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Found 391 results.

Vereine, Gemeinschaften, Vertretungen und Verbände Erkrath

Lage aller Zusammenkünfte verschiedenster Interessengemeinschaften im Stadtgebiet Erkrath.

Staatliche_Dienste - Einr_allg_polit_Weit - OGC WFS Interface

Der Kartendienst (WFS-Gruppe) stellt die Standorte der öffentlichen Landesverwaltung und der Kommunen dar.:Einrichtungen allgemeiner politischer Weiterbildung im Saarland

Schulen Landkreis Lüneburg

Im Landkreis Lüneburg gibt es ein flächendeckendes Angebot an allgemeinbildenden Schulen. Dazu gehören die Grundschulen, Hauptschulen, Realschulen, Gymnasien, Gesamtschulen und Förderschulen. Je nach Schulform unterscheiden sich die Zugangsvoraussetzungen, pädagogischen Konzepte und Abschlüsse. Die Daten zeigen die Standorte der Schulen des Landkreises nach Schulform.

Kindertageseinrichtungen Landkreis Lüneburg

Standorte verschiedener Kindertageseinrichtungen im Landkreis Lüneburg

WMS MRH Wissenschaft und Forschung

Web Map Service (WMS) zum Thema MRH Wissenschaft und Forschung. Zur genaueren Beschreibung der Daten und Datenverantwortung nutzen Sie bitte den Verweis zur Datensatzbeschreibung.

INSPIRE Download Service (predefined ATOM) für Datensatz Schulen Saarland

Beschreibung des INSPIRE Download Service (predefined Atom): Darstellung der Schulen im Saarland; Erfassung durch das Geodatenzentrum, anhand von Listen des Ministerium für Bildung (Bildungsserver) und Luftbildern, Hauskoordinaten. Erfasste Schulen: - Grundschulen - Realschulen - Erweiterte Realschulen - Gesamtschulen - Gymnasien - Förderschulen - Freie Waldorfschulen - Berufsschulen - Binationale Schulen - Hochschulen Beschreibung der Attributtabelle: KREIS--------: Landkreis Nummer RW-----------: Rechtswert HW-----------: Hochwert PLZ----------: Postleitzahl ORT_NAME-----: Ortsname POST_ORT-----: Ortsname Postanschrift HNR----------: Hausnummer ADZ----------: Hausnummer Zusatz SCHULFORM----: Schulform, Schulbezeichnung SCHULNAME----: Name der Schule 2_SCHULEN----: weitere Schulen im gleichen Gebäude 3_SCHULEN----: weitere Schulen im gleichen Gebäude 4_SCHULEN----: weitere Schulen im gleichen Gebäude SCHULREGION--: Name der Schulregion ERFASSUNG----: Erfasser und Datum SCHULKENN----: Schulkennziffer - Der/die Link(s) für das Herunterladen der Datensätze wird/werden dynamisch aus GetFeature Anfragen an einen WFS 1.1.0+ generiert

Biopores in the subsoil: Formation, nutrient turnover and effects on crops with distinct rooting systems (BioFoNT)

Perennial fodder cropping potentially increases subsoil biopore density by formation of extensive root systems and temporary soil rest. We will quantify root length density, earthworm abundance and biopore size classes after Medicago sativa, Cichorium intybus and Festuca arundinacea grown for 1, 2 and 3 years respectively in the applied research unit's Central Field Trial (CeFiT) which is established and maintained by our working group. Shoot parameters including transpiration, gas exchange and chlorophyll fluorescence will frequently be recorded. Precrop effects on oilseed rape and cereals will be quantified with regard to crop yield, nutrient transfer and H2-release. The soil associated with biopores (i.e. the driloshpere) is generally rich in nutrients as compared to the bulk soil and is therefore supposed to be a potential hot spot for nutrient acquisition. However, contact areas between roots and the pore wall have been reported to be low. It is still unclear to which extent the nutrients present in the drilosphere are used and which potential relevance subsoil biopores may have for the nutrient supply of crops. We will use a flexible videoscope to determine the root-soil contact in biopores. Nitrogen input into the drilosphere by earthworms and potential re-uptake of nitrogen from the drilosphere by subsequent crops with different rooting systems (oilseed rape vs. cereals) will be quantified using 15N as a tracer.

The importance of peripheral oceanic processes in the Labrador Sea for the Atlantic meridional overturning circulation

The Labrador Sea is one of the few places in the world ocean, where deep water formation takes place. This water is exported from the Labrador Sea to become part of the southward branch of the meridional overturning circulation. Previous observational work has largely focused on the role of deep convection in the interior of the Labrador Sea. Recent evidence from observations and numerical ocean models specifically indicate that processes near the ocean boundaries might be most relevant for both Eulerian downwelling of waters in the Labrador Sea and the fast export of newly transformed waters. We propose to analyze mooring based observations at the western margin of the Labrador Sea together with high resolution numerical model simulations to understand the role both processes play for the meridional overturning circulation in the subpolar North Atlantic. Specifically, we want to test (i) if (and where) downwelling occurs along the margins of the Labrador Sea, (ii) how downwelling relates to the seasonal evolution of convection and eddy activity, (iii) how fast waters newly transformed near the western margin of the Labrador Sea are exported, and (iv) how the two processes (downwelling, fast export) affect the temporal variability of the Atlantic meridional overturning circulation.

Coordination and administration of the priority programme SPP 1315 Biogeochemical Interfaces in Soil, Biotic and abiotic factors that dive the function of microbial communities at biogeochemical interfaces in different soils (BAMISO)

Biogeochemical interfaces shape microbial community function in soil. On the other hand microbial communities influence the properties of biogeochemical interfaces. Despite the importance of this interplay, basic understanding of the role of biogeochemical interfaces for microbial performance is still missing. We postulate that biogeochemical interfaces in soil are important for the formation of functional consortia of microorganisms, which are able to shape their own microenvironment and therefore influence the properties of interfaces in soil. Furthermore biogeochemical interfaces act as genetic memory of soils, as they can store DNA from dead microbes and protect it from degradation. We propose that for the formation of functional biogeochemical interfaces microbial dispersal (e.g. along fungal networks) in response to quality and quantity of bioavailable carbon and/or water availability plays a major role, as the development of functional guilds of microbes requires energy and depends on the redox state of the habitat.To address these questions, hexadecane degradation will be studied in differently developed artificial and natural soils. To answer the question on the role of carbon quantity and quality, experiments will be performed with and without litter material at different water contents of the soil. Experiments will be performed with intact soil columns as well as soil samples where the developed interface structure has been artificially destroyed. Molecular analysis of hexadecane degrading microbial communties will be done in vitro as well as in situ. The corresponding toolbox has been successfully developed in the first phase of the priority program including methods for genome, transcriptome and proteome analysis.

Biogenic formation of non-extractable residues from pesticides in soil

During microbial turnover of organic chemicals in soil, non-extractable residues (NER) are formed frequently. Studies on NER formation usually performed with radioisotope labelled tracer compounds are limited to localisation and quantitative analyses but their chemical composition is left unknown. Recently, we could show for 2,4-dichlorophenoxyacetic acid and ibuprofen that during microbial turnover in soil nearly all NER were derived from microbial biomass, since degrading bacteria use the pollutant carbon for their biomass synthesis. Their cell debris is subsequently stabilised within soil organic matter (SOM) forming biogenic NER (bioNER). It is still unknown whether bioNER are also formed during biodegradation of other, structurally different compound classes of organic contaminants. Therefore, agricultural soil will be incubated with labelled compounds of five classes of commonly used and emerging pesticides: organophosphate, phenylurea, triazinone, benzothiadiazine and aryloxyphenoxypropionic acid. The fate of the label will be monitored in both living and non-living SOM pools and the formation of bioNER will be quantified for each compound over extended periods of time. In addition, soil samples from long-term lysimeter studies with 14C-labelled pesticide residues (e.g. triazine, benzothiazole and phenoxypropionic acid group) will be also analysed for bioNER formation. The results will be summarised to identify the metabolic conditions of microorganisms needed for bioNER formation and to develop an extended concept of risk assessment including bioNER formation in soils.

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