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Der Datensatz enthält die Radverkehrsanlagen der Freien und Hansestadt Hamburg. Da es sich um einen routingfähigen Datensatz handelt, werden nicht nur klassische Radverkehrsanlagen (Radweg, Radfahrstreifen, Schutzstreifen etc.) erfasst, sondern auch Straßen und Wege, die von Radfahrenden nutzbar sind. Weiterhin werden auch Fußwege erfasst, wenn sie als sogenannte Schiebestrecken Lücken im Radverkehrsnetz füllen. Folgende Attribute werden bereitgestellt: - Status (Betrieb, Temporäre Anlage, …) - Straßenname - Art (Getrennter Geh-/Radweg, Gemeinsamer Geh-/Radweg, Radfahrstreifen, Schutzstreifen, Straße mit Mischverkehr bis 30 km/h, Fußgängerzone…) - Klasse (Radweg, Radfahrstreifen, Schutzstreifen, Fahrradstraße, Wege in Grünanlagen, Straße mit Mischverkehr, Schiebestrecke, Sonstige) - Zeitliche Beschränkung - Benutzungspflicht - Fahrtrichtung (in Geometrie-Richtung, in beide Richtungen) - Oberfläche (bituminöse Decke, wassergebundene Decke, Kunststein, Naturstein, …) - Breite in m - Hindernis (Durchfahrbarkeit gegeben, Umfahrung möglich, …) - Niveau (bodengleich, Tunnel, …) Die Visualisierung im WMS und somit auch im Geoportal erfolgt anhand des Attributs Klasse. Um die Übersichtlichkeit zu erhöhen, werden die Daten in sieben verschiedene Layer unterteilt, die sich an den Klassen orientieren. Langfristig, z.B. wegen Baumaßnahmen, gesperrte Wege werden nicht im Datensatz veröffentlicht. Sollten Sie Anmerkungen zum Datensatz haben oder Korrekturen melden wollen, schicken Sie diese bitte an radverkehrsnetz@gv.hamburg.de. Es kann keine Gewähr für die Richtigkeit aller Daten übernommen werden. Aufgrund der Aktualität des Datensatzes kann keine rechtssichere bzw. tagesaktuelle Aussage getroffen werden.
SP0 is conceived for coordination of the ICON research, for internal and external scientific exchange as well as for investigating development pathways of land use on the Philippines. The SP0 team will supervise the project activities as a whole, including reporting and final synthesis. It will design the ICON homepage, establish and maintain a web-based database and present the project and its results in scientific forums and public media. It will organize collaboration and scientific exchange with international networks dealing with atmospheric processes, global carbon, nitrogen, water and energy cycles, and long-term ecological research. Specifically, SP0 is devoted to ensuring a sound integration of the ICON project within the scientific communities of Germany and SE Asia. Supported by the ICON local research coordinator based at and employed by IRRI, it will coordinate with the IRRI farm management to assist other ICON subprojects with field setup, routine data collection and technical backstopping.
Suche von Schulen in Hamburg und Anzeige von Informationen zur jeweiligen Schule. Integriert im Schulinfosystem ist das Schulwegrouting. Finden Sie den kürzesten Fußweg von Ihrer Haustür zu den Schulen in Hamburg. Neben einer umfangreichen Filterfunktion gibt es auch die Möglichkeiten über die Vergleichsliste Schulen direkt miteinander zu vergleichen.
Das Geoportal der Metropolregion Hamburg ist der wesentliche Baustein der Geodateninfrastruktur der Metropolregion Hamburg (GDI-MRH). Es bündelt die Geodaten der Länder und Kommunen der Metropolregion Hamburg (MRH) und ergänzt diese durch übergreifende Themen, die teilweise bundesweit verfügbar sind oder von der Geschäftsstelle der Metropolregion erfasst oder erworben werden. Die im Geoportal MRH präsentierten Daten liegen in der Zuständigkeit verschiedener Akteure in der MRH. Weitere Informationen zu den Nutzungsbedingungen und inhaltlichen Ansprechpersonen erhalten Sie über die Metadaten der einzelnen Datensätze. Eine vollumfängliche Übersicht über die Datensätze des Geoportals bietet der Themenbaum des Geoportals MRH.
The hydrogeochemical dynamics in mountainous areas of the Korean Peninsula are mainly driven by a monsoon-type climate. To examine the interplay between hydrological processes and the mobilization and subsequent transport and export of nitrate and DOC from catchments, a field study was initiated in the Haean catchment in north-eastern South Korea under highly variable hydrologic conditions. In order to identify nitrate and DOC source areas, a subcatchment (blue dragon river) within the Haean basin, which includes different types of landuses (forest, dry land farming, and rice paddies), was selected. In 2009, high frequency surface water samples were collected at several locations during summer storm events. A similar but more comprehensive sampling routine was completed in 2010. In order to investigate the groundwater level fluctuations relative to the hydraulic potentials, a piezometer transect was installed across a second order stream of the subcatchment. The results so far suggest deep groundwater seepage to the aquifer with practically no base flow contributions to the stream in the mid-elevation range of the catchment. In 2009 the focus of research was within the subcatchment, in 2010 additionally a second piezometer transect was installed at a third order stream in the lower part of the catchment (main stem of the Mandae River) where more dynamic groundwater/surface water interactions are assumed due to expected higher groundwater levels in this part of the basin. In order to investigate these interactions piezometers equipped with temperature sensors and pressure transducers were installed directly into the river bed. Based on the observed temperature time series and the hydraulic potentials the water fluxes between the groundwater and the river can be calculated using the finite-difference numerical code, VS2DH. VS2DH solves Richard s equation for variably-saturated water flow, and the advection-conduction equation for energy transport. The field data collected at the second piezometer transect suggest that the investigated river reach exhibits primarily losing surface conditions throughout most of the year. Gaining groundwater conditions at the river reach are evident after monsoonal extreme precipitation events. At the transect streambed aggradation and degradation due to bedload transport was observed. Significant erosion has been reported throughout the catchment after extreme events. Results indicate that the event-based changes in streambed elevation, is an additional control on groundwater and surface water exchange. The streambed flux reversals were found to occur in conjunction with cooler in-stream temperatures at potential GW discharge locations. The export of nitrate and DOC were found to be variable in time and strongly correlated to the hydrologic dynamics, i.e. the monsoon and pre- and post-monsoon hydrological conditions. usw.
Integrated water resources management in an ecologically and economically adequate way is receiving more and more attention when it comes to the development of sustainable strategies in either developed or developing countries. Ecohydrological models like the SWAT model are widely applied tools for sustainable management of water resources at river basin scale. Nevertheless it is still not clearly understood, how river basin management drives changes in the hydrological balance and the water quality of catchments. This is especially apparent in lowland catchments characterized by low hydraulic gradients, flat topography, high potential for water retention, a large amount of tile drainages and a close interaction of surface- and groundwater.The objective of this project is thus to test the applicability of a biological tracer (i.e. diatoms) for the detection of surface runoff and drainage flow in the example case of the Kielstau catchment (50 km2) in northern Germany. Based on the diatom and water quality analyses of daily mixed, rain event based river and tile drainage samplings, we aim to1) quantify the contribution of surface runoff to total river discharge in lowlands,2) separate surface runoff from tile drainage flow based on different diatom concentration of each flow component and determine the entry pathways of phosphorus into the river, and 3) implement the detected runoff generation and phosphorous transport processes into the newly introduced tile-drainage routine of the ecohydrological SWAT model to improve the routine structure and the model performance.
There is growing public concern about the increasing occurrence of manmade substances with hormone like activity - so called endocrine disrupting chemicals (EDCs). The identification of a given chemical as an EDC is routinely based on experiments with (sub-)adult mice or rats. The project GenOvotox aims to develop a replacement method for such tests using the chicken embryo. Both, responses on the structural (anatomical and histological alterations) and molecular level are used to identify specific effects of EDCs in very early embryonic development. These responses are evaluated for their suitability to be used in the future on a routine basis for the identification of EDCs in a regulatory context. The work programme of GenOvotox, a joint project between the companyGenXPro GmbH and our department, comprises the establishment, validation and commercialisation of a molecular screening tool by: - using SuperSAGE (Matsumura et al. 2003, 2005, 2006) for mRNA analysis and genome-wide quantification of gene activity in early developmental stages of the chicken embryo, - achieving a dose-effect relationship of endocrine disruptors on a structural and molecular level, - getting justifiable replacement, reduction and refinement of animal testing methods (Russel & Burch 1959) in the context of REACh.
In Northern Thailand and Vietnam, fresh fruit marketing still plays the key role in utilisation of the highly perishable fruits studied. Increasing export rates aspired by local fruit producers are hindered by the present practice of shelf life extension based on sulphur fumigation and fungicide application, respectively, because of raising legal and consumer restriction. Alternative ways ensuring the demand for sound fruit of good eating quality are urgently required. Since picking, packing and marketing form the major costs of fruit production, E2.3 aims at improved productivity by optimisation of fresh fruit marketing through an integrated high-quality concept for shelf life extension to meet export qualities and standards and to facilitate the access to remote markets and processing factories. This approach relies on two pillars: (1) innovative postharvest processes and (2) plant-physiological preharvest factors affecting fruit quality and shelf life, chiefly the proper physiological maturity at harvest. Focus is on shelf life extension and color retention of litchis and longans by minimising enzymatic browning, microbial decay, and water loss through appropriate combinations of various techniques: (1) precooling on field until handover; (2) fruit disinfestation by thermal routines; (3) control of enzymatic browning by innovative inhibition strategies for polyphenoloxidase and peroxidase; (4) suitable shipping within a cool-chain with or without modified atmosphere packaging; (5) application of wetting agents or coatings. By analogy, integrated strategies for shelf life extension through deceleration of postharvest ripening in export of Thai mango cultivars are explored. To control enzymatic browning in Sapindaceae species, both inhibition experiments on isolated enzymes and application tests with shelf life studies simulating shipping conditions are used. Process optimisation is based on statistical experimental designs. Shelf life is monitored by established chemical methods for plant-physiological indicators of fruit quality, senescence and microbial decay, by the vital microbial count, and by microscopic studies of the peel structure. On-tree maturation is examined for each fruit species to specify physiological harvest maturity as to its impact on quality and shelf life, including studies with E1.2 on non-destructive maturity detection. Cultivation effects on fruit quality and shelf life are jointly investigated with D1.3 and B3.2.
The project aims at comprehensively characterizing metabolic regulations that are observed in reciprocal crosses of Arabidopsis thaliana compared to the corresponding parental lines and in recombinant inbred lines and corresponding test crosses. In the first 2-years period of the project, emphasis is given to acquire data for large sets of plant populations (P, F1, F2, RIL and TCRIL) by routine gas chromatography/time-of-flight mass spectrometry (GC/TOF), and to extend this method to large and thermolabile compounds by liquid chromatography/tandem mass spectrometry (LC/MS2), specifically membrane lipids, organic phosphates and glycosylated compounds. All plants will be grown under controlled environmental conditions and randomised block designs to allow statistical evaluations. Observed metabolic alterations are then mapped to biochemical pathways and cycles in order to found links between metabolite, protein, and gene regulations. Changes in metabolism are statistically analysed with respect to hybrid vigour (incrase in dry shoot matter) observed in F1 lines and recombinant inbred lines. Metabolic inheritance will be assessed by a combination of different statistical and computational tools and linked to heterosis effects in total growth. Physiological, metabolomic, and genetic marker data will be used for the identification of quantitative trait loci (QTL) in close collaboration with partner projects.
Recent progress in the operation of CO2 gas ion sources for accelerator mass spectrometer (AMS) 14C analysis on microgram-size samples opens a wide range of new applications in dating studies, e.g. for environmental and archeological applications. This proposal aims at implementing a gas ion source at the AMS system MICADAS at the Klaus-Tschira Laboratory of the Curt-Engelhorn-Zentrum für Archäometrie (CEZA) in Mannheim and to use this new capability for cutting-edge applications in environmental studies, namely the dating of small amounts of organic carbon contained in glacier ice and of specific organic compounds in ground water. Cold glaciers hold unique records on past climate and atmospheric composition. Mid-latitude ice cores furthermore enable reconstructions of recent ice chemistry changes, but cannot be dated by stratigraphic methods. For such ice bodies, only radiometric dating based on 14C analysis of organic matter contained in the ice matrix presently offers a reasonable dating potential in the late Holocene and beyond. The challenge of this approach lies in the very restricted availability of this matter, but the ability to analyse microgram samples of organic carbon from ice via a gas ion source should now enable reliable 14C dating of ice. Ground water constitutes an important water resource worldwide, especially in semi-arid regions, and in addition constitutes a useful climate archive. Dating of ground water by 14C in the dissolved inorganic carbon (DIC) is standard but problematic due to the complex carbonate geochemistry. Dating of ground water based on dissolved organic carbon (DOC) has been attempted with mixed success, but now the new analytical developments enable compound-specific 14C analyses of the various DOC components, offering the chance to identify compounds suitable for dating. This project is based on the extensive experience of the collaborating scientists in 14C analytics and applications as well as in the use of glacier ice and ground water as archives, including the development and application of 14C dating methods for these systems. It will establish 14C-measurements at the MICADAS AMS of the CEZA via a gas ion source on a routine base to analyse CO2-samples in the range of 5 to 40 microgram C at a precision down to 0,5 Prozent. By improving existing sample preparation techniques for glacier ice samples, reliable 14C values of the particulate and dissolved organic fractions from small (some 100 g) ice samples shall be obtained. This capability will be applied to constrain ages of cold, sedimentary glaciers as well as of small scale, cold Alpine congelation ice bodies. The project will further develop and test the tools required for micro-scale, compound-specific radiocarbon dating of ground water via its organic fraction. For this purpose, ground water samples from the Upper Rhine Graben area will be analysed, where extensive isotopic data, including DIC 14C values, are available for comparison.
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