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  • 1
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 171 (1953), S. 38-39 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The starting point was to consider continuous machine drawing in terms of a three-dimensional load-extension-temperature surface characteristic of the material, which during most of our investigation has been polyethylene terephthalate ('Terylene'). A 'contour map' for such a surface for this ...
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 176 (1955), S. 78-79 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Fig. 1. Calculated amorphous density (gm./c.c.) vs. percentage crystallinity ^, Production 'Terylene' polyester yarns ; A, Production 'Terylene' polyester yarns (heat-set); , yarns spun at low speed; O, yarns spun at high speed; o. 8, El, other experimental yarns; (g, unoriented crystalline ...
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  • 3
    Electronic Resource
    Electronic Resource
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Earth and Planetary Sciences 2 (1974), S. 179-212 
    ISSN: 0084-6597
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Journal of fish biology 48 (1996), S. 0 
    ISSN: 1095-8649
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Larvae and pupae of Chaoborus edulis may be the most important food resource of some deep-water demersal fish species in southern Lake Malawi. C. edulis feed on crustacean zooplankton, which in turn feed on phytoplankton. Hence, demersal fish production is supported directly by planktonic primary production, rather than through a detrital food chain.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 115 (1993), S. 225-241 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Melting experiments were performed on a natural mica-amphibole-rutile-ilmenite-clinopyroxene (MARID) sample from the Kaapvaal mantle lithosphere (AJE137) at 20 to 35 kbar and 800 to 1450°C. A solidus was determined at 1260°C and 30 kbar above which phlogopite, clinopyroxene and olivine were stable with an alkali-rich silicate melt. Olivine is the only crystallizing phase just below the liquidus of the AJE137 bulk composition and K-richterite was only stable in the subsolidus region (≤ 1100°C at 30 kbar). These results are consistent with previous studies in more simple systems. In experiments with 10 wt% added water the solidus was depressed by ca. 300°C and K-richterite was stabilized above this solidus. MARIDs represent a potential lowtemperature component in the lithospheric mantle beneath the Kaapvaal Craton of southern Africa. The addition of 〉 10 wt% water (with less than a 120°C rise of temperature above the geotherm) to this mantle region would create conditions for the melting of this component. This may then be incorporated in any continental flood basalt parent magma that traverse this lithospheric mantle. The derivation of MARIDs from a silicate melt of their bulk composition, even if water saturated, is considered unlikely as such small degree melts could not sustain the elevated liquidus temperatures required (〉 1200°C at 30 kbar) in a cold (〈 800°C at 30 kbar) mantle lithosphere. MARID xenoliths may be produced by the interaction of an alkali-rich fluid with a peridotite or as the residue to a group II kimberlitic parent magma that has undergone fractionation of olivine and the exsolution of a carbonatite component.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The phase relations of divariant and trivariant assemblages involving combinations of phengite, chlorite, biotite, K-feldspar, quartz and H2O in the KFASH, KMASH and KFMASH systems were calculated using a single thermodynamic data set (Holland and Powell 1998). The stability fields of the various equilibria are represented in P-T projections by contouring sets of compositional isopleths for the Tschermak (Al2(Fe,Mg)−1Si−1) and FeMg−1 exchanges controlled by the coexisting phases. Five multivariant continuous equilibria, which occur in different regions of P-T-X space, are calibrated as thermobarometers in metamorphic rocks of pelitic to quartzofeldspathic composition. More subtle P-T information, relating to the trajectories (dT/dz) along which reacting rocks have been buried or exhumed, can be extracted from the continuous reactions by investigating the recorded compositional trends in the Al2(Fe,Mg)−1Si−1 and FeMg−1 solutions. Singularities in P-T space are associated with some of these reactions and may result in unusual mineral textures and compositional trends. A fluid-absent singularity has particular petrological significance because it marks the transition between hydration and dehydration along a single reaction with increasing pressure and temperature. This behaviour causes the sequence of reactions among these minerals observed during metamorphism to be critically dependent on the P-T trajectory. Thermobarometric calculations show good agreement with respect to experimental and field-based data for phengite compositions less than about 50 mol% celadonite (〈∼3.5 Si p.f.u. phengite).
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Hoboken, NJ : Wiley-Blackwell
    Journal of Polymer Science 34 (1959), S. 741-760 
    ISSN: 0022-3832
    Keywords: Chemistry ; Polymer and Materials Science
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Physics
    Notes: Although crystallization under stress occurs in nearly all synthetic fiber making, giving fine fibrillar fiber structures, it has been relatively little studied; and the literature, centered mainly round coarser spherulitic crystallization, does not take us very far in understanding it. However, a simple experiment shows that it is very important. If a filament of amorphous polyethylene terephthalate is stretched over a hot plate between two roller moving at different speeds, stretching can take place either without crystalization at low tension, or with considerable crystallization at high tension, at the same temperature and speed, simply according to the method of starting the machine. A model visco-elastic theory based on Maxwell's equation is, therefore, developed to describe this behaviour using the simplest possible assumptions. Further experiments then show that this simple and partly empirical theory fits the observed behaviour of polyethylene terephthalate reasonably well, and the simple assumptions made, therefore, seem to give a first approximation to the course of strain induced crystallization. They correspond with the idea of exremely rapid crystallization from a nucleus to a small structural unit, the density of nucleation being dependent on the stress. Parallel work on the streching of spherulitic structures is then mentioned, and it is finally suggested that stress induction and rapid growth to a small structural unit may be common to both spherulitic crystallization under internal stresses, and fibrillar crystallization under an externally applied stress.
    Additional Material: 12 Ill.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Hoboken, NJ : Wiley-Blackwell
    Journal of Polymer Science 37 (1959), S. 313-315 
    ISSN: 0022-3832
    Keywords: Chemistry ; Polymer and Materials Science
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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  • 9
    Publication Date: 2015-12-24
    Description: We present a platform on the OMEGA EP Laser Facility that creates and diagnoses the conditions present during the preheat stage of the MAGnetized Liner Inertial Fusion (MagLIF) concept. Experiments were conducted using 9 kJ of 3ω (355 nm) light to heat an underdense deuterium gas (electron density: 2.5 × 10 20   cm − 3 = 0.025 of critical density) magnetized with a 10 T axial field. Results show that the deuterium plasma reached a peak electron temperature of 670 ± 140 eV, diagnosed using streaked spectroscopy of an argon dopant. The results demonstrate that plasmas relevant to the preheat stage of MagLIF can be produced at multiple laser facilities, thereby enabling more rapid progress in understanding magnetized preheat. Results are compared with magneto-radiation-hydrodynamics simulations, and plans for future experiments are described.
    Print ISSN: 1070-664X
    Electronic ISSN: 1089-7674
    Topics: Physics
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  • 10
    Publication Date: 2011-07-24
    Description: We have developed density–viscosity–composition (–µ– X ) models for natural aqueous fluids and hydrous melts, based on experimental data for silicate + H 2 O, especially for the pressure ( P ) and temperature ( T ) conditions above subduction zones. We examine hydrothermal and melt pathway systematics above subducting slabs into the Earth’s mantle, back up along the top-of-slab, and downward with the subduction. Aqueous slab fluids and hydrous mantle melts show distinct flow properties (as observed in activation energy in viscosity data) despite continuity in solute-polymerization characteristics. Buoyancy changes are small for fluids except in the localized vicinity of critical behaviour and at solidi where H 2 O partitions also into melt. Our model predicts dilute high- PT potassic haplogranite fluids to be less viscous than sodic varieties whereas for concentrated fluids a deep viscosity minimum occurs in mixed K/Na ( c . 1:1 molar) compositions. Higher dissolved silicate concentrations increase fluid density and viscosity leading to slower less-buoyant flow with increasing PT . Thus ascent rates of slab fluid increase by about an order of magnitude (from c . 10 –3·5 to 10 –4·3 m s –1 for porous flow; c . 1 to 7 m s –1 for flow through 1 mm wide fractures) with decompression from 5 to 3 GPa, as a result of decreasing solute loads, and µ. Mantle fluid viscosities are predicted (10 –4 to 10 –3·7 Pa s) to be approximately half those of crustal fluids (10 –3·9 to 10 –3·1 Pa s) and of lower density (e.g. 1·4 compared to 1·6 g cm –3 ), reflecting their compositional differences (here mainly SiO 2 ). Thus, ascending slab fluids tend to accelerate as they move back up the slab and also moving from slab to porous mantle. Slab melts are up to c . 6 orders of magnitude less viscous (e.g. c . 10 –0·5 to 10 2·5 Pa s) and therefore faster flowing than hydrous deep crustal granitoids (e.g. c . 10 6·5 to 10 3·5 Pa s), reflecting higher water contents of the former (e.g. 30 vs 10 wt %). Concentrated crustal fluids migrate 5–6 orders of magnitude faster than hydrous melt, mostly because of calculated viscosity differences. We find that fluids flow faster in the mantle than in the crust, and that most of the mass transfer through the mantle occurs via hydrous melt.
    Print ISSN: 0022-3530
    Electronic ISSN: 1460-2415
    Topics: Geosciences
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