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Radium in New Zealand agricultural soils: Phosphate fertiliser inputs, soil activity concentrations and fractionation profiles

机译:新西兰农业土壤中的镭:磷肥输入量,土壤活性浓度和分馏曲线

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摘要

Phosphate ores can contain high levels of U-238 and its decay products. Of these decay products Ra-226 is an important environmental contaminant, while Ra-228 from Th-232 day may also be present, albeit at lower activity concentrations. Acid processing of phosphate ore to triple superphosphate elutes a large proportion of the Ra-226 from the final product. However, fertiliser production in New Zealand generally avoids acid processing and instead uses single superphosphate and reactive phosphate rock to maintain crop yields, meaning that Ra-226 is retained in the final product. As a first step towards characterising the human health impacts from fertiliser-borne radium, research was undertaken to identify loading and long-term accumulation of Ra-226 and Ra-228 in New Zealand agricultural soils, as well as the fractionation of Ra-226 into different soil phases.Activity concentrations for Ra-226 of up to 1.6 kBq/kg were determined in phosphate-containing fertilisers used in New Zealand. In contrast, Ra-228 did not exceed 75 Bq/kg. Analysis of 40 New Zealand soils, covering a range of agricultural uses, showed activities of between (27-88) Bq/kg Ra-226 and (21-102) Bq/kg Ra-228. Unexpectedly, there was also a strong correlation between the two radium isotopes. In 13 of the agricultural soils, all with very high available phosphate levels, the fractionation profile of Ra-226 was determined. These data indicated that Ra-226 largely remains immobile in the residual phase of the soil. Calcium and available phosphate were significantly correlated with binding of Ra-226 into labile and non-labile fractions. Barium is also hypothesised to play a significant role in co-precipitating Ra-226 into non-labile soil fractions. While a high percentages of Ra-226 immobile in the non-labile fraction would allow for marked accumulation over time it may limit the availability for uptake into crops and thus the ionising radiation dose for consumers.
机译:磷酸盐矿石可能含有高含量的U-238及其衰变产物。在这些衰变产物中,Ra-226是重要的环境污染物,而Th-232天的Ra-228也可能存在,尽管其活性浓度较低。将磷酸盐矿石进行酸处理成三重过磷酸盐会从最终产品中洗脱出很大一部分Ra-226。但是,新西兰的化肥生产通常避免酸处理,而是使用单一的过磷酸钙和反应性磷酸盐岩来维持作物产量,这意味着Ra-226保留在最终产品中。作为表征肥料中镭对人类健康的影响的第一步,进行了研究以鉴定新西兰农业土壤中Ra-226和Ra-228的负载量和长期积累以及Ra-226的分离在新西兰使用的含磷酸盐的肥料中测定的Ra-226的活性浓度高达1.6 kBq / kg。相反,Ra-228不超过75 Bq / kg。对涵盖一系列农业用途的40种新西兰土壤进行的分析显示,其活性介于(27-88)Bq / kg Ra-226和(21-102)Bq / kg Ra-228之间。出乎意料的是,两种镭同位素之间也存在很强的相关性。在全部可用磷酸盐含量很高的13种农业土壤中,确定了Ra-226的分馏曲线。这些数据表明,Ra-226在土壤残留相中基本上保持不动。钙和可利用的磷酸盐与Ra-226结合到不稳定和非不稳定级分中具有显着相关性。还假设钡在将Ra-226共沉淀为不稳定土壤组分中起重要作用。虽然在不稳定的部分中高比例的Ra-226固定不动会随着时间的推移显着积累,但它可能会限制作物吸收作物的能力,从而限制消费者的电离辐射剂量。

著录项

  • 来源
    《Journal of Environmental Radioactivity》 |2019年第9期|119-126|共8页
  • 作者单位

    Minist Primary Ind, POB 2536, Wellington 6011, New Zealand|Univ Canterbury, Private Bag 4800, Christchurch 8140, New Zealand;

    Univ Canterbury, Private Bag 4800, Christchurch 8140, New Zealand;

    Inst Environm Sci & Res Ltd, POB 29-181, Christchurch 8540, New Zealand;

    Athabasca Univ, Fac Sci & Technol, Athabasca, AB, Canada|Athabasca Univ, Athabasca River Basin Res Inst, Athabasca, AB, Canada|Univ Alberta, Dept Biol Sci, Edmonton, AB, Canada;

    Massey Univ, Private Bag 11 222, Palmerston North 4442, New Zealand;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Superphosphate; Barite; Soil fractionation; Fertiliser contaminant;

    机译:过磷酸钙重晶石土壤分馏肥料污染物;
  • 入库时间 2022-08-18 04:24:00

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