995 resultados para 509.66


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Lt. General Holland M. Smith and other Marine officers examining maps and other documents around a table in field. No caption.

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Mode of access: Internet.

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Publisher's no.: 3955.

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Trägerband: 'L.lat.lex. 517'; Vorbesitzer: Dominikanerkloster Frankfurt am Main

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Trägerband: 15/474; Vorbesitzer: Dominikanerkloster Frankfurt am Main

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The article expands existing categorisations of political and economic governance by including literature on less developed countries (LDCs). In four consecutive negotiations between the US multinational Kaisers and the US and Ghana governments in the early 1960s, it is argued that the company reached levels of influence that are at odds with existing explanations. In order to understand corporate political activities in LDCs, analysis needs to go beyond static factors (political risk) and include dynamic factors such as diplomatic relations and 'arenas of power', and consider the role of the investor's home country relative to the host economy.

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http://digitalcommons.fiu.edu/com_images/1071/thumbnail.jpg

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Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (<5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.

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Trägerbände: Inc. qu. 979; Inc. oct. 271 Bd. 1; Vorbesitzer: Dominikanerkloster Frankfurt am Main