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  • Electronic Resource  (19)
  • 1980-1984  (11)
  • 1960-1964  (6)
  • 1900-1904  (2)
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  • Electronic Resource  (19)
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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    The European physical journal 171 (1963), S. 403-415 
    ISSN: 1434-601X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Description / Table of Contents: Zusammenfassung 1. Der aus dem Spektrum der Photoneutronen aus C12 zu ermittelnde Wirkungsquerschnitt für C12 (γ, n 0) C11 stimmt in seinem Verlaufe im wesentlichen mit dem Wirkungsquerschnitt für C12 (γ, n) C11 überein, enthält aber darüberhinaus deutliche Anzeichen einer komplexen Struktur. 2. Der aus dem Spektrum der Photoneutronen aus O16 ermittelte Wirkungsquerschnitt für O16 (γ, n 0) O15 stimmt mit dem Neutronenerzeugungsquerschnitt überein und zeigt wie dieser zwei ausgeprägte Linien, die mit den bereits aus der Untersuchung der Protonenspektren, der Totalabsorption vonγ-Quanten und der Reaktion N15 (p, γ 0) O16 bekannten Resonanzen imγ-Absorptionswirkungsquerschnitt beiE=22,2 und 24,2 MeV übereinstimmen. 3. Sowohl bei C12 als auch bei O16 stimmt $$\sigma _{(\gamma ,n_0 )} $$ mit $$\sigma _{(\gamma ,p_0 )} $$ in der Form — d.h., soweit erkennbar, auch in der Feinstruktur — wie im absoluten Betrage überein. 4. Bei der (γ, n)-Reaktion an C12 und O16 überwiegen die Übergänge zu den Grundzuständen der Folgekerne.
    Notes: Abstract The (γ, n)-reactions on carbon and oxygen were studied using the 30,5 MeV brems-strahlung beam of the Heidelberg betatron. The photoneutrons were detected via the recoil protons in a stilbene scintillator. The pulse height spectrum of scintillations produced in the stilbene crystal by the recoil protons is analyzed to yield the incident neutron energy distribution. Theγ-ray and electron background was strongly reduced through pulse shape discrimination. To test the apparatus the spectrum of the neutrons from a Po-α-Be source was measured. The energy spectrum of the photo-neutrons from O16 shows clearly two peaks at excitation energies of 22,4 and 24,4 MeV also seen in the photo-proton spectra. The energy distribution of the neutrons from C12 (γ, n) too contains indication of structure already known from the proton spectra from C12 (γ, p). The derived cross sections of C12 (γ, n 0) and O16 (γ, n 0) coincide as well in their shape as in their absolute magnitude with the corresponding (γ, p 0)-cross sections. In both C12 (γ, n) and O16 (γ, n)-reaction the neutrons seem to leave the final nucleus mainly in its ground state.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    The European physical journal 309 (1982), S. 183-184 
    ISSN: 1434-601X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Mass distributions of fission-like fragments from the system 271 MeV40Ar+165Ho have been measured as a function of the angle. An expected dependence of the mass distribution width on angle due to the claimed contribution of “fast fission” could not be observed.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    The European physical journal 315 (1984), S. 1-11 
    ISSN: 1434-601X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Using the atomic beam magnetic resonance method, precision measurements of the hyperfine structure and Zeeman interactions have been performed in the ground state 4f 126s 2 3 H 6 of167Er. The experimental data were analyzed using an effective operator parametrized in the space of states of the ground state multiplet. It yielded eight effective hyperfine structure and Zeeman interaction constants which served to calculate the seven hyperfine separations of the ground state. The results are: $$\begin{gathered} 2F 2F' v_{FF'} (MHz) \hfill \\ 5 7 - 354.371 9409 (27) \hfill \\ 7 9 - 2{\text{78}}{\text{.231}} {\text{8263(14)}} \hfill \\ {\text{9}} 11 - 69.050 7785 (4) \hfill \\ 11 13 + 302.735 3731(12) \hfill \\ 13 15 + 866.691 3871(10) \hfill \\ 15 17 + 1,652.383 5154 (6) \hfill \\ 17 19 + 2,689.380 8050(10) \hfill \\ \end{gathered}$$ From the effective Zeeman interaction constants it was possible to determine an improvedg I -value, uncorrected for atomic diamagnetism: $$ g_I = + 0.086 775 (19) \cdot 10^{ - 3}$$ Furthermore a hexadecapole interaction corresponding to a diagonal hexadecapole interaction constant $$A_4 = - 16 (10) Hz$$ could be established which is of the order of magnitude expected from Coulomb excitation experiments as well as theoretical calculations.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    The European physical journal 174 (1963), S. 227-230 
    ISSN: 1434-601X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract The neutrons from a Po-α-Be source were detected via the recoil protons in a stilbene scintillator. The pulse height spectrum of the scintillations produced in the stilbene crystal by the recoil protons is analysed to yield the incident neutron energy distribution. Theγ-ray background was eliminated through pulse shape discrimination. Separately the spectrum of neutrons coincident withγ-rays, i.e. of neutrons from the Be9(α,n)C12* reaction, has been determined. The resulting spectra are compared to previous measurements. The structure of the spectra is not compatible with an isotropic angular distribution of the neutrons relative to theα-direction. Furthermore it could be shown that the fraction of reactions leading to the 7,65 MeV state of C12 is only about 10−3.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    The European physical journal 165 (1961), S. 485-490 
    ISSN: 1434-601X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Li2CO3 and Na2C4H8O8 have been irradiated by 34 MeV bremsstrahlung. The yield of the induced O15 activity has been measured relative to the yield of the C12(γ, n)C11 resp. Cu63(γ, n)Cu62 reaction by detecting the annihilation quanta. Additional yield measurements with the bremsstrahlung beam attenuated by 18 mm of lead were made to determine the ratio of the integrated cross sections for the reactions O16(γ, n)O15 and C12(γ, n)C11 resp. Cu63(γ, n)Cu62. Using the cross section ofBarber et al. for C12(γ, n)C11, the cross section integrated up to 33 MeV for O16(γ, n)O15 was obtained to 61±7 MeVmb.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1434-601X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Angular and energy correlations betweenα-particles and quasi-elastic projectile-like heavy ions have been measured for36Ar+197Au collisions atE LAB=380MeV. The majority of the observed coincident events can be understood in terms of a statistical emission process whereas only a small fraction of the events, mainly at forward angles, can be attributed to a direct process.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1434-601X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract The number and energy spectra of neutrons evaporated by the heavy and light fragments in deep inelastic collisions have been obtained for the system 240 MeV40Ar +197Au. They indicate that at the scission point the deformation energy is a large part of the total excitation energy espe cially for the light fragment. In the last two years, neutron emission has been studied in deep inelastic reactions1−6. All the results are similar: the incident energy which is lost during the process is transformed into excitation energy of the final fragments and is shared between the two products proportionnally to their masses. This means that the nuclear temperature was uniform in the composite system. The excitation energy equilibration time is really very short since equilibration is achieved after reaction times as small as 10−22 s2,6. Moreover, no preequilibrium emission (direct neutrons-) has been observed.
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1434-601X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Angular and energy correlations betweenα-particles and deep-inelastic projectile-like fragments were measured for the system36Ar+197Au atE Lab=380 MeV. At most half of the coincident events can be attributed to statistical emission ofα-particles from the fully accelerated projectile-like fragments. The remainder of the events may be due to direct emission during the first 10−22 s of the scattering process and to preequilibrium processes taking place within some 10−21 s.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    The European physical journal 314 (1983), S. 143-147 
    ISSN: 1434-601X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract For the reaction 290 MeV20Ne+197Au the number of neutrons emitted in coincidence withα-particles is used to discriminate between two equally important but qualitatively different mechanisms for the emission of fastα-particles. They are connected with low and high inelasticity, respectively, and the resultingα-particles differ in mean velocity and velocity distribution.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Mineralogy and petrology 27 (1980), S. 233-260 
    ISSN: 1438-1168
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Summary The extensive siderite mineralization of the Hüttenberg deposit is restricted to marble series of the “Saualm Crystalline”. The Ordovician to Devonian age of this metamorphic complex and its Variscan structure is well substantiated. Large-scale tectonic investigations show that the main directions of the B-axes of all types of rocks occurring within the deposit have the same directions. This is also confirmed by investigations of the grain texture: B- as well as S-tectonite orientation can be found. The macroscopically visibles is also attributed to this strong Variscan folding as (h0l)-plane. The axial directions which can be inferred from this orientation coincide exactly with the Variscan large-scale and small-scale folds. Influence of a pre-Variscan or Alpidic phase can also be observed. There is also a distinct orientation of growth fabric. No clear conclusions could be drawn, however, as to their origin. The detection of metasomatic processes neither gives any information as to the process of enrichment nor does it mean that the entire content of the deposit has been added by metasomatic exchange of matter. It is concluded that a mobilization of already existing iron has taken place during the Variscan orogenesis. Such depositional processes could be released to a minor extent only by the fracture tectonics of the Alpidic orogenesis. Thus, quantitative evidence is provided for the first time to show that this “metasomatic” deposit has, in fact, been derived from pre-metamorphic sedimentary iron concentrations.
    Notes: Zusammenfassung Die mächtigen Sideritvererzungen der Lagerstätte Hüttenberg sind auf Marmorzüge des Saualmkristallins beschränkt, dessen ordovizisch-silurisch-devonisches Alter und dessen durch die variszische, synmetamorphe Orogenese geprägter Bau heute als weitgehend gesichert angesehen wird. Großtektonische Untersuchungen zeigen, daß die B-Achsenhauptrichtungen aller im Bereich der Lagerstätte auftretenden Gesteinstypen, einschließlich derer der vererzten Partien, gleichgerichtet sind. Das wird auch durch die Korngefügeuntersuchungen bestätigt: deutlich tritt sowohl eine B- wie auch S-Tektonitregelung hervor, wobei dieser starken Formung auch das makroskopisch sichtbares als (h0l)-Fläche zuordenbar ist und die aus der Tektonitregelung erschließbaren Achsen in ihrer Richtung mit den variszisch angelegten Groß- und Kleinfalten übereinstimmen. Eine die variszische Orogenese überdauernde Thermometamorphose hat die bestehenden Regelungen nicht verwischt, ein Einfluß einer vorvariszischen oder einer alpidischen Phase ist im Korngefüge nicht nachweisbar. Erhalten sind auch Wachstumsgefügeregelungen, die aber wegen ihrer Mehrdeutigkeit keine klaren Schlußfolgerungen über ihre Entstehung erlauben. Die Korngefügeuntersuchungen bestätigen auch, daß der Metasomatose bei der Ausbildung der Lagerstätte in ihrer heutigen Form eine wesentliche Rolle zukommt. Der Nachweis metasomatischer Prozesse sagt aber nichts über den eigentlichen Eisenanreicherungsvorgang aus und bedeutet keinesfalls, daß der Lagerstätteninhalt durch metasomatischen Stoffaustausch zugeführt wurde. Es wird vielmehr auf eine Mobilisation schon primär vorhandenen Eisens durch Druck- und Temperaturerhöhung während der variszischen Orogenese und der damit verbundenen Thermometamorphose geschlossen; die Bruchtektonik der alpidischen Gebirgsbildungsphase konnte solche lagerstättenbildende Prozesse nur mehr in geringem Maß auslösen.
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