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Effect of biotite, zeolite, heavy clay, bentonite and apatite on the uptake of radiocesium by grass from peat soil

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Abstract

Biotite is a potassium rich mineral, which is used as a fertilizer in organic farming and as a soil amendment in conventional farming. Its ability to reduce 134Cs uptake by ryegrass from peat soil was studied in pot experiments and compared with zeolite, heavy clay, bentonite and apatite. In addition, the long-term effect of biotite on 137Cs uptake from peat soil was studied in the peat field.

In the pot experiments in the first cut of ryegrass, the minerals decreased 134Cs uptake by plants in the following order: zeolite > heavy clay > bentonite > biotite > apatite. Apatite did not have any effect on the plant 134Cs level. In the later cuts, the uptake of 134Cs from biotite-treated soil decreased further while that from soils treated with other minerals remained unchanged or even increased. In general, 134Cs uptake by plants decreased with increasing mineral level. The decrease of 134Cs uptake became more efficient, especially at the early growth stage, by mixing small amounts of zeolite in biotite. The results of the field experiment indicated the long-term effect of biotite on reducing 134Cs uptake by plants. Biotite application rate was 30 t ha-1. The five-year mean of the plant/soil concentration ratio of 137Cs was 0.05 for biotite-treated soil, in contrast to 0.14 for the control soil. On the whole, biotite reduced considerably the 137Cs level of plants on peat soil and this effect was long-lasting. For an effective reduction of plant radiocesium a great quantity of biotite is needed and therefore it is most suitable for greenhouse cultivation where contaminated slightly decomposed peat is used as a growing medium.

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  1. Resource Management Research, Agricultural Research Centre of Finland, FIN-31600, Jokioinen, FinlandFAX No

    A. Paasikallio

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Paasikallio, A. Effect of biotite, zeolite, heavy clay, bentonite and apatite on the uptake of radiocesium by grass from peat soil. Plant Soil 206, 213–222 (1999). https://doi.org/10.1023/A:1004412512557

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