1987
DOI: 10.1524/ract.1987.41.4.181
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Ground Depositions and Air Concentrations of Chernobyl Fallout Radionuclides at Munich-Neuherberg

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Cited by 103 publications
(25 citation statements)
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“…In the figure, the vertical profiles are shown for Chernobyl-derived l34 Cs, for ,37 Cs due to weapons fallout ( ,J7 Cs-f), and for stable Cs. The '"Cs-f was calculated using an isotopic ratio of '"Cs/ lw Cs = 1.75 for Chernobyl cesium on 1 May 1986 [ 15]. The profile for ,34 Cs shows a maximum in the Of and Oh layers, being lower in the litter layer and the mineral horizons, as reported in many papers.…”
Section: Vertical Distributions In Soilsmentioning
confidence: 77%
“…In the figure, the vertical profiles are shown for Chernobyl-derived l34 Cs, for ,37 Cs due to weapons fallout ( ,J7 Cs-f), and for stable Cs. The '"Cs-f was calculated using an isotopic ratio of '"Cs/ lw Cs = 1.75 for Chernobyl cesium on 1 May 1986 [ 15]. The profile for ,34 Cs shows a maximum in the Of and Oh layers, being lower in the litter layer and the mineral horizons, as reported in many papers.…”
Section: Vertical Distributions In Soilsmentioning
confidence: 77%
“…Therefore, we have recently started to investigate the potential of 239+240 Pu from global fallout (Pu) as a tracer of soil movement in a steep field (inclination 20%) near Scheyern in Bavaria. Plutonium was also deposited by the Chernobyl fallout, but in Germany the amount of this fraction is negligible (<1% of the total inventory, Hötzl et al 1987). In an earlier paper (Schimmack et al 2001), we compared the activity patterns of Cs and Pu.…”
Section: Introductionmentioning
confidence: 99%
“…For this reason, 134 Cs was also determined in all soil samples. The fraction of Chernobyl-derived 137 Cs from the 137 Cs and 134 Cs measured in the samples can then be obtained for each soil sample by using the ratio of 137 Cs/ 134 Cs=1.75, as observed on 30 April 1986 in the deposition in Bavaria/Germany [3].…”
Section: Soil Typesmentioning
confidence: 99%
“…To obtain the values of k i for a given radionuclide in a given soil layer, the differential equation system of Eqs. (3)(4) is integrated numerically. The values for k i are varied until the compartment activity matches the observed activity in this compartment.…”
Section: Compartment Modelmentioning
confidence: 99%