Der Kartenviewer ist eine Standardanwendung des GeoSN. Durch Verwendung von Parametern kann die Kartenansicht individuell angepasst werden. Werden bspw. Koordinaten oder eine Adresse kombiniert mit einer speziellen Zoomstufe in die Webadresse integriert, so startet der Kartenviewer an einer bestimmten Position und in einem entsprechenden Maßstab. Wahlweise kann die Position mit einem Pin markiert werden. Ab 1:10.000 werden die Haltestellen des ÖPNV sichtbar. Weitere Parameter für das Starten der eigenen Kartenansicht sind bspw. ein spezielles Flurstück, eine weitere Webkarte (WMS), die über eine URL erreicht werden kann oder eine im Web befindliche KML-Datei mit eigenen Inhalten. Diese Anwendung eignet sich insbesondere, um schnell und unkompliziert Anfahrts- oder Eventkarten zu erstellen und in eigene Webseiten zu integrieren. Der Kartenviewer wird ständig weiterentwickelt. Die einzelnen Parameter und deren Syntax erfragen Sie bitte beim Service Desk des GeoSN (siehe Kontakt).
Raw navigation data acquired by the navigation system of the Senckenberg during the expedition SEN2212 which took place on the 3rd of May 2022 between Jade and Wangerooge in the German North Sea coast. The track was acquired with a Hemisphere Cresent R131RCVR GPS antenna and recorded with the Ocean Floor Observation Protocol (OFOP) software. No further processing was undertaken. The data is provided as a master track with 1 sec resolution derived from the position sensors' data. This cruise was an activity of the CONMAR project of the DAM research mission "Protection and Sustainable Use of Marine Areas".
The thermal conductivity on cores is measured in two steps (see Pribnow 1994). First, one face end of the core is sawed and polished. The half space line source is pressed against this preparated face (without further contact medium like water) by a computerized device. The position of the heat source is varied in 15 degree intervals around one semicircle. At each position, 3 repeating measurements are performed. The line source azimuth of the lowest measured thermal conductivity is the strike of the foliation plane. On the other hand, the thermal conductivity is maximal parallel to that direction. This apparent paradox can be explained by the experimental method, because the measurement plane is perpendicular to the orientation of the line source (Pribnow 1994).In a second step a calotte plane perpendicular to the strike of foliation is prepared. A second series of thermal conductivity measurements in 15 degree intervals ...
The thermal conductivity on cores is measured in two steps (see Pribnow 1994). First, one face end of the core is sawed and polished. The half space line source is pressed against this preparated face (without further contact medium like water) by a computerized device. The position of the heat source is varied in 15 degree intervals around one semicircle. At each position, 3 repeating measurements are performed. The line source azimuth of the lowest measured thermal conductivity is the strike of the foliation plane. On the other hand, the thermal conductivity is maximal parallel to that direction. This apparent paradox can be explained by the experimental method, because the measurement plane is perpendicular to the orientation of the line source (Pribnow 1994).In a second step a calotte plane perpendicular to the strike of foliation is prepared. A second series of thermal conductivity measurements in 15 degree intervals ...