Der Kartendienst (WMS-Gruppe) stellt die Geodaten aus dem Bereich Bergbau bereit.:Betriebe unter Bergaufsicht im Saarland, Standorte, Sole, Bundesberggesetz (BBergG)
Bebauungspläne und Umringe der Gemeinde Kleinblittersdorf Ortsteil Rilchingen-Hanweiler (Saarland):Bebauungsplan "Sole-Thermalbad 1.Änderung" der Gemeinde Kleinblittersdorf, Ortsteil Rilchingen-Hanweiler
Bebauungspläne und Umringe der Gemeinde Kleinblittersdorf Ortsteil Rilchingen-Hanweiler (Saarland):Bebauungsplan "Sole-Thermalbad 3 Änderung" der Gemeinde Kleinblittersdorf, Ortsteil Rilchingen-Hanweiler
Bebauungspläne und Umringe der Gemeinde Kleinblittersdorf Ortsteil Rilchingen-Hanweiler (Saarland):Bebauungsplan "Sole-Thermalbad 4 Aenderung" der Gemeinde Kleinblittersdorf, Ortsteil Rilchingen-Hanweiler
Bebauungspläne und Umringe der Gemeinde Kleinblittersdorf Ortsteil Rilchingen-Hanweiler (Saarland):Bebauungsplan "Sole-Thermalbad 2 Änderung" der Gemeinde Kleinblittersdorf, Ortsteil Rilchingen-Hanweiler
Bebauungspläne und Umringe der Gemeinde Kleinblittersdorf Ortsteil Rilchingen-Hanweiler (Saarland):Bebauungsplan "Sole-Thermalbad" der Gemeinde Kleinblittersdorf, Ortsteil Rilchingen-Hanweiler
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Das Projekt "Sub project: The Geothermal Field of the Chesapeake Bay Impact Structure" wird vom Umweltbundesamt gefördert und von Karlsruher Institut für Technologie (KIT), Geophysikalisches Institut durchgeführt. Within the frame of the aims of the ICDP Chesapeake Bay Impact Structure (CBIS) Project, we want to investigate the present geothermal and hydraulic regime of the central part of this impact structure. To reach this aim we will determine local vertical and lateral regional heat flow variations in the CBIS area in cooperation with our partners in Moscow, Prague and colleagues from USGS. The results of this investigation will contribute to the hydrogeological research with respect to the threatening of the fresh groundwater resources of the region by the CB impact brines. Another aim of our project is to extend the variability of common models for the interpretation of transient thermal signals to time-varying boundary conditions, as they exist in boreholes caused e.g. by artesian outflow of water.
Das Projekt "The role of sympagic meiofauna for the flow of organic matter and energy in the Antarctic and Arctic sea-ice foodwebs" wird vom Umweltbundesamt gefördert und von Universität Kiel, Institut für Polarökologie durchgeführt. The brine channels in sea ice (Fig. 1) of both polar regions are the habitat of sympagic (ice-associated) bacteria, algae, protozoans and small metazoans greater than 20 mym (meiofauna, Fig. 2), including copepods, plathyelminthes, rotifers, nematodes, cnidarians, nudibranchs and ctenophores. Primary production of sympagic algae forms the basis of the sea-ice food web, which is coupled to the pelagic ecosystem and higher trophic levels. The overall objective of this project is to reveal the qualitative and quantitative role of sympagic meiofauna for the flow of organic matter and energy in the Antarctic and Arctic sea-ice foodwebs. The major focus is on sympagic meiofauna because this group could, due to in part very high abundances, play an important role within the sea-ice ecosystem. Moreover, since sympagic metazoans are a food source for higher trophic levels (e.g. larger zooplankton, fish), they probably occupy a key position in coupling processes between the sea ice and pelagic ecosystems. Sympagic meiofauna can thus be supposed to significantly contribute to the flow of organic matter and energy in polar marine food webs. In spite of this, little information on the feeding ecology of this group is available as yet.
Das Projekt "Sub project: The Geothermal Field of the Chesapeake Bay Impact Structure" wird vom Umweltbundesamt gefördert und von Karlsruher Institut für Technologie (KIT), Geophysikalisches Institut durchgeführt. Within the frame of the aims of the ICDP Chesapeake Bay Impact Structure (CBIS) Project, our primary goal is to perform an investigation of the present geothermal and hydraulic regime of the central part of this impact structure. To reach this aim we will determine local and regional heat flow variations in lateral and vertical direction in the CBIS area in cooperation with our partners in Berlin, Moscow, Prague and colleagues from USGS. The results of this investigation will contribute to the hydro-geological research concerning the threatening of the fresh groundwater resources of the region by the CB impact brines. Another aim of our project is to investigate the possibilities to extend the variability of the models for the interpretation of transient thermal signals, caused in boreholes e.g. by artesian outflow of water.