Marin B, Chopin E I B, Jupinet B, Gauthier D
GEGENA(2) EA 3795, University of Reims Champagne-Ardenne, 2 esplanade Roland Garros, 51100 Reims, France.
Talanta. 2008 Oct 19;77(1):282-8. doi: 10.1016/j.talanta.2008.06.023. Epub 2008 Jun 27.
The aim of the study was to determine total trace (Cd, Co, Cr, Cu, Mn, Pb and Zn) and major (Al and Fe) element concentrations in calcareous soils using microwave-assisted digestion procedures. The literature showing lack of consensus regarding digestion procedures and unsatisfying recoveries for calcareous materials, four procedures using various acid combinations (HCl, HNO(3), H(2)O(2), HF) and volumes were tested using a certified reference material (CRM 141R) and natural calcareous soil samples. Digests were analysed by inductively coupled plasma-atomic emission spectrometry (ICP-AES). Repeatability (R.S.D. <5%) and recoveries (82-116%) showed that the procedures were precise and accurate for most elements. Five calcareous soil samples from a Champagne vineyard plot were, then, subjected to these procedures. In calcareous materials, the presence of HF resulted in Al being severely underestimated (recovery <5%) and Co overestimated (recovery >124%) due to complex formation or spectrochemical interferences, respectively. As digestion was not significantly influenced by the addition of H(2)O(2), the procedure corresponding to Aqua regia (HCl-HNO(3)) appeared as the best compromise and was selected for further multielemental environmental studies on calcareous materials, even if the absence of HF could lead to incomplete digestion of accessory silicate minerals. Results for a vineyard plot showed that the soils were contaminated (3.65 mg kg(-1) Cd, 67 mg kg(-1) Cr, 278 mg kg(-1) Cu, 143 mg kg(-1) Pb and 400 mg kg(-1) Zn) as a consequence of urban waste and copper-treatment applications.
本研究的目的是使用微波辅助消解程序测定石灰性土壤中的总痕量元素(镉、钴、铬、铜、锰、铅和锌)和主要元素(铝和铁)浓度。鉴于文献表明对于消解程序缺乏共识,且石灰性材料的回收率不尽人意,因此使用了经认证的参考物质(CRM 141R)和天然石灰性土壤样品,对四种使用不同酸组合(盐酸、硝酸、过氧化氢、氢氟酸)和体积的程序进行了测试。消解液通过电感耦合等离子体原子发射光谱法(ICP - AES)进行分析。重复性(相对标准偏差<5%)和回收率(82 - 116%)表明,这些程序对于大多数元素而言是精确且准确的。随后,对来自香槟葡萄园地块的五个石灰性土壤样品进行了这些程序的测试。在石灰性材料中,由于形成络合物或光谱化学干扰,氢氟酸的存在分别导致铝被严重低估(回收率<5%)和钴被高估(回收率>124%)。由于添加过氧化氢对消解没有显著影响,对应王水(盐酸 - 硝酸)的程序似乎是最佳折衷方案,并被选用于对石灰性材料进行进一步的多元素环境研究,即便缺少氢氟酸可能导致副硅酸盐矿物的消解不完全。一个葡萄园地块的结果表明,由于城市垃圾和铜处理应用,土壤受到了污染(镉含量为3.65毫克/千克,铬含量为67毫克/千克,铜含量为278毫克/千克,铅含量为143毫克/千克,锌含量为400毫克/千克)。