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  • 1
    Keywords: Forschungsbericht
    Type of Medium: Online Resource
    Pages: 95 p. = 1964 kB, text and images
    Edition: [Electronic ed.]
    Language: German
    Note: Contract no. BMBF 03 N 5002 C , nIndex , Differences between the printed and electronic version of the document are possible
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  • 2
    ISSN: 1435-1420
    Keywords: Key words Transit thrombus of the right heart ; pulmonary embolism ; thrombolysis with streptokinase in high dose ; Schlüsselwörter Ultrahochdosierte Streptokinasekurzzeitlyse ; Lungenembolie ; rechtsatrialer Transit-Thrombus
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Description / Table of Contents: Zusammenfassung Ein 68jähriger Patient mit seit fünf Tagen bestehender Dyspnoe wurde nach nuklearmedizinischem Hinweis auf eine Lungenembolie im Stadium II–III einer Sonographie vor der geplanten Lysetherapie unterzogen. Dabei fand sich ein rechtsatrialer, flottierender Thrombus. Bei bestehender akuter vitaler Gefährdung wurde eine Ultrahochdosierte Streptokinasekurzzeitlyse (UHSK) mit 9.000.000 Einheiten Streptokinase über 6 Stunden und paralleler intravenöser Antikoagulation mit Heparin eingeleitet. Nach 3 Zyklen hatte sich der Transit-Thrombus vollständig und die Thrombose des Beines weitgehend aufgelöst. Diese Therapieform stellt eine interessante Alternative bei dem angesprochenen Krankheitsbild dar.
    Notes: Summary A 68-year-old patient with dyspnea since 5 days from pulmonary embolism documented by perfusion scintigraphy underwent examination with ultrasound before thrombolytic therapy. US showed a transit-thrombus in the right atrium. Because of threat to life a thrombolytic therapy was given with 9 million IE of streptokinase over 6 h (UHSK) and additional therapy with heparin. After three courses of UHSK the transit-thrombus and the thrombosis of the leg had nearly completely resolved. This mode of therapy is an interesting alternative in treatment for pulmonary embolism and transit-thrombus of the right heart.
    Type of Medium: Electronic Resource
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  • 3
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    In:  EPIC3Posterbeitrag auf dem 4. Symposium Massenspektrometrische Verfahren der Elementspurenanalyse, 28.9.-1.10.1998, Mainz.
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 4
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    In:  Geowissenschaftliche Bewertungsgrundlagen zur Nutzung hydrogeothermaler Ressourcen in Norddeutschland | Scientific technical report ; 97/15
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/bookPart
    Format: application/pdf
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  • 5
    Publication Date: 2020-12-10
    Description: The utilization of geothermal reservoirs as alternative energy source is becoming increasingly important worldwide. Through close-range aerial photogrammetry realized by unmanned aircraft systems (UAS), this study investigates the surface expression of a leaking warm water reservoir in Waiwera, New Zealand, that has been known for many centuries but remained little explored. Due to overproduction during the 1960s and 1970s the reservoir has suffered significant pressure reduction, which resulted in the loss of artesian conditions and led to the desiccation of the hot springs in close succession. However, shortly after the recent shutdown of the primary user (Waiwera Thermal Resort & Spa) renewed artesian activity was reported by locals but no hot spring activity has been observed so far. Therefore, this study was carried out in October 2019 to assess the actual conditions of thermal activity in the area of the former hot springs. UAS with coupled thermal infrared cameras were used for thermal mapping and the obtained data show renewed activity of the hot springs on the beachfront of Waiwera. Faults and fractures were identified as important fluid pathways, as well as individual fluid conducting lithologies.
    Language: English
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 6
    Publication Date: 2020-12-10
    Description: Numerical simulation has become an inevitable tool for improving the understanding on coupled processes in the geological subsurface and its utilisation. However, most of the available open source and commercial modelling codes do not come with flexible chemical modules or simply do not offer a straight-forward way to couple third-party chemical libraries. For that reason, the simple and efficient TRANsport Simulation Environment (TRANSE) has been developed based on the Finite Difference Method in order to solve the density-driven formulation of the Darcy flow equation, coupled with the equations for transport of heat and chemical species. Simple explicit, weighted semi-implicit or fully-implicit numerical schemes are available for the solution of the system of partial differential equations, whereby the entire numerical code is composed of less than 1000 lines of Python code, only. A diffusive flux-corrected advection scheme can be employed in addition to pure upwinding to minimise numerical diffusion in advection-dominated transport problems. The objective of the present study is to verify the numerical code implementation by means of benchmarks for density-driven fluid flow and advection-dominated transport. In summary, TRANSE exhibits a very good agreement with established numerical simulation codes for the benchmarks investigated here. Consequently, its applicability to numerical density-driven flow and transport problems is proven. The main advantage of the presented numerical code is that the implementation of complex problem-specific couplings between flow, transport and chemical reactions becomes feasible without substantial investments in code development using a low-level programming language, but the easy-to-read and -learn Python programming language.
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 7
    Publication Date: 2020-12-10
    Description: Barite scales in geothermal installations are a highly unwanted effect of circulating deep saline fluids. They build up in the reservoir if supersaturated fluids are re-injected, leading to irreversible loss of injectivity. A model is presented for calculating the total expected barite precipitation. To determine the related injectivity decline over time, the spatial precipitation distribution in the subsurface near the injection well is assessed by modelling barite growth kinetics in a radially diverging Darcy flow domain. Flow and reservoir properties as well as fluid chemistry are chosen to represent reservoirs subject to geothermal exploration located in the North German Basin (NGB) and the Upper Rhine Graben (URG) in Germany. Fluids encountered at similar depths are hotter in the URG, while they are more saline in the NGB. The associated scaling amount normalised to flow rate is similar for both regions. The predicted injectivity decline after 10 years, on the other hand, is far greater for the NGB (64%) compared to the URG (24%), due to the temperature- and salinity-dependent precipitation rate. The systems in the NGB are at higher risk. Finally, a lightweight score is developed for approximating the injectivity loss using the Damköhler number, flow rate and total barite scaling potential. This formula can be easily applied to geothermal installations without running complex reactive transport simulations.
    Language: English
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 8
    Publication Date: 2021-01-19
    Description: Energy supply in Germany is subject to a profound change. The present paper addresses the German potential of storing excess energy from renewable power sources in the geological subsurface. Wind and solar electricity can be transformed into hydrogen, and with carbon dioxide subsequently into methane. When needed, electricity is regained in a gas turbine power plant combusting the methane. Here, we are taking into account the actual German storage capacity for natural gas and show that the outlined technology is ready for operation and economically competitive. The current potential for combined storage of methane and carbon dioxide allows to store around 80 TWh renewable excess energy. This is far more than required to date and estimated to provide the entire coverage in 2050.
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 9
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    In:  Glückauf-Mining-Reporter : international journal for mining, tunnelling, equipment and technology
    Publication Date: 2021-02-02
    Description: To limit global warming to 2 °C above pre-industrial levels, our society is confronted with the urgent need to make the transition to a globally sustainable energy system (1). Geothermal energy is available regardless of season or time and, unlike many other renewable energies, is therefore suitable for base-load sytems. Geothermal energy is regarded as renewable as heat flows back into the reservoir due to temperature conditions and transport processes. It uses the energy source from the earth’s interior, which is inexhaustible by human standards. Geothermal energy can play an important role in the decarbonization of the energy system in Germany. In Central Europe, the greatest geothermal potential lies in the crystalline basement with important hotspots in areas under tectonic tension. These include the Upper Rhine Graben as a rift zone with hydrothermal fluid flows and exceptional temperature anomalies in the deep underground (2). The technology “Enhanced Geothermal Systems” (EGS) was developed to exploit the geothermal potential in the crystalline (3). EGS use the deep fractured subsoil as a natural heat exchanger. With at least two boreholes, a thermal water cycle is created that brings geothermal energy to the surface and makes it usable (4). However, since relatively high flow rates (〉 10 l/s) are required for economic operation, the natural permeability of the rock in the crystalline – in contrast to hydrothermal systems – must be increased by hydraulic or chemical stimulation measures (reservoir engineering) to increase the flow rates. A major challenge for EGS is to control and minimize the induced seismicity generated in this process, both in the reservoir engineering and operation phase and with a view to increasing public acceptance. A profound understanding of the multi-physical processes in the reservoir, such as the complex interactions of the fluid with the reservoir at high flow rates, is indispensable for this. New scientifically based strategies and technologies are urgently needed to exploit the geothermal potential economically and at the same time in an environmentally compatible way.
    Language: English , German
    Type: info:eu-repo/semantics/article
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  • 10
    Publication Date: 2020-02-12
    Description: Wie geochemisch-thermodynamische Modellierungen gezeigt haben, können während des Betriebs einer geothermischen Heizanlage durch Druck- und Temperaturveränderungen Baryt, Anhydrit/Gips oder Cölestin ausfallen. Das Fällungsverhalten der Erdalkalisulfate wurde unter In-situ-Bedingungen (Druck, Temperatur, Salinität 216 g/l) in einem Durchströmungsversuch bestimmt. Es wird eine Durchströmungsanlage vorgestellt, die Drucke bis zu 250 bar und hohe Temperaturen bei der Durchströmung eines Sandsteinkerns zuläßt. Ergänzende Fällungsexperimente bestätigen eine zu erwartende Reaktion zweiter Ordnung bei der Kristallisation von Baryt mit einer mittleren Geschwindigkeitskonstanten von 2,5 • 10-4 l mg-1 h-1. Die real lösliche Menge Baryt (2,5 mg/l Ba und 450 mg/l SO4) ist höher als das thermodynamische Gleichgewicht vorhersagt. Cölestin und Anhydrit oder Gipsausfällungen konnten nicht nachgewiesen werden. Bei der Durchströmung des Sandsteinkerns unter In-situ- Bedingungen findet keine Ausfällung von Baryt, Anhydrit/ Gips oder Cölestin statt. Obwohl Kristallisationskeime im Sandstein vorhanden sind, erfolgt keine Fällung aus den metastabilen Lösungen.
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/article
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