Twining J R, Zaw M, Russell R, Wilde K
Radionuclide Environmental Pathways Project, Australian Nuclear Science and Technology Organisation, PMB 1, Menai, New South Wales 2234, Australia.
J Environ Radioact. 2004;76(1-2):265-72. doi: 10.1016/j.jenvrad.2004.03.031.
Very little is known of the factors controlling soil-to-plant transfer of radionuclides in tropical environments. As part of an IAEA/FAO coordinated research project (CRP) designed to elucidate some of those factors, near-surface samples of two agricultural red-earth soils (Blain and Tippera) were collected from a study site in the Northern Territory. The climate is tropical monsoonal with crops being grown over the wet season from December to March/April. It is important to understand soil variables that may be related to this dramatic seasonality. In this investigation, soil redox state and microbial populations were assessed before and after the growing season with a view to generating hypotheses for future evaluation. The X-ray absorption near edge structure (XANES) technique was used to determine overall changes in the solid-state redox speciation of Fe and Mn in soils across the growing period. Fe speciation did not change but approximately 10% of the total Mn was oxidised from Mn(II) to Mn(III) and Mn(IV) in both soils between October 1999 and April 2000. An apparent disconnect between Fe and Mn was not unexpected given the >10 times higher concentration of Fe in the soils compared with Mn. These results have implications for the bioavailability of redox sensitive radionuclides such as Tc and Pu. Similarly, microbial population estimates were derived before and after the growing period. Total bacterial populations did not vary from 10(6) to 10(7) colonies per gram. Fungal populations increased over the growing season from 3-6 x 10(5) to 1-4 x 10(6) colonies per gram of soil. Fungi have the potential to decrease soil pH and hence increase the bioavailability of radionuclides such as Cs. In addition, fungi act to facilitate plant nutrition. This could lead to enhanced accumulation of nutrient analogues (e.g. Sr and Ra for Ca; Tc for Mn), but this effect may be masked by improved biomass production.
对于热带环境中控制放射性核素从土壤向植物转移的因素,人们了解甚少。作为国际原子能机构/联合国粮食及农业组织协调研究项目(CRP)的一部分,该项目旨在阐明其中一些因素,从北领地的一个研究地点采集了两种农业红壤(布莱因土和蒂佩拉土)的近地表样本。当地气候为热带季风气候,作物在12月至3月/4月的雨季种植。了解可能与这种显著季节性相关的土壤变量非常重要。在这项调查中,在生长季节前后评估了土壤氧化还原状态和微生物种群,以便为未来的评估提出假设。利用X射线吸收近边结构(XANES)技术测定了整个生长期间土壤中Fe和Mn的固态氧化还原形态的总体变化。Fe的形态没有变化,但在1999年10月至2000年4月期间,两种土壤中约10%的总Mn从Mn(II)氧化为Mn(III)和Mn(IV)。考虑到土壤中Fe的浓度比Mn高10倍以上,Fe和Mn之间明显的不相关性并不意外。这些结果对氧化还原敏感的放射性核素如Tc和Pu的生物有效性有影响。同样,在生长季节前后对微生物种群进行了估计。每克土壤中的细菌总数在10⁶至10⁷个菌落之间没有变化。真菌种群在生长季节从每克土壤3 - 6×10⁵个菌落增加到1 - 4×10⁶个菌落。真菌有可能降低土壤pH值,从而增加Cs等放射性核素的生物有效性。此外,真菌有助于促进植物营养。这可能导致营养类似物(如Ca的Sr和Ra;Mn的Tc)的积累增加,但这种影响可能会被生物量产量的提高所掩盖。