1000 resultados para Germany. Heer. 14. Reservekorps.


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Text on the back: Zur Erinnerung an den Sommer in Schoenau-Koenigsee 1921. Mollings.

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Postcard written to Therese Gottschalk nee Molling at Norderney

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Left: Freddy Godshaw (Gottschalk); right: Peter Zander

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In the apartment on Ruemkorffstrasse that the Gottschalks occupied after being forced to sell their house.

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This portrait shows Elizabeth with pig tails. In a defiant mood, she cut them off.

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Morgen hat Reserve Ruh / Auf Wiedersehen / Beste Gruesse; postcard signer Gottschalk; addressee: L Nurzinsky, Altona-Othmarschen, Aidikes Str.

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Text on the back: Zur Erinnerung an den Sommer in Schoenau-Koenigsee 1921. Mollings.

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Postcard written to Therese Gottschalk nee Molling at Norderney

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The seafloor of central Eckernförde Bay is characterised by soft muddy sediments that contain free methane gas. Bubbles of free gas cause acoustic turbidity which is observed with acoustic remote sensing systems. Repeated surveys with subbottom profiler and side scan sonar revealed an annual period both of depth of the acoustic turbidity and backscatter strength. The effects are delayed by 3–4 months relative to the atmospheric temperature cycle. In addition, prominent pockmarks, partly related to gas seepage, were detected with the acoustic systems. In a direct approach gas concentrations were measured from cores using the gas chromatography technique. From different tests it is concluded that subsampling of a core should start at its base and should be completed as soon as possible, at least within 35 min after core recovery. Comparison of methane concentrations of summer and winter cores revealed no significant seasonal variation. Thus, it is concluded that the temperature and pressure influences upon solubility control the depth variability of acoustic turbidity which is observed with acoustic remote sensing systems. The delay relative to the atmospheric temperature cycle is caused by slow heat transfer through the water column. The atmospheric temperature cycle as ‘exiting function’ for variable gas solubility offers an opportunity for modelling and predicting the depth of the acoustic turbidity. In practice, however, small-scale variations of, e.g., salinity, or gas concentration profile in the sediment impose limits to predictions. In addition, oceanographic influences as mixing in the water column, variable water inflow, etc. are further complications that reduce the reliability of predictions.