Migration of 137Cs in tributaries, lake water and sediment of Lago Maggiore (Italy, Switzerland) - analysis and comparison with Lago di Lugano and other lakes.
This paper describes the behaviour of 137Cs in Lago Maggiore and other pre-alpine lakes as a consequence of atmospheric nuclear weapons testing fallout and the fallout from the nuclear accident in Chernobyl. It presents data on the 137Cs distribution in tributaries, lake water, bottom sediments and reveals the role of (137)Cs as a marker of the sedimentation processes. The run-off of 137Cs from the watershed to the lake is described with a simple compartment model. Measurements of the activity concentration of (137)Cs in sediments are compared with the output of a model (diffusion-convection type) which describes the input of 137Cs into and its vertical distribution within the sediment. Varying sedimentation rates (0.05-0.90g(cm2y)(-1)) in Lago Maggiore are compared with data of other authors. Sedimentation rates and total distribution coefficients (of about 10(5) Lkg(-1)) in Lago Maggiore are discussed and compared with those of Lago di Lugano, Lake Constance, and Lake Vorsee.
Putyrskaya
Victoria
V
Hochschule Ravensburg-Weingarten, University of Applied Sciences, Doggenriedstr., D-88250 Weingarten, Germany.
Klemt
Eckehard
E
Röllin
Stefan
S
D002586:Cesium / Q000737:chemistry*; D002588:Cesium Radioisotopes / Q000737:chemistry; D047852:Chernobyl Nuclear Accident; D005618:Fresh Water / Q000737:chemistry*; D019015:Geologic Sediments / Q000737:chemistry*; D006863:Hydrogen-Ion Concentration; D007558:Italy; D054043:Nuclear Weapons; D010100:Oxygen / Q000737:chemistry; D011847:Radioactive Fallout; D013557:Switzerland; D013696:Temperature; D014872:Water Movements
D002588:Cesium Radioisotopes; D011847:Radioactive Fallout; D002586:Cesium; D010100:Oxygen