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1.
J Environ Radioact ; 208-209: 106047, 2019 Nov.
Artículo en Inglés | MEDLINE | ID: mdl-31526956

RESUMEN

As part of an underground gas migration study, two radioactive noble gases (37Ar and 127Xe) and two stable tracer gases (SF6 and PFDMCH) were injected into a historic nuclear explosion test chimney and allowed to migrate naturally. The purpose of this experiment was to provide a bounding case (natural transport) for the flow of radioactive noble gases following an underground nuclear explosion. To accomplish this, soil gas samples were collected from a series of boreholes and a range of depths from the shallow subsurface (3 m) to deeper levels (~160 m) over a period of eleven months. These samples have provided insights into the development and evolution of the subsurface plume and constrained the relative migration rates of the radioactive and stable gas species in the case when the driving pressure from the cavity is low. Analysis of the samples concluded that the stable tracer SF6 was consistently enriched in the subsurface samples relative to the radiotracer 127Xe, but the ratios of SF6 and 37Ar remained similar throughout the samples.


Asunto(s)
Gases Nobles/análisis , Armas Nucleares , Monitoreo de Radiación , Radiactividad , Explosiones , Nevada , Medidas de Seguridad
2.
J Environ Radioact ; 127: 127-32, 2014 Jan.
Artículo en Inglés | MEDLINE | ID: mdl-24211671

RESUMEN

Systems designed to monitor airborne radionuclides released from underground nuclear explosions detected radioactive fallout across the northern hemisphere resulting from the Fukushima Dai-ichi Nuclear Power Plant accident in March 2011. Sampling data from multiple International Modeling System locations are combined with atmospheric transport modeling to estimate the magnitude and time sequence of releases of (133)Xe. Modeled dilution factors at five different detection locations were combined with 57 atmospheric concentration measurements of (133)Xe taken from March 18 to March 23 to estimate the source term. This analysis suggests that 92% of the 1.24 × 10(19) Bq of (133)Xe present in the three operating reactors at the time of the earthquake was released to the atmosphere over a 3 d period. An uncertainty analysis bounds the release estimates to 54-129% of available (133)Xe inventory.


Asunto(s)
Contaminantes Radiactivos del Aire/análisis , Accidente Nuclear de Fukushima , Modelos Teóricos , Ceniza Radiactiva/análisis , Radioisótopos de Xenón/análisis , Atmósfera , Monitoreo de Radiación/métodos
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