| Literature DB >> 23619806 |
Peter Saetre1, Jack Valentin, Per Lagerås, Rodolfo Avila, Ulrik Kautsky.
Abstract
The radiation doses to humans resulting from a potential release of radionuclides from a geological repository for long-lived waste are assessed over tens or even hundreds of thousands of years. Ingestion is expected to be the major exposure pathway, and the group with the highest exposures will be those that consume the most contaminated food. In this paper, we characterize the group of individuals with the highest exposures by considering the physical and biological characteristics of the contaminated area and human requirements for energy and nutrients. We then calculate intake rates based on land-use scenarios drawn from self-sustained communities spanning prehistoric times to an industrial-age agrarian culture. The approach is illustrated by simulating groundwater release of four radionuclides to an expected discharge area. We argue that the derived intake rates may serve as credible bounding cases when projected doses are evaluated for compliance with regulatory criteria.Entities:
Mesh:
Year: 2013 PMID: 23619806 PMCID: PMC3636367 DOI: 10.1007/s13280-013-0400-z
Source DB: PubMed Journal: Ambio ISSN: 0044-7447 Impact factor: 5.129
Exposure through ingestion for ecosystems expected to receive direct or indirect releases of contaminated groundwater from a geological repository. Environmental media and examples of contaminated food items are listed together with self-sustaining human cultures associated with habits and land-uses expected to result in high intake rates
| Ecosystem | Environmental media | Pathways | Food items | Most exposed group |
|---|---|---|---|---|
| Sea | Sea water and surface sediments | Marine food web | Fish | Fisherman, Hunter-gatherer |
| Lake/stream | Lake water and surface sediments | Fresh water food web | Fish, Crayfish | Hunter-gatherer |
| Mire | Mire sediments (peat) | Mire food webs | Fungi, Berries, Game | Hunter-gatherer |
| Peat/agricultural soil | Haymaking/fertilization | Meat, milk/crops | Farmer | |
| Arable | Agricultural soil | Draining and cultivation of peat | Meat, milk, crops | Farmer |
Land use and consumption of an Iron-Age family farm, corresponding to 6 adult individuals. Calculations assume a mixed herd of livestock (7 cows, 3 heifers, 3 oxen, 5 pigs, and 16 sheep) with milk cows making up less than half of the animal stock. Updated from Widgren (1979)
| Land use | Area (ha) | Food item | Productivity (kg year−1 m−2) | Calorie content (kcal/kg) | Yearly production (kcal) | Daily consumption (kcal/individual) |
|---|---|---|---|---|---|---|
| Arable | 3 | Cereal | 0.05 | 3200 | 4 800 000 | 2192 |
| Meadow | 30 | Dairy productsb | 0.0047 | 400 | 1 116 000 | 510 |
| Pasturea | 30 | Meatb | 0.0005 | 2000 | 600 000 | 274 |
| 2975 |
aMinimum area of pasture assuming primary productivity as meadow (500 kg hay/ha)
bMeat and dairy product productivity expressed per unit area of pasture and meadows combined
Fig. 1Cultivation of a drained mire. ‘Autumn Ploughing in the Marshland’, painting by Ester Almqvist 1911 (photo Hossein Sehatlou). Gothenburg Museum of Art
Fig. 2Use of agricultural land (a) and corresponding productivity (b) at the turn of the nineteenth century in Sweden. The numbers are based on official national statistics from the Swedish Board of Agriculture. The productivity from animal husbandry (*) has been calculated with respect to the area of green fodder and two thirds of the area used for cereal and root crop production, respectively
Fig. 3Intake rates (Bq year−1) of contaminated food given a unit release rate (1 Bq year−1) of contaminant for three land-use scenarios (green agriculture in the industrial period, blue hunter-gatherers, red infield-outland farming system) and four radionuclides (top left Ni-59, top right Np-237, bottom left Ra-226, bottom right Se-79). The results are based on simulations of one discharge area that develops from a sea basin into a lake–mire ecosystem. Vertical lines represent the start of lake isolation (a), time when discharge area is 2 m above sea level (b), and the time when the mire has grown to fully cover the original lake basin (c)