四酸体系微波消解-电感耦合等离子体质谱法测定土壤中的稀土和钡钍铅等35种元素

Determination of 35 Elements includings REEs, Ba, Th and Pb in Soil by Inductively Coupled Plasma-Mass Spectrometry with Four-Acid Ultrawave Digestion

  • 摘要: 土壤元素分析对地质调查、资源勘探等领域具有重要意义,但金属及稀土元素(REEs)的多元素单流程同步消解和分析常面临难溶元素(如REEs、Ba、Th等)消解不完全和复杂基质质谱干扰等问题。传统压力封闭酸溶法虽对Li、Be、Ti等元素回收效果较好,但对REEs等难溶元素的回收率偏低(多数<90%),难以满足一般元素与难溶元素同步分析需求。本文通过对比4 mL逆王水与不同用量氢氟酸、高氯酸组成的15个酸消解体系和2种赶酸条件对国家土壤标准物质37种元素的消解效果,建立了微波消解-四酸体系结合ICP-MS/MS的土壤多元素同步分析方法,确定了最优条件为3 mL硝酸+1 mL盐酸+2 mL氢氟酸+0.8 mL高氯酸的消解体系,与多次补加硝酸强化赶酸,可有效破坏硅酸盐矿物结构,促进难溶氧化物溶解,并通过多次补酸与高温驱除残留氢氟酸,避免生成难溶氟化物沉淀。经GBW07565等8种国家土壤标准物质及典型农作物(西藏青稞、新疆西红柿、江西水稻)根系土验证,本方法可准确测定除Cd、Cr外的35种目标元素,方法检出限为0.0005~3.410mg/kg,所有样品相对标准偏差(RSD)为0.25%~14.1%,实际土壤样品的加标回收率为81.6%~107.4%,显示出良好的稳定性和适用性。与传统压力封闭酸溶法相比,本方法显著提高了REEs、Ba、Th等难溶元素的回收率(多数>90%),为不同基质土壤多元素高效分析提供了可靠的解决方案。

     

    Abstract: The analysis of soil elements is of great significance to geological survey, resource exploration and other fields. However, the simultaneous digestion and analysis of multi-element single-process of metals and rare earth elements (REEs) often face the problems of incomplete digestion of insoluble elements (such as REEs, Ba, Th, etc.) and interference of complex matrix mass spectrometry. Although the traditional pressurized acid digestion method shows good recovery for elements like Li, Be, and Ti, the recovery rate of insoluble elements such as REEs is low (most < 90%), which makes it difficult to meet the needs of simultaneous analysis of general elements and insoluble elements. In this paper, by comparing the digestion effects of 15 acid digestion systems composed of 4 mL of inverse aqua regia, different amounts of hydrofluoric acid and perchloric acid and two kinds of acid removal conditions on 37 elements of national soil standard materials, the ultrawave digestion-four acid system combined with ICP-MS/MS was established. The optimal conditions were determined as follows: 3 mL nitric acid + 1 mL hydrochloric acid + 2 mL hydrofluoric acid + 0.8 mL perchloric acid digestion system and multiple additions of nitric acid to strengthen the acid removal combination. This method effectively destroys silicate mineral structures, promotes the dissolution of refractory oxides, and through repeated acid addition and high-temperature acid driving, removes residual hydrofluoric acid, avoiding the formation of insoluble fluoride precipitates. The method was systematically verified using 8 national soil standard materials (including GBW07565, etc.) and root soil of typical crops (Xizang highland barley, Xinjiang tomato, Jiangxi rice). The results show that this method can accurately determine 35 target elements except Cd and Cr, with a method detection limit of 0.0005–3.410 mg/kg. The relative standard deviation (RSD) of all samples was 0.2%–14.1% and the recovery of actual samples was 81.6%–107.4%. The results show that the method has good stability and applicability. Compared with the traditional pressurized closed acid dissolution method, this method significantly improves the recovery rate of REEs, Ba, Th and other elements (mostly>90%), and provides an efficient and reliable solution for multi-element analysis of different matrix soils.

     

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