Transfer of 137Cs into Maize (Zea mays L.) at Different Growth Stages in the Area Contaminated by the Chernobyl Fallout
Related Experiment Video
Updated: Aug 28, 2026

Measuring Fluxes of Mineral Nutrients and Toxicants in Plants with Radioactive Tracers
Published on: August 22, 2014
Tatiana Paramonova1,2, Olga Denisova1,2, Natalia Kuzmenkova1,3
1Laboratory of Geochemistry of Natural Waters, Geography Faculty, Lomonosov Moscow State University, Moscow 119991, Russia.
Abstract:
Accumulation of radionuclides in crop products can pose public health risks. Parameters of 137Cs root uptake by maize were investigated at four growth stages, from leaf development to ripening (June-September), in the post-Chernobyl area of the Plavsk radioactive hotspot (the Tula region of Russia). It was established that the chernozem of the agrosystem still contains about 180 kBq 137Cs m-2. Seasonal trends of 137Cs activity concentrations in above- and belowground parts of maize differ appreciably. In aerial parts, the 137Cs accumulation rate increases as vegetative organs develop from June to July, then drops when generative organs appear in August. In the belowground biomass, the 137Cs content increases with the growth of fine roots, which serve as relative concentrators of the radionuclide. However, at all stages of growth, radionuclide transfer to maize occurs with low intensity. It does not directly depend on changes in biomass, dry matter content, or 40K content, and only slightly relates to the ash content. The transfer factor is estimated to be 6.2 × 10-3 for cob kernels (grain) and 3.8 × 10-2 for stems and leaves, which corresponds to the IAEA-recommended values and ensures acceptable levels of 137Cs accumulation in crop products produced in the territory.
