Logic Colloquium '80 (no TOC) by Dirk van Dalen, etc.

By Dirk van Dalen, etc.

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There are numerous historical orphan sources throughout the world, which may become mixed with previously uncontaminated soils. The fact that many uranium ores have activity concentrations much higher than those reported in UNSCEAR for 226Ra suggests that there must be some soils contaminated with orphan sources of TENORM with activity concentrations of 226Ra of the order of 103 Bq kgÀ1. 3. , Lucas, 1964; Lockart, 1964; Tanner, 1964, 1980; Tanner and Olsen, 1992). Activity concentrations of 222Rn outdoors vary from o1 up to a few tens of Bq mÀ3 (Gesell, 1983; NAS-NRC, 1999).

0 19 Source: Adapted from US DoE (2001). Note: - Means decomposes to Solubility -UO2F2 Slightly soluble Soluble Insoluble Insoluble Insoluble Known global inventory of depleted uranium with distribution by country, metric tons, chemical form, and percentage. 926 USEC, former United States Enrichment Corporation; COGEMA, “Compagnie Générale des Matières Nucléaires” which is today AREVA NC; EURODIF, European Gaseous Diffusion Uranium Enrichment Consortium; BNFL, British Nuclear Fuels; URENCO, the joint industrial enterprise established under the Treaty of Almelo; JNFL, Japan Nuclear Fuel Limited; JNC, Japan Nuclear Fuel Cycle Development Institute; CNNC, China National Nuclear Corporation; KAERI, Korea Atomic Energy Research Institute; NECSA, Nuclear Energy Corporation of South Africa.

5 – and STh is the measured activity concentration measured through the 208Tl photo-peak (in Bq kgÀ1), SU is the activity concentration measured through the 214Bi photopeaks (in Bq kgÀ1), and SK is the activity concentration measured through the 40K photo-peak (in Bq kgÀ1). 0, and CTh, CU, CK are, respectively, the concentrations of Th, U, and K in soil. 2) were reported to be 8, 11, and 4%, respectively. These relative estimates 34 Technologically Enhanced Natural Radiation and corresponding errors are based on the geological formations under the soils measured.

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