This is a preliminary study of the depth distribution of (137)Cs radionuclides in cultivated anthrosol soil of a 15-year old peach tree plantation at the experimental field "Radmilovac" near Belgrade. Before planting, the soil was ploughed at the depth of 1 m. The soil had not been annually ploughed, irrigated and treated with mineral fertilizers for three years before sampling. Activity concentration for (137)Cs ranged from 1.8 Bq kg(-1) to 35 Bq kg(-1). Along the soil depth it varied highly, reaching as high a total variation coefficient as 83 %. Radiocaesium distribution patterns depended on the extent of soil mixing in the plough layer, as it was mechanically transferred from the surface to the lower soil layers during cultivation. (137)Cs was associated with humus content and fixation to clay fractions in the soil. Our results single out soil's hygroscopic water as a valuable parameter for (137)Cs behaviour that could be used commonly if the measurement is standardised.

译文

这是对贝尔格莱德附近 “Radmilovac” 实验场的15年桃树人工林栽培的anthrosol土壤中 (137)Cs放射性核素深度分布的初步研究。在种植之前,将土壤犁入1 m的深度。在采样之前,三年没有每年对土壤进行耕作,灌溉和用矿物肥料处理。(137)Cs的活性浓度范围为1.8 bqkg (-1) 至35bqkg (-1)。沿土壤深度变化很大,总变异系数达到83%。放射性铯的分布模式取决于耕层中土壤混合的程度,因为在耕作过程中将其从地表机械转移到较低的土壤层。(137)Cs与土壤中的腐殖质含量和对粘土组分的固定有关。我们的结果将土壤的吸湿水作为 (137)Cs行为的有价值的参数,如果对测量进行标准化,则通常可以使用。

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