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Title: Deposition and dose from the May 18, 1980 eruption of Mount St. Helens

Conference ·
OSTI ID:6720267

The downwind deposition and radiation dose have been calculated for the tropospheric part of the ash cloud from the May 18, 1980 eruption of Mount St. Helens, using a large-cloud diffusion model. At that time the naturally occurring radionuclides of radium and thorium, whose radon daughters normally seep very slowly from the rocks and soil, were violently released to the atmosphere. The largest dose to an individual from these nuclides is small (in the microrem range), but the population dose to those affected by the radioactivity in the ash is about 100 person-rem. This population dose from Mount St. Helens is much greater than the annual person-rem routinely released by a typical large nuclear power plant. It is estimated that subsequent eruptions of Mount St. Helens have doubled or tripled the person-rem calculated for the initial large eruption; this total population dose is about the same as the lower-bound estimate of the population dose from the 1979 accident at the Three Mile Island nuclear power plant. The long-range global ash deposition of the May 18 eruption has been estimated through 1984, using a global deposition model. The maximum deposition is nearly 1000 kg/km/sup 2/ and occurs in the spring of 1981 over middle latitudes of the Northern Hemisphere.

Research Organization:
California Univ., Livermore (USA). Lawrence Livermore National Lab.
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
6720267
Report Number(s):
UCRL-85084; CONF-801160-1; TRN: 81-001992
Resource Relation:
Conference: Symposium and workshop on the Mount St. Helens eruption, Washington, DC, USA, 18 Nov 1980
Country of Publication:
United States
Language:
English