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- Concrete (4)
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Hochtemperaturtribologie
(2010)
Die Temperatur ist eine fundamentale Beanspruchungs- bzw. Einflussgröße für alle tribologischen Systeme. Für die in zahlreichen tribologischen Systemen benötigten Schmierstoffe liegen die thermischen Stabilitätsgrenzen bei etwa 400?°C. Es wird die tribologische Prüftechnik für Tribomaterialien beschrieben, die für den Einsatz in tribologischen Systemen bei hohen Betriebstemperaturen verwendbar sind. Ausgehend von metallurgischen Lösungsansätzen aus der Tribologieforschung werden Anwendungsmöglichkeiten hochtemperaturbeständiger Ingenieurwerkstoffe mit Beispielen aus der Automobiltechnik (Luftlagerung von Turboladern, Leistungssteigerung von Bremsmaterialien), der Fertigungstechnik (Standzeitverlängerung von Werkzeugen) und dem chemischen Anlagenbau (Effizienzsteigerung von Kühlkreisläufen) dargestellt.
The introduction of an innovative process for non-destructive testing is described in terms of its different phases and how the process is controlled in the Fraunhofer IZFP in order to obtain optimal results. Examples are discussed of applications by IZFP in various important and safety-relevant industrial sectors where the automated inspection systems were introduced. These case studies include the inspection of railway components such as the wheel sets of the German high-speed train and in-line pipe inspection by using intelligent pipeline inspection gauges. Complex inspection systems, both hardware and software, developed in partnership with the Federal Institute for Materials Research and Inspection (BAM), were applied to inspection tasks in civil engineering. Two automated systems based on a robot and on a flexible manipulation are presented. Both systems can be applied to diverse inspection technologies and to the data fusion of various types of non-destructive testing (NDT) data.
Plasmapolymerisation
(2010)
Fallbeispiele für die Anwendung der 3D-Messtechnik und der aktiven Thermografie in der Denkmalpflege
(2010)
Solar energy has been transformed into useful redox differences or disequilibria within the Earth´s crust since the onset of anoxygenic and oxygenic photosynthesis in the Precambrian. Inorganic oxidized carbon is transformed into reduced carbon compounds by capturing and storing solar energy. During this process, many different organic compounds are formed including carbohydrates, proteins, hydrocarbons, and various other complex organic metabolic products and their diagenetic polymerization products (melanin, humic substances, petroleum, coal, and kerogen). Many of these solar energy-enriched compounds, however, are oxidized immediately or during the diagenetic transformation of sediments. The oxidation agents are oxygen, sulfate, iron, and other oxidized compounds, which in turn are partly enriched with the original solar energy. On a global biogeochemical scale, however, sulfur and iron are the most important elements. Geological evidence shows that biogeochemical cycles tend to yield stable ratios between the most oxidized forms of carbon (carbon dioxide and calcium/magnesium carbonate) and the most reduced forms (diamond, coal, methane, and hydrocarbons). Throughout the Earths history and evolution, this equilibrium ratio is around 1:4, maximally 1:5. When too much carbon is stored in the crust in the form of reduced compounds or vice versa, climatic and biogeomorphogenetic consequences upset the equilibrium. The biosphere reacts in a way to return to the optimal ratio. Excellent examples for this fluctuating equilibrium are the Carboniferous (too much organic carbon stored), the Permian (too little organic carbon stored), and the Tertiary with a generally equivalent production of hydrocarbons and carbonates. At present, we are in a period in which there is a global biogeochemical need to oxidize reduced carbon compounds as fast as possible in order to avoid even more dramatic global climate shifts. The highly evolved human genome seems to be the tool for this shift. Enormous amounts of reduced carbon are turned into the oxidized form as carbon dioxide, which by various biogeochemical pathways is quickly transformed into carbonate, another oxidized form of carbon that can be stabilized and stored in the sedimentary record. Fast recycling of excessively stored solar energy may enable the survival of a global biosphere under highly stressed conditions.
This chapter provides an overview of methods that are commonly used for the analysis of the original water content of fresh and hardened concrete. The methods consist of direct methods, which detect the water content or the water/cement ratio primarily, as well as indirect methods, which measure other material characteristics related to the water content.