922 resultados para ATOMIC-BOMB SURVIVORS


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"DNA 6034F."

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Mode of access: Internet.

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"April 1969."

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"DNA 6033F."

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"DNA 6005F."

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"5 February 1981."

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The purpose of this study was to investigate how the Truman administration used fear to generate popular support for its Cold War foreign policies. Three issues were examined through the use of published government documents, personal memoirs, and weekly periodicals to assess the responses of the American public: the enactment of universal military training (UMT), the Soviet detonation of an atomic device, and the Truman administration's decision to build the hydrogen bomb. This study shows that the changing attitudes in the Truman administration toward the Soviet Union occurred in a climate of fear. Through press releases and by exerting influence on the media, the administration attempted to control the information the public received. Through the use of propaganda, the Truman administration pursued the implementation of UMT, generated fear of the Soviet Union after its detonation of the atomic bomb, and gained relative public support for the decision to build the hydrogen bomb.

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Concentrations of Cd, Pb, Zn, Cu, Co, Ni, Fe, and Al203, water content, the amounts of organic carbon, the ratio of 13C/12C and the 14C-activity of the organic fraction were determined with sediment depth from a 34 cm long box-core from the Bornholm Basin (Baltic Sea). The average sedimentation rate was 2.4 mm/yr. The upper portion of the core contained increasing amounts of 14C-inactive organic carbon, and above 3 cm depth, man-made 14C from atomic bomb tests. The concentrations of the heavy metals Cd, Pb, Zn, and Cu increase strongly towards the surface, while other metals, as Fe, Ni and Co remain almost unchanged. This phenomenon is attributed to anthropogenic influences. A comparison of the Kieler Bucht, the Bornholm and the Gotland Basins shows that today the anthropogenic addition of Zn is about 100 mg/m**2 yr in all three basins. The beginning of this excess of Zn, however, is delayed by about 20 years in, the Bornholm Basin and by about 40 years in the Gotland Basin. It is suggested that SW-NE transport of these anthropogenically mobilized metals may be related to periodic bottom water renewal in the Baltic Sea sedimentary basins.