937 resultados para 091301 Acoustics and Noise Control (excl. Architectural Acoustics)


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This paper seeks to delineate some preliminary factors and working methods that could work in favour of establishing a workable international export control regime for dual-use goods and technologies. Drawing on the work initiated by various United Nations initiatives and the Wassenaar Agreement, but specifically looking at the European Union export regime model, this working paper asks if and how a similar model could be adopted at the international level. Far from suggesting that the EU regime should of could be adopted on a global basis or that the regime is full-proof, the authors acknowledge that EU regulations are seen as among the most stringent of frameworks on dual-use goods and technologies available. Accordingly, this paper asks what elements of the EU’s control regime could be of international benefit after the ATT negotiations and how it could be adopted on a more international basis. Indeed, any future ATT control mechanism for dual-use items will have to draw on existing arms transfers and control regimes. It does this through an analysis of the ATT and the current discourse on dual-use goods and technologies in the negotiations, an stocktaking of the strengths and weaknesses of the EU’s export control regime and by asking what elements of the EU’s regime could be utilised for international control mechanisms after a future ATT is negotiated.

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Planktic d18O and d13C records and point count records of biogenic, volcanic, and nonvolcanic terrigenous [ice-rafted debris (IRD)] sediment components from Hole 919A in the Irminger basin, northern North Atlantic provide a comprehensive dataset from which a paleoceanographic reconstruction for the last 630 kyr has been developed. The paleoceanographic evolution of the Irminger basin during this time contains both long-term patterns and significant developmental steps. One long-term pattern observed is the persistent deposition of hematite-stained ice-rafted debris. This record suggests that the modern and late Pleistocene discharges of icebergs from northern redbed regions to the Irminger Sea lie in the low end of the range observed over the last 630 kyr. In addition, Arctic front fluctuations appear to have been the main controlling factor on the long-term accumulation patterns of IRD and planktic biogenic groups. The Hole 919A sediment record also contains a long-term association between felsic volcanic ash abundances and light d18O excursions in both interglacial and glacial stages, which suggests a causal link between deglaciations and explosive Icelandic eruptions. A significant developmental step in the paleoceanographic reconstruction based on benthic evidence was for diminished supply of Denmark Strait Overflow Water (DSOW) beginning at ~380 ka, possibly initiated by the influx of meltwater from broad-scale iceberg discharges along the east Greenland coast. There is also planktic evidence of a two-step cooling of sea surface conditions in the Irminger basin, first at ~338-309 ka and later at ~211-190 ka, after which both glacials and interglacials were colder as the Arctic front migrated southeast of Site 919. In addition to offering these findings, this reconstruction provides a longer-term geologic context for the interpretation of more recent paleoceanographic events and patterns of deposition from this region.

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F and Frev available only in microfiche

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Federal Highway Administration, Office of Research and Development, Washington, D.C.

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Mode of access: Internet.

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"Literature cited": p. 133-135.

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Federal Highway Administration, Office of Research, Washington, D.C.

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Federal Highway Administration, Washington, D.C.