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Removal of U(VI) from aqueous solutions by the nano-iron oxyhydroxides

机译:纳米羟基氧化铁从水溶液中去除U(VI)

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The nano-iron oxyhydroxides (α- and γ-FeOOH) were synthesized by oxidation of the various raw materials (FeSO _4 and FeCl _2) as iron precursors under alkaline conditions. Morphologies of nano-iron oxyhydroxides were characterized by high resolution transmission electron microscope (HRTEM), X-ray powder diffraction (XRD) and specific surface area (SSA), respectively. The removal of U(VI) from aqueous solution by nano-iron oxyhydroxides was also investigated as a function of contact time, U(VI) concentration, pH, ionic strength and temperature under ambient conditions. The occurrence of needle-like shape of nano-goethite and rod-like shape of nano-lepidocrocite were attributed to oxidization of Fe ~(2+) under different conditions in terms of XRD analysis and HRTEM images. The sorption results indicated that the removal of U(VI) strongly depended on pH and were independent of ionic strength. Langmuir model was employed to model the sorption isotherms of U(VI) at three various temperatures of 293, 313 and 333 K. The thermodynamic parameters (ΔH°, ΔS° and ΔG°) computed from the temperature showed that sorption process of U(VI) on nanoiron oxyhydroxides was endothermic and spontaneous. The mechanism of U(VI) sorption on nano-iron oxyhydroxides was assumed to outer-sphere surface complexation at low pH (pH < 5.0) and at low ionic strength conditions (IS = 0.01 M NaClO _4), whereas the uptake of U(VI) was dominated by surface precipitation at high pH conditions. Thereby nano-iron oxyhydroxides can be used as an efficient backfill materials for the in situ disposal of U(VI)-bearing contaminated groundwater.
机译:通过在碱性条件下氧化各种原料(FeSO _4和FeCl _2)作为铁前体,合成了纳米羟基氧化铁(α-和γ-FeOOH)。分别通过高分辨率透射电子显微镜(HRTEM),X射线粉末衍射(XRD)和比表面积(SSA)表征了羟基氧化铁的形态。还研究了在环境条件下,纳米羟基氧化铁从水溶液中去除U(VI)与接触时间,U(VI)浓度,pH,离子强度和温度的关系。 XRD分析和HRTEM图像分析表明,针状纳米针铁矿和棒状针铁云母的出现是由于Fe〜(2+)在不同条件下的氧化所致。吸附结果表明,U(VI)的去除强烈依赖于pH值,并且与离子强度无关。用Langmuir模型对U(VI)在293、313和333 K的三个不同温度下的吸附等温线进行建模。由温度计算出的热力学参数(ΔH°,ΔS°和ΔG°)表明,U(VI)的吸附过程VI)在羟基氧化铁上是吸热的和自发的。假定U(VI)吸附在羟基氧化铁上的机理是在低pH(pH <5.0)和低离子强度条件下(IS = 0.01 M NaClO _4)外球表面络合,而U(VI)的吸收VI)主要是在高pH条件下发生表面沉淀。因此,纳米羟基氧化铁可用作有效地回填材料,用于原位处理含U(VI)的受污染地下水。

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