387 resultados para Ramcke, Jochim Hinrich.


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Each volume has also special t.-p.

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Mode of access: Internet.

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"Das Jahr 1849 ... aus dem Jahrgange 1849 der "Neuen Jahrbücher fur Geschichte und Politik"."

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With this is bound his Samling af betaenkninger og forslag kommende den Kongelige Grònlandske handel. 1856.

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Back Row: coach John Orr, trainer, Leroy Jochim, John Whitten, Campy Russell, C.J. Kupec, Ernie Johnson, John Lockard, asst. coach Jim Dutcher

Middle Row: mngr. Cyrus Warner?, Wayman Britt, Gregory Buss, Joe Johnson, Bill Ayler, mngr. Joel Blom, mngr. ?

Front Row: co-captain Henry Wilmore, co-captain Ken Brady

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Back Row: mngr. Charles Kostantacos, Joe Johnson, Lloyd Schinnerer, Lionel Worrell, coach John Orr, Wayman Britt, William Ayler, Steve Grote, Mngr. Joel Blom, trainer Leroy Jochim

Front Row: asst. coach Jim Dutcher, Richard White?, Jake Whitten, Campy Russell, C.J. Kupec, Chuck Rogers, Don Johnston, asst. coach Bill Frieder

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Back Row: mngr. Charles Kostantacos, Joe Johnson, Lloyd Schinnerer, Lionel Worrell, coach John Orr, Wayman Britt, William Ayler, Steve Grote, Mngr. Joel Blom, trainer Leroy Jochim

Front Row: asst. coach Jim Dutcher, Richard White?, Jake Whitten, Campy Russell, C.J. Kupec, Chuck Rogers, Don Johnston, asst. coach Bill Frieder

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Poems, short stories and a novel.

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Chemical turbulence in the oscillatory catalytic CO oxidation on Pt(110) is suppressed by means of focused laser light. The laser locally heats the platinum surface which leads to a local increase of the oscillation frequency, and to the formation of a pacemaker which emits target waves. These waves slowly entrain the medium and suppress the spatiotemporal chaos present in the absence of laser light. Our experimental results are confirmed by a detailed numerical analysis of one- and two-dimensional media using the Krischer-Eiswirth-Ertl model for CO oxidation on Pt110. Different control regimes are identified and the dispersion relation of the system is determined using the pacemaker as an externally tunable wave source.

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The stable carbon isotopic signature of carbon dioxide (d13CO2) measured in the air occlusions of polar ice provides important constraints on the carbon cycle in past climates. In order to exploit this information for previous glacial periods, one must use deep, clathrated ice, where the occluded air is preserved not in bubbles but in the form of air hydrates. Therefore, it must be established whether the original atmospheric d13CO2 signature can be reconstructed from clathrated ice. We present a comparative study using coeval bubbly ice from Berkner Island and ice from the bubble-clathrate transformation zone (BCTZ) of EPICA Dome C (EDC). In the EDC samples the gas is partitioned into clathrates and remaining bubbles as shown by erroneously low and scattered CO2 concentration values, presenting a worst-case test for d13CO2 reconstructions. Even so, the reconstructed atmospheric d13CO2 values show only slightly larger scatter. The difference to data from coeval bubbly ice is statistically significant. However, the 0.16 per mil magnitude of the offset is small for practical purposes, especially in light of uncertainty from non-uniform corrections for diffusion related fractionation that could contribute to the discrepancy. Our results are promising for palaeo-atmospheric studies of d13CO2 using a ball mill dry extraction technique below the BCTZ of ice cores, where gas is not subject to fractionation into microfractures and between clathrate and bubble reservoirs.

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During the past six years organic geochemical, micropaleontological, and sedimentological investigations were carried out within the framework of the multidisciplinary bilateral German-Russian research project ''System Laptev Sea'' and detailed biological investigations within the project ''German-Russian Investigations of the Marginal Seas of the Eurasian Arctic'', In order to understand the Laptev Sea ecosystem and to obtain information about sources and fate of organic carbon, the distribution of phyto- and zooplankton, diatoms, chlorophyll a benthic macrofauna, palynomorphs, grain size, total organic carbon, d13Corg and biomarkers (n-alkanes, fatty acids) were determined. In general, the influence of the major rivers draining into the Laptev Sea, is reflected in the water column as well as in the surface sediments. In both habitats three ecological provinces can be distinguished, i.e., the southeastern Laptev Sea, the central Laptev Sea, and the northern Laptev Sea. Additionally, clear differences between the western and the eastern Laptev Sea occur. The comparison of the different data sets of the water column and the surface sediments provide information about organic carbon sources and pathways in the Laptev Sea shelf and continental slope area.