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The problem of the generation of a gravitational wave by an acoustic one is studied in the high-frequency domain for a perfect fluid. The negative result which is found may be of some relevance for astrophysical and cosmological applications.  相似文献   
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Abstract. Silicate grains in space have attracted recently a wide interest of astrophysicists due to the increasing amount and quality of observational data, especially thanks to the results obtained by the Infrared Space Observatory. The observations have shown that the presence of silicates is ubiquitous in space and that their properties vary with environmental characteristics. Silicates, together with carbon, are the principal components of solid matter in space. Since their formation, silicate grains cross many environments characterised by different physical and chemical conditions which can induce changes to their nature. Moreover, the transformations experienced in the interplay of silicate grains and the medium where they are dipped, are part of a series of processes which are the subject of possible changes in the nature of the space environment itself. Then, chemical and physical changes of silicate grains during their life play a key role in the chemical evolution of the entire Galaxy. The knowledge of silicate properties related to the conditions where they are found in space is strictly related to the study in the laboratory of the possible formation and transformation mechanisms they experience. The application of production and processing methods, capable to reproduce actual space conditions, together with the use of analytical techniques to investigate the nature of the material samples, form a subject of a complex laboratory experimental approach directed to the understanding of cosmic matter. The goal of the present paper is to review the experimental methods applied in various laboratories to the simulation and characterisation of cosmic silicate analogues. The paper describes also laboratory studies of the chemical reactions undergone and induced by silicate grains. The comparison of available laboratory results with observational data shows the essential constraints imposed by astronomical observations and, at the same time, indicates the most puzzling problems that deserve particular attention for the future. The outstanding open problems are reported and discussed. The final purpose of this paper is to provide an overview of the present stage of knowledge about silicates in space and to provide to the reader some indication of the future developments in the field. Received 25 April 2002 / Published online 14 November 2002 Send offprint requests to: L. Colangeli e–mail: colangeli@na.astro.it  相似文献   
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In this paper we calculate thegf-values of some transitions ofYii and Zrii to test the reliability of the commonly used values for astrophysical applications. For ZrII we show the inadequacy of the values used at the present time  相似文献   
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Earth, Moon, and Planets -  相似文献   
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Preface     
Earth, Moon, and Planets -  相似文献   
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We have analyzed X-ray images of the solar corona obtained by the S-054 telescope on Skylab, together with H filtergrams from the Catania Astrophysical Observatory and EUV and magnetic data, to study the morphology and the evolution of the coronal structures associated with prominences (coronal cavities).X-ray cavities are associated with prominences and are enclosed by series of loops of hot plasma typically higher than 5 × 109 cm. Helmet streamers can be observed only at very large heights (> 1 solar radius). The cavities show a higher luminosity when prominences have temporarily disappeared. The density in one of these X-ray cavities ( 3 × 108cm–3) is insufficient to allow formation of dense ( 1011 cm–3) prominences by local condensation from the corona.Prominences associated with young (up to three solar rotations) and old (greater than eight) magnetic neutral lines are significantly less stable than those associated with middle-aged neutral lines. Downward bending of the top of the inner magnetic loop, necessary in some models of prominences, is not detected in these X-ray observations. The relevance of these results to models of prominence formation is discussed.Presently at Osservatorio Astrofisico di Arcetri, Firenze, Italy.  相似文献   
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