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Low-sulphate water sample preparation for LSC detection of ~(35)S avoiding sulphate precipitation

机译:低硫酸盐水样品制备,用于〜(35)S的LSC检测,避免硫酸盐沉淀

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Information about groundwater residence times is essential for evaluating appropriate groundwater abstraction rates and aquifer vulnerabilities and hence for sustainable groundwater management in general. Naturally occurring radionuclides are suitable tools for related investigations. While the applicability of several long-lived radionuclides for the investigation of long-term processes has been demonstrated frequently, residence times of less than one year are only scarcely discussed in the literature. That is due to the rather small number of applicable radionuclides that show adequately short half-lives. A promising approach for investigating sub-yearly residence times applies radioactive sulphur. S-35 is continuously produced in the upper atmosphere from where it is transferred with the rain to the groundwater. As soon as the water enters the subsurface its S-35 activity concentration decreases with an 87.4 day half-life. This makes S-35 suitable for investigating sub-yearly groundwater residence times. However, the low S-35 activities in natural waters require sulphate preconcentration for S-35 detection by means of liquid scintillation counting (LSC). That is usually done by sulphate extraction from large water samples with an anion-exchange resin (Amberlite IRA400, Cl-form), elution from the resin with NaCl, and precipitation as BaSO4. Our study aimed at optimizing the standard sample preparation procedure by avoiding the laborious precipitation step. We suggest (i) sulphate extraction using the exchange resin Amberlite IRA67 (OH-form), (ii) elution with ammonium hydroxide, (iii) evaporation of the eluate and (iv) dissolving the resulting dry precipitate in 2 ml H2O. In contrast to the standard approach our method results in a final sample solution of low ionic strength, which allows applying the water miscible scintillation cocktail Hionic-Fluor. Since Hionic-Fluor accepts only aqueous solutions of low ionic strength the approach is applicable for waters with high S-35/(SO42-)-S-32 ratios, i.e., low total sulphate sample loads (e.g. rainwater).
机译:有关地下水停留时间的信息对于评估适当的地下水抽取率和含水层脆弱性,以及总体而言对可持续的地下水管理至关重要。天然存在的放射性核素是进行相关研究的合适工具。尽管已经频繁地证明了几种长寿命放射性核素在长期过程研究中的适用性,但文献中很少讨论不到一年的停留时间。那是由于显示出足够短的半衰期的适用放射性核素的数量很少。研究亚年停留时间的一种有前途的方法是使用放射性硫。 S-35在高层大气中连续产生,并随雨水从那里转移到地下水中。一旦水进入地下,其S-35活性浓度就会降低,半衰期为87.4天。这使得S-35适用于调查次年地下水停留时间。但是,天然水中低的S-35活性需要通过液体闪烁计数(LSC)对S-35进行硫酸盐预浓缩。通常通过用阴离子交换树脂(Amberlite IRA400,Cl型)从大型水样中硫酸盐萃取,用NaCl洗脱树脂并以BaSO4沉淀的方式完成。我们的研究旨在通过避免费力的沉淀步骤来优化标准样品制备程序。我们建议(i)使用交换树脂Amberlite IRA67(OH-form)进行硫酸盐萃取,(ii)用氢氧化铵洗脱,(iii)洗脱液蒸发,以及(iv)将所得的干燥沉淀溶于2 ml H2O。与标准方法相反,我们的方法产生的最终样品溶液的离子强度较低,因此可以使用与水混溶的闪烁混合物Hionic-Fluor。由于Hionic-Fluor仅接受低离子强度的水溶液,因此该方法适用于S-35 /(SO42-)-S-32比高的水,即总硫酸盐样品负荷低(例如雨水)。

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