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  • 1
    Publication Date: 2011-08-24
    Description: BACKGROUND: It is well known that space travel cause post-flight orthostatic hypotension and it was assumed that autonomic cardiovascular control deteriorates in space. Lower body negative pressure (LBNP) was used to assess autonomic function of the cardiovascular system. METHODS: LBNP tests were performed on six crew-members before and on the first days post-flight in a series of three space missions. Additionally, two of the subjects performed LBNP tests in-flight. LBNP mimics fluid distribution of upright posture in a gravity independent way. It causes an artificial sequestration of blood, reduces preload, and filtrates plasma into the lower part of the body. Fluid distribution was assessed by bioelectrical impedance and anthropometric measurements. RESULTS: Heart rate, blood pressure, and total peripheral resistance increased significantly during LBNP experiments in-flight. The decrease in stroke volume, the increased pooling of blood, and the increased filtration of plasma into the lower limbs during LBNP indicated that a plasma volume reduction and a deficit of the interstitial volume of lower limbs rather than a change in cardiovascular control was responsible for the in-flight response. Post-flight LBNP showed no signs of cardiovascular deterioration. The still more pronounced haemodynamic changes during LBNP reflected the expected behaviour of cardiovascular control faced with less intravascular volume. In-flight, the status of an intra-and extravascular fluid deficit increases sympathetic activity, the release of vasoactive substances and consequently blood pressure. Post-flight, blood pressure decreases significantly below pre-flight values after restoration of volume deficits. CONCLUSION: We conclude that the cardiovascular changes in-flight are a consequence of a fluid deficit rather than a consequence of changes in autonomic signal processing.
    Keywords: Aerospace Medicine
    Type: European journal of clinical investigation (ISSN 0014-2972); Volume 30; 12; 1055-65
    Format: text
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  • 2
    Publication Date: 2019-06-28
    Description: At the ends of a monocoque fuselage concentrated axial forces in the skin must generally be taken up. Such axial forces must also be taken up in the case of other members where axial forces from the neighboring stressed skin construction must be considered. In order to take up these axial forces two bulkheads or reinforcing frames may be arranged at the positions where the forces are applied. If these bulkheads are in the form of rings, bending moments are set up in them. In the present paper computations are performed for obtaining the value of these bending moments.
    Type: NACA-TM-847
    Format: application/pdf
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  • 3
    Publication Date: 2019-06-28
    Description: An implicit time marching finite difference method is used to predict two dimensional turbulent flow at a Reynolds number of 440,000 and a Mach number of 0.574 over a shortened NACA 0012 airfoil with a trailing edge of 4.5% thickness and semicircular shape. The flow is found to be unsteady but periodic in the trailing edge region. Thus, lift and drag fluctuate at small amplitudes around mean values and at distinct frequencies.
    Keywords: FLUID MECHANICS AND HEAT TRANSFER
    Type: NASA-TM-84278 , A-9029 , NAS 1.15:84278
    Format: application/pdf
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  • 4
    Publication Date: 2017-12-19
    Description: This paper presents an event stratigraphy based on data documenting the history of vegetation cover, lake-level changes and fire frequency, as well as volcanic eruptions, over the Last Glacial–early Holocene transition from a terrestrial sediment sequence recovered at Lake Accesa in Tuscany (north-central Italy). On the basis of an age–depth model inferred from 13 radiocarbon dates and six tephra horizons, the Oldest Dryas–Bølling warming event was dated to ca. 14 560 cal. yr BP and the Younger Dryas event to ca. 12 700–11 650 cal. yr BP. Four sub-millennial scale cooling phases were recognised from pollen data at ca. 14 300–14 200, 13 900–13 700, 13 400–13 100 and 11 350–11 150 cal. yr BP. The last three may be Mediterranean equivalents to the Older Dryas (GI-1d), Intra-Allerød (GI-1b) and Preboreal Oscillation (PBO) cooling events defined from the GRIP ice-core and indicate strong climatic linkages between the North Atlantic and Mediterranean areas during the last Termination. The first may correspond to Intra-Bølling cold oscillations registered by various palaeoclimatic records in the North Atlantic region. The lake-level record shows that the sub-millennial scale climatic oscillations which punctuated the last deglaciation were associated in central Italy with different successive patterns of hydrological changes from the Bølling warming to the 8.2 ka cold reversal. Copyright © 2006 John Wiley & Sons, Ltd.
    Type: Article , PeerReviewed
    Format: text
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  • 5
    Publication Date: 2017-09-19
    Type: Report , NonPeerReviewed
    Format: text
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  • 6
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    In:  (Bachelor thesis), Christian-Albrechts-Universität, Kiel, 48 pp
    Publication Date: 2016-01-05
    Keywords: Studiengang
    Type: Thesis , NonPeerReviewed
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  • 7
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    In:  (Bachelor thesis), Christian-Albrechts-Universität, Kiel, 78 pp
    Publication Date: 2013-02-07
    Keywords: Studiengang
    Type: Thesis , NonPeerReviewed
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  • 8
    Publication Date: 2023-11-20
    Description: Microbiomes are omnipresent companions of macro organisms. Survival and fitness of individuals depends on them. Many human diseases originate in a shift of microbiome, and it cannot be excluded that marine organisms are suffering from the same issue. Complex symbiotic systems depend on numerous factors and can have devastating effects on the holobiont, which is the host along with its associated microorganisms, as an ecological unit. Marine organisms are exposed to prolonged ocean acidification and rising temperatures, leading to sustained pathological changes. Algal bleaching, also named "ice-ice" disease, is a pigmentary abnormality of different macro algae causing perish of the organisms. The "Jekyll & Hyde" theory verified, that symbiotic bacteria change from "friends" into "foes" through environmental conditions. These assays prove, for the first time, the dependence of A. vermiculophyllums microbiome on temperature. A. vermiculophyllum is a red algae, found around the northern hemisphere. Despite its ability to adapt, it is affected by this disease. Previous assays investigated its microbiome and assigned certain bacteria strains to it. 22 as protective or pathogenic classified strains and their metabolites were examined in this experiment. Tips of A. vermiculophyllum were inoculated with cells or supernatant of one strain at a time for five days at five different temperatures. Bleached tips were counted before and afterwards. The present data reveals new possibilities to investigate the microbiome of red algae and inches closer to the origin of algal bleaching.
    Type: Thesis , NonPeerReviewed
    Format: text
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  • 9
    Publication Date: 2021-03-29
    Description: Die Hauptstrasse Nr. 8 zwischen Schwyz und Sattel verläuft durch aktive und tiefgründige Permanentrutschungen. Im lehmigen, matrix-gestützten Gehängeschutt der Rutschung ‚Spiegelberg’ wurde zwischen 1979–81 die Gütschbrücke erstellt (LK: 690.314/211.943; 670 m ü.M.) und unter Anwendung von Gründungsschutzschächten im unterlagernden Fels fundiert. Beim Aushub des Schutzschachtes für den Pfeiler WL-Nord wurden in der Tiefe von 25 m bzw. 38 m unter Oberkante Terrain zwei Nadelbaumfragmente gefunden. Letzterer Holzfund lag wenige Meter über der Felsoberfläche. Die 14C-Altersdatierung der Holzfunde (beide Pinus sylvestris) ergaben kalibrierte Altersspannen zwischen 11.690–11.270 cal. a BP (2s) am Übergang vom Grönland Stadial 1 (GS-1; ‚Jüngere Dryas’) zum Holozän bzw. 13.830–13.640 cal. a BP (2s) zu Beginn der spätglazialen Wärmeschwankung GI-1c (Grönland Interstadial 1c; ‚Allerød’). Die vorliegenden Daten zeigen, dass die Hanginstabilitäten bei ‚Spiegelberg’ nach dem Zerfall des letzteiszeitlichen Muota/Reussgletschers zu Beginn des Spätglazials eingesetzt haben mussten, und die Waldkiefer schon kurz nach den Kälterückschlägen des GI-1d (‚Aegelsee-Schwankung’) bzw. des GS-1 am nördlichen Alpenrand präsent war.
    Description: research
    Keywords: 551 ; vegetation history ; late glacial ; C-14 dating ; H8 Schwyz–Sattel ; Steinen ; Engelstock ; subalpine molasse ; landslide area
    Language: German
    Type: article , Verlagsversion
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  • 10
    Publication Date: 2021-05-06
    Description: The sedimentary and morphological evidence for Lateglacial glacier fluctuations in the Lienz area provides a strong case against the currently used pentapartite stratigraphic subdivision of the Alpine Lateglacial (ALG; c. 19–11.7 ka) i.e. the timespan between the Würmian Pleniglacial (= Alpine Last Glacial Maximum; AlpLGM) and the beginning of the Holocene. The results of comprehensive geological mapping (including the detection of mass movements) supported by geochronological data and pollen analysis revealed that the ALG- record of the Schobergruppe mountains and the Lienz Dolomites can be subdivided into four unconformity-bounded (allostratgraphic) units which are linked to three climatostratigraphically-defined phases of glacier activity. Delta deposits and till of local glaciers document the phase of ice-decay after the AlpLGM. Between this period and the Bølling/Allerød (B/A) interstadial only one glacier stabilisation with massive end moraines, correlated with the Gschnitz stadial, is evident. Multiple end moraines prove the presence of very active glacier tongues during the Younger Dryas aged Egesen stadial. The 10Be exposure dating of an end moraine, previously attributed to the Daun stadial (pre-B/A interstadial) based on ΔELA values, provided an age of 12.8 ± 0.6 ka indicating it is of Younger Dryas age. This case highlights the pitfalls of the commonly used ΔELA-based stratigraphic ALG subdivision and the subsequent derivation of palaeoclimatic implications. ΔELAs are still considered as a useful tool for correlation on the local scale e.g. in one mountain group with a quite comparable topography and lithology and taking into account the limitations, especially the impact of debris cover. However, our results show that a stratigraphic correlation across the whole Alpine chain via ΔELAs is not a successful approach potentially leading to bias and, eventually, to circular arguments.
    Description: research
    Keywords: 551.7 ; palynology ; alps ; late pleistocene ; lateglacial ; younger dryas ; geological mapping ; allostratigraphy ; climatostratigraphy ; exposure dating ; deformable bed
    Language: English
    Type: article , Verlagsversion
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