API src

Found 524 results.

Pegel im Odergebiet: Hohensaaten-Finow, Oder

Der Pegel Hohensaaten-Finow wurde als Lattenpegel im Jahr 1853 in unmittelbarer Nähe zum Flusslauf der Oder an der ehemaligen Finow-Schleuse errichtet. Die Schleuse fungierte als Bindeglied zwischen dem Finow-Kanal und der Oder. Nach Verfüllung der Schleuse in den 1960er Jahren verblieb eine buchtartige Erweiterung des Flusses, an welcher der Pegel weiterhin betrieben wird. Die Wasserstandsbeobachtungen an dem Pegel sind seit dem Abflussjahr 1901 im Gewässerkundlichen Jahrbuch veröffentlicht. In den Gewässerkundlichen Jahrbüchern 1901-1934 trägt der Pegel den Namen Pegel Hohensaat(h)en, Schleuse bzw. Finowschleuse, seit 1935 wird die heutige Bezeichnung Pegel Hohensaaten-Finow verwendet. Tägliche Durchflusswerte sind im Gewässerkundlichen Jahrbuch ab Jahrgang 1959 enthalten. Der Pegel wurde im Oktober 1979 mit einem Schreibpegel ausgerüstet. Höhe des Pegelnullpunktes: vor  01.11.1926   NN+ 0,128 m ab   01.11.1926   NN+ 0,143 m  (Änderung des Höhensystems; die Höhenlage des Pegels zum Gelände hat sich nicht geändert) ab   01.11.1959   NN+ 0,16   m  (Neufeststellung; die Höhenlage des Pegels zum Gelände hat sich nicht geändert) ab   01.11.2010   NHN+ 0,149 m (Umstellung auf das Höhensystem DE_DHHN92_NH_BB/NHN/160)

Geochemical composition of S1 sediment core from Lower Odra Valley, NW Poland

Oxbow lakes are continuous archives of flood events. On 28th June 2022 a 7.5 m long bottom sediment core (S1: 53.24758°N and 14.46271°E, 2.4 m b.s.l.) was collected from an oxbow lake in the Lower Odra Valley, NW Poland. Drilling was conducted using an Instorf sampler (Russian type; chamber dimension: 10 x 50 cm), onboard a "Manat" catamaran motorboat. After core recovery, each half-metre section was packed into a PVC tube and kept in cool rooms with a constant temperature. Samples were collected every 4 cm. For the first 2 m of the core grain-size, geochemical and Chironomidae analyses as well as radiocarbon dating were performed, which allow to identify flood events in the last 3200 years.

Chironomidae based temperature reconstructions from S1 sediment core, Lower Odra Valley, NW Poland

Oxbow lakes are continuous archives of flood events. On 28th June 2022 a 7.5 m long bottom sediment core (S1: 53.24758°N and 14.46271°E, 2.4 m b.s.l.) was collected from an oxbow lake in the Lower Odra Valley, NW Poland. Drilling was conducted using an Instorf sampler (Russian type; chamber dimension: 10 x 50 cm), onboard a "Manat" catamaran motorboat. After core recovery, each half-metre section was packed into a PVC tube and kept in cool rooms with a constant temperature. Samples were collected every 4 cm. For the first 2 m of the core grain-size, geochemical and Chironomidae analyses as well as radiocarbon dating were performed, which allow to identify flood events in the last 3200 years.

Grain-size analysis of S1 sediment core from Lower Odra Valley, NW Poland

Oxbow lakes are continuous archives of flood events. On 28th June 2022 a 7.5 m long bottom sediment core (S1: 53.24758°N and 14.46271°E, 2.4 m b.s.l.) was collected from an oxbow lake in the Lower Odra Valley, NW Poland. Drilling was conducted using an Instorf sampler (Russian type; chamber dimension: 10 x 50 cm), onboard a "Manat" catamaran motorboat. After core recovery, each half-metre section was packed into a PVC tube and kept in cool rooms with a constant temperature. Samples were collected every 4 cm. For the first 2 m of the core grain-size, geochemical and Chironomidae analyses as well as radiocarbon dating were performed, which allow to identify flood events in the last 3200 years.

Chironomidae composition of S1 sediment core from Lower Odra Valley, NW Poland

Oxbow lakes are continuous archives of flood events. On 28th June 2022 a 7.5 m long bottom sediment core (S1: 53.24758°N and 14.46271°E, 2.4 m b.s.l.) was collected from an oxbow lake in the Lower Odra Valley, NW Poland. Drilling was conducted using an Instorf sampler (Russian type; chamber dimension: 10 x 50 cm), onboard a "Manat" catamaran motorboat. After core recovery, each half-metre section was packed into a PVC tube and kept in cool rooms with a constant temperature. Samples were collected every 4 cm. For the first 2 m of the core grain-size, geochemical and Chironomidae analyses as well as radiocarbon dating were performed, which allow to identify flood events in the last 3200 years.

Stable isotope and hydrochemical composition of fresh water in rivers of the Basin of Pöhlde, and the Rhume karst springs, Germany, under different seasonal and discharge conditions

The hydrochemical and stable isotope composition of fresh surface water in rivers (Sieber and Oder) of a karst area in the southwestern foreland of the Harz Mountains, Germany, was investigated at several occasions between years 1986 and 1992. The campaigns covered different seasonal and hydrological (discharge) conditions, including a snow-melt induced high water at the rivers. Aim of the study was the investigation of the impact of discharge conditions at the river water loosing water to underground passage in the Basin of Pöhlde, dissolving carbonate and sulfate minerals in the karst aquifers, and reappearing in the karst springs of the Rhume river. Besides physical characterization, hydrochemical major and minor elements were measaured, as weill as the carbon isotope composition of DIC, the sulfur and oxygen isotope composition of sulfate, and the oxygen isotope composition of water. Results reflect the impact of hydrological conditions on the subterrestrial carbon and sulfur cycles.

Bebauungsplan Nr. 215 Am Kirschenbrink

Die Stadt Goslar verfügt über ca. 600 analoge und digitale Bebauungspläne.

Bebauungsplan Nr. 212 Oker Mitte

Die Stadt Goslar verfügt über ca. 600 analoge und digitale Bebauungspläne.

Bebauungsplan Nr. 232.A.4 Bei der Eiche

Die Stadt Goslar verfügt über ca. 600 analoge und digitale Bebauungspläne.

Bebauungsplan Nr. 232.A.2 Bei der Eiche

Die Stadt Goslar verfügt über ca. 600 analoge und digitale Bebauungspläne.

1 2 3 4 5 … 51 52 53