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olivesandorange

Move factors (TF) of 134Cs to olive and citrus trees made on two unique, actually hanging out there for a 3-year nursery separate. Two-year-old trees were moved with their whole rootball into huge pots containing the ruined soil (110 kg pot-1).


The dirt was moved to each pot in layers on the most raised sign of which 134Cs as CsCl was streamed (18.5 MBq pot-1). For both evergreen trees, soil type basically affected radiocaesium move. 134Cs focus was lower for the calcareous-significant soil than for the horrendous light soil.


Move parts of orange trees were higher than those of olive trees in the damaging light soil.


However a huge load of 134Cs was surveyed in olives made on the disastrous light soil, no 134Cs was perceived in the normal olive oil when an oil part (5% f.w.) was taken out.





Clashing with the standard the eatable piece of the oranges showed the most raised 134Cs centralization of all plant parts.


The relationship between 134Cs take-up and potassium content in the different plant compartments was comparably centered around when picked trees were sliced down.


The potassium fixation in the plants was not commonly fascinating between the trees filling in the two kinds of soil notwithstanding the enormous contrasts during the 134Cs take-up in the two soils.


TF values and potassium content in the different plant compartments of each tree were remarkably related.


For the two yields move factors as well as potassium content were the most brought up in the making plant parts (new leaves and branches, blossoms). The exchange elements of 134Cs for the zeroed in on trees are in practically identical immense degree as the likely gains of yearly yields made under commensurate circumstances.

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