Evolution and Mass Loss of AGB Stars in the Small Magellanic Cloud     

J.A.D.L. Blommaert  N.R. Trams  K. Okumura  M.A.T. Groenewegen  J.Th. Van Loon  L.B.F.M. Waters  M.R. Cioni  H.J. Habing  A.A. Zijlstra  C. Loup 《Astrophysics and Space Science》1997,255(1-2):399-400

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Chemical Evolution in the Early Universe: Can Damp Lyα Systems Be Spiral Galaxies?     

Ángeles I. Díaz  Mercedes Mollá  Federico Ferrini 《Astrophysics and Space Science》1998,263(1-4):71-74

The distribution of element abundances with redshift in Damped Lyα (DLA) systems can be adequately reproduced by the same models reproducing the halo and disk components of the Milky Way Galaxy at different galactocentric distances. In this sense, DLA systems are well represented by normal spiral galaxies in their early evolutionary stages. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   

Upper‐crustal extension during oblique collision: the Temsamane extensional detachment (eastern Rif,Morocco)     

Guillermo Booth‐Rea  Antonio Jabaloy‐Sánchez  Ali Azdimousa  Lahcen Asebriy  Mercedes Vázquez Vílchez  José Miguel Martínez‐Martínez 《地学学报》2012,24(6):505-512

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Multi-method characterization of DOM from the Turia river (Spain)     

Sergio Navalon  Mercedes Alvaro  Isabel Alcaina  Hermenegildo Garcia 《Applied Geochemistry》2010

Water concentrates from Turia river (1.5 mg L⁻¹ total organic C) obtained by nanofiltration (membrane mass cut-off 90 Da) were fractioned by non-ionic Amberlite resins (DAX8 and XAD4) to afford three samples termed as hydrophobic acid (50%), transphilic acid (24%) and hydrophobic neutral (12%). If a nanofiltration membrane 270 Da mass cut-off is used then about 50% of dissolved organic matter is not retained. These three fractions were characterized by analytical and spectroscopic techniques (¹H NMR, MALDI–TOF-MS, ESI–API-MS, ESI–MS/MS). Overall, these data are compatible with the presence of oligosaccharides, oligopeptides and fatty acids as the main components of dissolved organic matter. Particularly revealing was the information from MALDI–TOF-MS and ESI–MS/MS where series of compounds differing in the number of hexose units were identified. The three fractions have many spectroscopic similarities and, particularly the hydrophobic and transphilic ones, are really almost identical. This similarity in the fraction composition shows that the conventional fractionation procedure is inefficient as a standard general method for separation of different compound types. The composition of dissolved organic matter was confirmed, and some individual organic compounds identified, by GC–MS analysis of the silylated derivatives obtained by reacting the fractions with a mixture of N,O-bis(trimethylsilyl)trifluoroacetamide with trimethylchlorosilane (10%). Thus, rather surprisingly, the dissolved organic matter of this natural raw water is predominantly composed of a relatively simple mixture of a few types of compounds with molecular weights well below 1100 Da (about six hexose units). These results, particularly the absence of detectable amounts of high molecular weight humic acids and low molecular weight phenolic compounds indicates that trihalomethanes formed in the water disinfection process by Cl₂ really derive from oligosaccharides and oligopeptides. Also, the data suggests alternative strategies to effect a more efficient fractionation of the dissolved organic matter.  相似文献   

Galactic evolution along the hubble sequence     

Mercedes MollÁ  Angeles I. DÍaz 《Astrophysics and Space Science》2003,284(2):767-770

A generalization of the multiphase chemical evolution model applied to a wide set of theoretical galaxies is shown. This set of models has been computed by using the so-called Universal Rotation Curve from (Persic, Salucci and Steel, 1996) to calculate the radial mass distributions of each theoretical galaxy. By assuming that the molecular cloud and star formation efficiencies depend on the morphological type of each galaxy, we construct a bi-parametric grid of models whose results are valid in principle for any spiral galaxy, of given maximum rotation velocity or total mass, and morphological type. This revised version was published online in August 2006 with corrections to the Cover Date.  相似文献   

Radial Gradients of Abundances     

Mercedes Mollá  Angeles I. DÍaz  F. Ferrini 《Astrophysics and Space Science》2002,281(1-2):141-142

We have computed a set of multiphase chemical evolution models in which the radial mass distributions of each theoretical galaxy is calculated using the universal rotation curve from Persic, Salucci and Steel (1996). We obtain the chemical evolution for galaxies of different masses and morphological types by changing the efficiencies to form molecular clouds and stars according with these types. We obtain the radial distributions of diffuse and molecular gas densities, the star formation rate and abundances for 15 elements for each galaxy. This revised version was published online in September 2006 with corrections to the Cover Date.  相似文献   

http://www.sciencedirect.com/science/article/pii/S1674987113000029   总被引：1，自引：0，他引：1  

Daniel A. Gregori  Jose Kostadinoff  Guillermina Alvarez  Ariel Raniolo  Leonardo Strazzere  Juan C. Martinez  Mercedes Barros 《地学前缘(英文版)》2013,4(6):693-708

The Preandean geological configuration of the eastern North Patagonian Massif is established through the use of geological and geophysical analysis.The positive gravity anomalies located near the Atlantic coast are due to 535 and 540 Ma old rocks belonging to the Pampean Orogeny （Precambrian-middle Cambrian）,which are widely recognized in central and northern Argentina.The Famatinian Cycle （Ordovician-Devonian） is represented by a Silurian-Devonian marine basin equivalent to those of eastern-central Argentina and South Africa,and which was deformed at the end of the Devonian byan～E-W to WNW-ESE compressional event,part of the Famatinian Orogeny.Containing strong gravity gradients,the NW-SE belt is coincident with fault zones which were originated during the Gondwanide Orogeny.This event also produced NW-SE overthrusting of the Silurian-Devonian sequences and strike-slip faults that displaced blocks in the same direction.This deformation event belongs to the Gondwanide Orogeny that includes movements related to a counterclockwise rotation of blocks in northern Patagonia.The strong negative anomalies located in the western part of the area stem from the presence of rocks of the Jurassic Ca（n）adón Asfalto basin interbedded in the Marifil Complex.These volcaniclastic sequences show mild deformation of accommodation zones in a pre-Jurassic paleorelief.  相似文献   

An evaluation of ontology matching techniques on geospatial ontologies     

Francisco Delgado  M. Mercedes Martínez-González  Javier Finat 《International journal of geographical information science》2013,27(12):2279-2301

Standardization is one of the pillars of interoperability. In this context, efforts promoted by the Open Geospatial Consortium, such as CityGML (Technical University, Berlin), a standard for exchanging three-dimensional models or urban city objects, are welcomed. However, information from other domains of interest (e.g. energy efficiency or building information modeling) is needed for tasks such as land planning, large-scale flooding analysis, or demand/supply energy simulations. CityGML allows extension in order to integrate information from other domains, but the development process is expensive because there is no way to perform it automatically. The discovery of correspondences between CityGML concepts and other domains concepts poses a significant challenge.

Ontology matching is the research field emerged from the Semantic Web to address automatic ontology integration. Using the ontology underlying CityGML and the ontologies which model other domains of interest, ontology matching would be able to find the correspondences that would permit the integration in a more automatic manner than it is done now.

In this paper, we evaluate if ontology matching techniques allow performing an automatic integration of geospatial information modeled from different viewpoints. In order to achieve this, an evaluation methodology was designed, and it was applied to the discovery of relationships between CityGML and ontologies coming from the building information modeling and Geospatial Semantic Web domains. The methodology and the results of the evaluation are presented. The best results have been achieved using string-based techniques, while matching systems give the worst precision and recall. Only in a few cases the values are over 50%, which shows the limitations when these techniques are applied to ontologies with a partial overlap.  相似文献   

Removal of Phenol by Immobilization of Trametes versicolor in Silica–Alginate–Fungus Biocomposites and Loofa Sponge          下载免费PDF全文

Maira Carabajal  Mercedes Perullini  Matias Jobbágy  René Ullrich  Martin Hofrichter  Laura Levin 《洁净——土壤、空气、水》2016,44(2):180-188

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The Puesto Piris Formation: Evidence of basin-development in the North Patagonian Massif during crustal extension associated with Gondwana breakup     

Leonardo Strazzere  Daniel A. Gregori  Leonardo Benedini  Paulo Marcos  Mercedes V. Barros  Mauro C. Geraldes  Cecilia Pavon Pivetta 《地学前缘(英文版)》2019,10(1):299-314

The Marifil Volcanic Complex, exposed in the eastern North Patagonian Massif, Argentina, includes up to 550 m of red conglomerates, sandstones, black siltstones, limestones, and reworked tuff of the Puesto Piris Formation. The basal part of this unit, which was deposited in high-gradient topographic relief, is composed of conglomerates and sandstones with thin layers of reworked tuffs. The lithofacies associations of the basal part indicate that the depositional mechanisms were mantled and gravitational flows.The middle part of the unit consists of fine sandstones, limestones, and black siltstones that were deposited in low-energy fluvial and lacustrine environments. The outcrops are located along the NEe SW direction and the major thickest units represented by limestones and siltstones, occur near the southeastern border of this NEeS W depocenter. Since the rhyolitic and trachytic lava flows and tuffs of the Marifil Volcanic Complex are interbedded with the sedimentary sequences of the Puesto Piris Formation,both units are coeval. Zircon Ue Pb age was obtained for a trachytic lava flow(193.4 ±3.1 Ma) suggesting that sedimentation and volcanism are Sinemurian. This extensional episode was recorded in the eastern,western, and southwestern sectors of the North Patagonian Massif, and is possibly associated with the Gondwana supercontinent breakup.  相似文献