The 11.5 micrometer emission from carbon stars: Comparison with IR spectra of submicrometer-sized silicon carbide grains     

C. Friedemann  J. Gürtler  Regina Schmidt  J. Dorschner 《Astrophysics and Space Science》1981,79(2):405-417

In this paper the results of an experimental investigation of the spectra of submicrometersized silicon carbide grains are presented. The grains manufactured from two types of commercial -SiC were prepared according to the Jena IR spectroscopy program for particulates of cosmic importance. From the spectral records mass absorption coefficients have been derived. These data have been used to make a comparison of the laboratory spectra with the well-known 11.5 m emission band observed in the spectra of carbon stars, which is probably due to a transition in circumstellar SiC grains. For this aim, a simple model of an optically thin circumstellar envelope containing SiC grains has been calculated. The theoretical profile of the 11.5 m band derived by means of this model and based on the experimental mass absorption coefficients of SiC grains shows a striking similarity with the observed profile in the spectrum of the carbon star Y CVn. The total amount of SiC dust in the envelope of this star has been estimated at about 10²⁴ g.  相似文献   

Bycatch: complementary information for understanding fish behaviour. Namibian Cape hake (M. capensis and M. paradoxus) as a case study     

Gordoa  Ana; Lesch  Heinrich; Rodergas  Silvia 《ICES Journal of Marine Science》2006,63(8):1513-1519

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Geometry and evolution of Holocene transgressive and regressive barriers on the semi-arid coast of NE Brazil     

Luciano Henrique de Oliveira Caldas  Josibel Gomes de Oliveira Jr  Walter Eugênio de Medeiros  Karl Stattegger  Helenice Vital 《Geo-Marine Letters》2006,26(5):249-263

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Do endocrine disrupting chemicals threaten Mediterranean swordfish? Preliminary results of vitellogenin and Zona radiata proteins in Xiphias gladius     

M. Cristina Fossi  Silvia Casini  Stefania Ancora  Alessandra Moscatelli  Antonella Ausili  Giuseppe Notarbartolo-di-Sciara 《Marine environmental research》2001,52(5)

Endocrine Disrupting Chemicals (EDCs) have the potential to alter hormone pathways that regulate reproductive processes in wildlife and fishes. In this research the hypothesis that Mediterranean top predator species (such as large pelagic fish) are potentially at risk due to EDCs is investigated. These marine organisms tend to accumulate high concentrations of EDCs such as polyhalogenated aromatic hydrocarbons (PHAHs). The potential effects of EDCs on a fish species of commercial interest, the top predator Xiphias gladius (swordfish), were investigated using vitellogenin (Vtg) and Zona radiata proteins (Zrp) as diagnostic and prognostic biomarkers. Dramatic induction of typically female proteins (Vtg and Zrp) was detected by ELISA and Western Blot in adult males of the species. These results are the first warning of the potential risk for reproductive function of Mediterranean top predators, and suggest the need for continuous monitoring of this fragile marine environment.  相似文献   

Documentary sources of the sea surges in Venice fromad 787 to 1867     

Silvia Enzi  Dario Camuffo 《Natural Hazards》1995,12(3):225-287

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Recent observations of the WR central star of the planetary nebula LMC-N66     

Miriam Peña  Manuel Peimbert  Silvia Torres-Peimbert  Maria Teresa Ruiz  Jose Maza 《Astrophysics and Space Science》1996,238(1):55-58

The recent evolution of the central star of the planetary nebula LMC-N66 is presented. Before 1987, it showed a weak continuum with aT _eff120 000 K andL _bol25 000L and in a few years it developed strong WR features (P Cygni line profiles in N v at 124.0 nm and C IV at 155.0 nm, wide Heii emission, etc.) typical of a WN 4.5. Additionally the stellar continuum increased by a large factor and the absolute visual magnitude of the star changed from + 1.24 in 1987 to–2.57 in January, 1995. The WR features and enhanced continuum, evidencing a powerful mass-loss event remained with small variations for more than 5 years. Recent ultraviolet and optical data shows that the mass-loss seems to have diminished abruptly in the last three months.  相似文献   

Depth of the brittle-ductile transition in a transcurrent boundary zone     

Michele Dragoni  Silvia Pondrelli 《Pure and Applied Geophysics》1991,135(3):447-461

A model is proposed which describes the boundary zone between two transcurrent plates as a viscoelastic body, with rheological properties changing with depth. In this model, the brittle-ductile transition is defined as the depth at which the time derivative of shear stress changes from positive to negative values. Variations of this depth are studied as functions of geothermal gradient, rheological parameters and strain rate, using a power law rheology with exponent ranging from 1 to 4. Stress relaxation in the ductile zone is controlled by a local characteristic time, which depends on petrology, temperature and, in the case of non-Newtonian rheology, on strain rate. The composition and the hydration degree of crustal rocks may also sensibly influence the depth of the brittle-ductile transition. The model predictions are compared with observations regarding the San Andreas, Imperial Valley and North Anatolian Faults: it is found that values ofn from 1 to 3 are more appropriate to reproduce the transition depth inferred by the seismicity distribution.  相似文献   

Trace element distribution in annual stalagmite laminae mapped by micrometer-resolution X-ray fluorescence: Implications for incorporation of environmentally significant species   总被引：3，自引：0，他引：3  

Andrea Borsato  Silvia Frisia  Andrea Somogyi  Jean Susini 《Geochimica et cosmochimica acta》2007,71(6):1494-1512

Stalagmite ER78, from Grotta di Ernesto cave in NE Italy displays clear annual lamination consistent with its shallow depth below a forest ecosystem subject to autumnal peaking of water infiltration. Synchrotron radiation scanning micro-X-ray fluorescence analyses of heavy elements at European Synchrotron Radiation Facility beamline ID22, and light elements at ID21, with 1-3 μm resolution has been combined with data from ion microprobe analyses to reveal chemical variability across the visible layers of these annual laminae. A series of elements display a symmetrical peak, centered around the thin, dark layer at the top of each lamina. The peak concentration is ordered Y > Zn, Cu and Pb > P and Br. This hierarchy is thought to reflect the selectivity of transport of these elements, possibly by organic colloids flushed from the soil zone during autumn infiltration. Ion microprobe analysis indicates Na and F also increase, as does H, the latter reflecting increased microporosity. Sr displays a trough around the dark and thin autumn layer implying that its incorporation may be limited by competition with other elements. Mg and S show a different pattern of annual variation and Fe displays none. The trace metals, Br and Y display peak abundance in the early 20th century, which appears to reflect a period of tree-felling rather than a climatic anomaly. The results demonstrate the power of the high spatial resolution and low detection limits of the synchrotron technique, and its ability to produce quantitative maps that allow distinction of layered structure from that of isolated particles, or irregular inhomogeneities.  相似文献   

Palynological biozones and radiometric data at the Carboniferous–Permian boundary in western Gondwana     

Silvia N. Csari 《Gondwana Research》2007,11(4):529-536

Absolute radiometric data obtained recently in Upper Paleozoic basins of South America and Southern Africa are available to constrain the age of some palynological biozones defined in the Western Gondwana. Some dates obtained from Argentina coincide with southern Africa's and are useful to constrain the palynological associations. In this way, the Permian Argentinian Lueckisporites–Weylandites (LW) Biozone is compared with the Lueckisporites virkkiae Biozone of Brazil and Zone 3 of South Africa. On the other hand, the palynofloras from Dwyka (South Africa) are comparable with Argentinian and Brazilian associations recovered near the Carboniferous–Permian boundary. Tuffaceous intervals of the Dwyka Group in South Africa suggest the beginning of that sequence at 307 Ma reaching the 290 Ma at the top. The available palynological, paleoenvironmental and radiometric data from these three western Gondwanan areas are analyzed and compared.  相似文献   

Precise hypocentre relocation of microearthquakes in a high-temperature geothermal field: the Torfajökull central volcano, Iceland     

Regina Lippitsch  Robert S. White  Heidi Soosalu 《Geophysical Journal International》2005,160(1):371-388

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