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Characterization and identification of mixed-metal phosphates in soils: the application of Raman spectroscopy

机译:土壤中混合金属磷酸盐的表征与鉴定:拉曼光谱法的应用

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The development of protocols for the identification of metal phosphates in phosphate-treated, metal-contaminated soils is a necessary yet problematical step in the validation of remediation schemes involving immobilization of metals as phosphate phases. The potential for Raman spectroscopy to be applied to the identification of these phosphates in soils has yet to be fully explored. With this in mind, a range of synthetic mixed-metal hydroxylapatites has been characterized and added to soils at known concentrations for analysis using both bulk X-ray powder diffraction (XRD) and Raman spectroscopy. Mixed-metal hydroxylapatites in the binary series Ca-Cd, Ca-Pb, Ca-Sr and Cd-Pb synthesized in the presence of acetate and carbonate ions, were characterized using a range of analytical techniques including XRD, analytical scanning electron microscopy (SEM), infrared spectroscopy (IR), inductively coupled plasma-atomic emission spectrometry (ICP-AES) and Raman spectroscopy. Only the Ca-Cd series displays complete solid solution, although under the synthesis conditions of this study the Cd_5(PO_4)_3OH end member could not be synthesized as a pure phase. Within the Ca-Cd series the cell parameters, IR active modes and Raman active bands vary linearly as a function of Cd content. X-ray diffraction and extended X-ray absorption fine structure spectroscopy (EXAFS) suggest that the Cd is distributed across both the Ca(1) and Ca(2) sites, even at low Cd concentrations. In order to explore the likely detection limits for mixed-metal phosphates in soils for XRD and Raman spectroscopy, soils doped with mixed-metal hydroxylapatites at concentrations of 5, 1 and 0.5 wt. percent were then studied. X-ray diffraction could not confirm unambiguously the presence or identity of mixed-metal phosphates in soils at concentrations below 5 wt. percent. Raman spectroscopy proved a far more sensitive method for the identification of mixed-metal hydroxylapatites in soils, which could positively identify the presence of such phases in soils at all the dopant concentrations used in this study. Moreover, Raman spectroscopy could also provide an accurate assessment of the degree of chemical substitution in the hydroxylapatites even when present in soils at concentrations as low as 0.1 percent.
机译:在验证涉及将金属固定为磷酸盐相的修复方案的验证中,制定用于在磷酸盐处理过的,金属污染的土壤中鉴定金属磷酸盐的规程是必要的但有问题的步骤。拉曼光谱法用于鉴定土壤中这些磷酸盐的潜力尚未得到充分探索。考虑到这一点,已对一系列合成的混合金属羟基磷灰石进行了表征,并以已知的浓度将其添加到土壤中,以便使用体X射线粉末衍射(XRD)和拉曼光谱法进行分析。使用包括X射线衍射,分析扫描电子显微镜(SEM)在内的多种分析技术表征了在乙酸根和碳酸根离子存在下合成的Ca-Cd,Ca-Pb,Ca-Sr和Cd-Pb二元系列的混合金属羟基磷灰石),红外光谱(IR),电感耦合等离子体原子发射光谱(ICP-AES)和拉曼光谱。尽管在本研究的合成条件下,Cd_5(PO_4)_3OH端基不能作为纯相合成,但只有Ca-Cd系列显示出完全的固溶体。在Ca-Cd系列中,电池参数,IR活性模式和拉曼活性带随Cd含量线性变化。 X射线衍射和扩展的X射线吸收精细结构光谱(EXAFS)表明,即使在低Cd浓度下,Cd也会分布在Ca(1)和Ca(2)位置上。为了探索XRD和拉曼光谱法在土壤中混合金属磷酸盐的可能检出限,掺杂了5、1和0.5 wt。%混合金属羟基磷灰石的土壤。然后研究百分比。 X射线衍射无法明确地确认浓度低于5 wt。%的土壤中混合金属磷酸盐的存在或特性。百分。拉曼光谱法证明了一种用于鉴定土壤中混合金属羟基磷灰石的灵敏得多的方法,该方法可以肯定地鉴定本研究中使用的所有掺​​杂剂浓度下土壤中此类相的存在。此外,即使当土壤中磷灰石的浓度低至0.1%时,拉曼光谱法也可以准确评估羟基磷灰石中的化学取代度。

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