productivity. Floodplain deposition is also counteracting the increasing climate change induced hazard by sea level rise in the delta. Despite this importance, a sediment database of the Mekong Delta is lacking, and the knowledge about erosion and deposition processes is limited. In the Vietnamese part of the Delta, the annually flooded natural floodplains have been replaced by a dense system of channels, dikes, paddy fields, and aquaculture ponds, resulting in floodplain compartments protected by ring dikes. The agricultural productivity depends on the sediment and associated nutrient input to the floodplains by the annual floods. However, no quantitative information regarding their sediment trapping efficiency has been reported yet. The present study investigates deposition and erosion based on intensive field measurements in three consecutive years (2008, 2009, and 2010). Optical backscatter sensors are used in combination with sediment traps for interpreting deposition and erosion processes in different locations. In our study area, the mean calculated deposition rate is 6.86 kg/m2 (≈ 6 mm/year). The key parameters for calculating erosion and deposition are estimated, i.e. the critical bed shear stress for deposition and erosion and the surface constant erosion rate. The bulk of the floodplain sediment deposition is found to occur during the initial stage of floodplain inundation. This finding has direct implications on the operation of sluice gates in order to optimize sediment input and distribution in the floodplains. Copyright © 2013 John Wiley & Sons, Ltd. 相似文献
66.
67.
Tamás Mikes Björn Baresel Andreas Kronz Dirk Frei István Dunkl Raimon Tolosana‐Delgado Hilmar Von Eynatten 《地学学报》2009,21(6):495-506
Three independent single‐grain geochronometers applied to detrital minerals from Central Dinaride sediments constrain the timing of felsic magmatism that associated the Jurassic evolution of the Neotethys. The Lower Cretaceous clastic wedge of the Bosnian Flysch, sourced from the Dinaride ophiolitic thrust complex, yields magmatic monazite and zircon grains with dominant age components of 164 ± 3 and 152 ± 10 Ma respectively. A unique tephra horizon within the Adriatic Carbonate Platform was dated at 148 ± 11 Ma by apatite fission track analysis. These consistent results suggest that leucocractic melt generation in the Central Dinaride segment of the Neotethys culminated in Middle to Late Jurassic times, coeval with and slightly post‐dating subophiolitic sole metamorphism. Growth of magmatic monazite and explosive volcanism call for supra‐subduction‐zone processes at the convergent Neotethyan margin. New compilation of geochronological data demonstrates that such Jurassic felsic rocks are widespread in the entire Dinaride–Hellenide orogen. 相似文献
68.
Antonio García-Alix Gonzalo Jiménez-Moreno Francisco J. Jiménez-Espejo Fernando García-García Antonio Delgado Huertas 《Quaternary Research》2014
The Bølling–Allerød interstadial is the closest warm time period to the Holocene. The study of the climate variability during this most recent warm scenario provides a natural record of potential environmental changes related with global temperature variations. Little is known about this interstadial in the Southern Iberian Peninsula. Therefore, the exceptional climatic record of the Otiñar paleo-lake (ca. 14.5–14.0 cal ka BP), provides environmental information about the first part of this interstadial (Bølling) in this key region. Although the studied high-resolution isotopic record point to almost invariant hydrological conditions in the paleo-lake, with little change in the carbon budget and important limestone dissolution, the pollen record shows an increase in forest species that can be interpreted as a warming trend and an increase in humidity during the Bølling in the area. This record is one of the few continental archives that show this climatic trend in Southern Iberia, agreeing with many other regional records from the western Mediterranean. This does not agree with higher latitude records that show an opposite trend. This opposite pattern in precipitation between the western Mediterranean and more northern latitudes could be explained by a persistent and increasing negative NAO mode during the Bølling in this area. 相似文献
69.
Theodor Kostiuk Tilak Hewagama Kelly E. Fast John Annen Guido Sonnabend Juan D. Delgado Richard Achterberg 《Planetary and Space Science》2010,58(13):1715-1723
The Cassini Huygens mission provides a unique opportunity to combine ground-based and spacecraft investigations to increase our understanding of chemical and dynamical processes in Titan’s atmosphere. Spectroscopic measurements from both vantage points enable retrieving global wind structure, temperature structure, and atmospheric composition. An updated analysis of Titan data obtained with the NASA Goddard Space Flight Center’s Infrared Heterodyne Spectrometer (IRHS) and Heterodyne Instrument for Planetary Wind and Composition (HIPWAC) prior to and during the Cassini Huygens mission is compared to retrievals from measurements with the Cassini Composite Infrared Spectrometer (CIRS). IRHS/HIPWAC results include the first direct stratospheric wind measurements on Titan, constraints on stratospheric temperature, and the study of atmospheric molecular composition. These results are compared to CIRS retrievals of wind and temperature profile from thermal mapping data and ethane abundance at 10-15° South latitude, near the equatorial region. IRHS/HIPWAC wind results are combined with other direct techniques, stellar occultation measurements, and CIRS results to explore seasonal variability over nearly one Titan year and to provide an empirical altitude profile of stratospheric winds, varying from ∼50 to 210 m/s prograde. The advantage of fully resolved line spectra in species abundance measurements is illustrated by comparing the possible effect on retrieved ethane abundance by blended spectral features of other molecular constituents, e.g., acetylene (C2H2), ethylene (C2H4), allene (C3H4), and propane (C3H8), which overlap the ν9 band of ethane, and are not resolved at lower spectral resolution. IR heterodyne spectral resolution can discriminate weak spectral features that overlap the ν9 band of ethane, enabling ethane lines alone to be used to retrieve abundance. Titan’s stratospheric mean ethane mole fraction (8.6±3 ppmv) retrieved from IRHS/HIPWAC emission line profiles (resolving power λ?Δλ∼106) is compared to past values obtained from lower resolution spectra and from CIRS measurements (resolving power λ?Δλ∼2×103) and more compatible recent analysis. Results illustrate how high spectral resolution ground-based studies complement the spectral and spatial coverage and resolution of moderate spectral resolution space-borne spectrometers. 相似文献
70.
R. M. González Delgado M. Cerviño L. P. Martins C. Leitherer P. H. Hauschildt 《Monthly notices of the Royal Astronomical Society》2005,357(3):945-960
We present the single stellar population (SSP) synthesis results of our new synthetic stellar atmosphere models library with a spectral sampling of 0.3 Å, covering the wavelength range from 3000 to 7000 Å for a wide range of metallicities (twice solar, solar, half solar and 1/10 solar). The stellar library is composed of 1650 spectra computed with the latest improvements in stellar atmospheres. In particular, it incorporates non-local thermodynamic equilibrium (LTE) line-blanketed models for hot ( T eff ≥ 27 500 K) , and LTE line-blanketed models (Phoenix) for cool (3000 ≤ T eff ≤ 4500 K) stars. Because of the high spectral resolution of this library, evolutionary synthesis models can be used to predict the strength of numerous weak absorption lines and the evolution of the profiles of the strongest lines over a wide range of ages. The SSP results have been calculated for ages from 1 Myr to 17 Gyr using the stellar evolutionary tracks provided by the Geneva and Padova groups. For young stellar populations, our results have a very detailed coverage of high-temperature stars with similar results for the Padova and Geneva isochrones. For intermediate and old stellar populations, our results, once degraded to a lower resolution, are similar to the ones obtained by other groups (limitations imposed by the stellar evolutionary physics notwidthstanding). The limitations and advantages of our models for the analysis of integrated populations are described. The full set of the stellar library and the evolutionary models are available for retrieval at the websites http://www.iaa.csic.es/~rosa and http://www.iaa.csic.es/~mcs/sed@ , or on request from the first two authors. 相似文献