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  • 1
    Digitale Medien
    Digitale Medien
    Springer
    Space science reviews 1 (1963), S. 589-611 
    ISSN: 1572-9672
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Physik
    Notizen: Conclusions Since all the models referred to above reproduce observations of zodiacal light, but vary considerably in their composition, it is clear that the ambiguities must be resolved if we are to achieve a reliable description of interplanetary matter. For such purpose we must acquire additional information on the following aspects of the problem: a) Scattering functions of non-spherical particles, studied either by optical or microwave experiments using particles in form and refractive index similar to the micrometeorites collected by sounding rockets. b) Brightness and polarization of zodiacal light obtained by sounding rockets and satellites. All ground measurements are disturbed by terrestrial airglow, but this difficulty will be overcome by measurements made from altitudes 〉 150 km. In addition to their greater reliability in representing zodiacal light, such observations will provide data within the regions of elongation between the corona and 20° and from 90° to 180°, as et almost unobserved. Any marked deviation of the observations from the prediction by the models referred to above would have importance for further study. c) Particle counts and electron density measurements by deep space probes. Although space probes can provide only samples, results will be significant for obtaining a better estimate of both numbers of electrons and the presence of small particles in interplanetary space. Especially must we determine whether there is only a cloud of small particles around the earth (Whipple, 1961b) or whether the submicron particles, as collected by Soberman et al., are spread out over a major region of the solar system. Such a solution would justify the application of Type III models. On the basis of the information outlined above, we might possibly find by optical methods models which, combined with our knowledge of the particulate content of space derived from meteorites and mechanical considerations (see Whipple, 1962a), would greatly enhance our understanding of the interplanetary media Such models might be similar to Type III but with a spatial variation in particle size and density distribution which also takes into consideration the properties of the Corona. It must be emphasized, however, that the present measurements and analyses do not warrant reliable conclusions about the electron density.
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Digitale Medien
    Digitale Medien
    Springer
    Physics and chemistry of minerals 17 (1991), S. 611-616 
    ISSN: 1432-2021
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Chemie und Pharmazie , Geologie und Paläontologie , Physik
    Notizen: Abstract The components of the interfacial surface tension of talc and pyrophyllite were determined by measuring the rate of the capillary rise of a number of liquids through thin, sedimented deposits of the powdered minerals. The rate of capillary rise of a liquid in a powder is related to the contact angle between the liquid and the solid by the Washburn equation. The contact angles thus derived were used to determine the apolar (Lifshitzvan der Waals) component, γ LW , and the polar, electronacceptor and electron-donor parameters, γ ⊕ and γ ⊖ respectively, of the Lewis acid/base component of the total interfacial surface energy using the Young equation. The values of γ LW for talc and pyrophyllite (31.5 and 34.4 mJ/m2) are slightly smaller than for smectite clay minerals (e.g., the value for hectorite is 39.9 mJ/m2), the electron donor parameter values are roughly comparable for talc and pyrophyllite (γ ⊕ = 2.4 and 1.7 mJ/m2) as are the values of the electron acceptor parameter (γ ⊖ = 2.7 and 3.2 mJ/m2). The well-known hydrophobicity of these two minerals is due to the remarkably small value (for silicate minerals) of γ ⊖(γ⊕ is normally small or zero for silicates and many other oxides). The small values of both γ ⊕ and γ ⊖ mean that the Lewis acid/base interactions between talc or pyrophyllite and highly polar water molecules are very weak. In contrast, low-charge smectites, the minerals most similar chemically and structurally to talc and pyrophyllite, have much greater values of γ ⊖ (≥ 30 mJ/m2) and are hydrophyllic.
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Digitale Medien
    Digitale Medien
    Springer
    Astrophysics and space science 15 (1972), S. 401-403 
    ISSN: 1572-946X
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Physik
    Notizen: Abstract Corrected values of the efficiency factorQ pr of light pressure are presented for spherical particles of graphite and metallic materials.
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    ISSN: 1572-9672
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Physik
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 5
    Digitale Medien
    Digitale Medien
    Springer
    Fresenius' Zeitschrift für analytische Chemie 307 (1981), S. 127-128 
    ISSN: 1618-2650
    Schlagwort(e): Best. von Wasser in Kieselgel ; Röntgenfluorescenz-Spektrometrie
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Chemie und Pharmazie
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
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