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Effect of Ashing Temperature on Accurate Determination of Plutonium in Soil Samples

机译:灰化温度对土壤样品中Determination准确测定的影响

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An acidic leaching method using HNO3 is widely employed to release the global fallout Pu from soil samples for further chemical separations in radioecology and toxicology studies and in many applications using Pu as a useful tracer. In the methods sample ash treatment step to decompose organic matter in soil, various ashing temperatures (400-900 degrees C) are used; however, the effect of ashing temperature on the accurate Pu analysis has not been well investigated. In this study, two standard reference soils (IAEA-soil-6 and IAEA-375) were used to determine the ashing temperature effect (from 375 to 600 degrees C) on the HNO3 leaching method. The Pu analytical results of both standard reference materials showed that lower Pu239+240 activity was observed when the ashing temperature exceeded 450 degrees C, and the 239+240Pu activity continued to decrease as the ashing temperature was raised. Approximately 40% of the Pu content could not be leached out by concentrated HNO3 after ashing for 4 h at 600 degrees C. The Pu loss was attributed to the formation of refractory materials, which are insoluble in HNO3 solution. This hypothesis was confirmed by the XRD analysis of soil samples, which revealed that plagioclase-like silicate materials were formed after high-temperature ashing. To ensure Pu release efficiency in HNO3 leaching, we recommend 450 degrees C as the ideal ashing temperature. This recommendation is also useful for analysis of other important artificial radionuclides (e.g., Cs-137, Sr-90, Am-241) for which an ashing process is needed to decompose the organic content in soil samples.
机译:广泛使用一种使用HNO3的酸性浸出方法从土壤样品中释放出全球沉降的Pu,以便在放射生态学和毒理学研究以及许多使用Pu作为有用示踪剂的应用中进行进一步的化学分离。在样品灰分处理步骤中分解土壤中的有机物的方法中,使用了各种灰化温度(400-900摄氏度)。但是,灰化温度对准确的Pu分析的影响尚未得到很好的研究。在这项研究中,使用两种标准参考土壤(IAEA-soil-6和IAEA-375)来确定HNO3浸出方法的灰化温度效应(从375到600摄氏度)。两种标准参考材料的Pu分析结果均显示,当灰化温度超过450摄氏度时,Pu239 + 240的活性较低,并且随着灰化温度的升高,239 + 240Pu活性持续降低。在600℃下灰化4 h后,浓的HNO3不能浸出约40%的Pu。Pu的损失归因于难熔材料的形成,难熔材料不溶于HNO3溶液。通过土壤样品的XRD分析证实了这一假设,该发现表明高温灰化后形成了斜长石状硅酸盐材料。为了确保HNO3浸出过程中Pu的释放效率,我们建议将450摄氏度作为理想的灰化温度。该建议对于分析其他重要的人工放射性核素(例如Cs-137,Sr-90,Am-241)也很有用,需要对其进行灰化处理以分解土壤样品中的有机物。

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