Anthropogenic ¹²⁹I in the atmosphere: Overview over major sources, transport processes and deposition pattern

Wet and, to a lesser extent, dry deposition of atmospheric ¹²⁹I are known to represent the dominating processes responsible for ¹²⁹I in continental environmental samples that are remote from ¹²⁹I sources and not directly influenced by any liquid ¹²⁹I release of nuclear installations. Up to now, however, little is known about the major emitters and the related global deposition pattern of ¹²⁹I.In this work an overview over major sources of ¹²⁹I is given, and hitherto unknown time-dependent releases from these were estimated. Total gaseous ¹²⁹I releases from the US and former Soviet reprocessing facilities Hanford, Savannah River, Mayak, Seversk and Zheleznogorsk were found to have been 0.53, 0.27, 1.05, 0.23 and 0.14TBq, respectively. These facilities were thus identified as major airborne ¹²⁹I emitters.The global deposition pattern due to the ¹²⁹I released, depending on geographic latitude and longitude, and on time was studied using a box model describing the global atmospheric transport and deposition of ¹²⁹I. The model predictions are compared to ¹²⁹I concentrations measured by means of Accelerator Mass Spectrometry (AMS) in water samples that were collected from various lakes in Asia, Africa, America and New Zealand, and to published values.As a result, both pattern and temporal evolution of ¹²⁹I deposition values measured in and calculated for different types of environmental samples are, in general, in good agreement. This supports our estimate on atmospheric ¹²⁹I releases and the considered substantial transport and deposition mechanisms in our model calculations.