Thiocyanate Dual Wavelength Spectrophotometric Determination of Molybdenum in High Lead Ores
摘 要
在常规的硫氰酸盐光度法测定钼的硫酸介质中,加入80 g·L-1乙二胺四乙酸二钠盐(EDTA-2Na)溶液7 mL,使48 mg·L-1以下共存的铅(Ⅱ)无法生成硫酸铅,不干扰钼的测定,应用此条件测定了含铅量较高的矿石中钼的含量。样品(0.100 0~0.500 0 g)于高铝坩埚中,用过氧化钠3 g融熔,熔块用水浸出,定容至100 mL,分取部分试液,加入EDTA-2Na溶液7 mL后按常规条件显色,用双波长方法以460 nm(λ1)为测定波长,650 nm(λ2)为参比波长测量吸光度(A),计算ΔA(Aλ1-Aλ2)。钼的质量浓度在6.0 mg·L-1以内与相应的ΔA之间呈线性关系,方法的检出限(3s/k)为8.1×10-3mg·L-1。应用此方法测定了2个CRM(GBW 07238,GBW 07285)中的钼量,测定值与认定值相符,测定值的相对标准偏差(n=9)依次为2.8%,1.2%。
Abstract
In the H2SO4 medium of the conventional method of thiocyanate photometric determination of molybdenum, by addition of 7 mL of 80 g·L-1 EDTA-2Na solution, the interference of co-existing Pb2+ up to 48 mg·L-1 due to formation of PbSO4 was eliminated. This procedure was applied to SCN--photometric determination of molybdenum in ore samples with high lead contents. The ore sample (0.100 0-0.500 0 g) was fused with 3 g of Na2O2 in a high-aluminum crucible, the melt was taken up with water, and made up its volume to 100 mL. An aliquot of the sample solution was taken, and its molybdenum content was determined by the conventional SCN--photometric procedure after addition of 7 mL of the EDTA-2Na solution. Value of absorbance difference (ΔA=Aλ1-Aλ2) of colored solution was measured by dual-wavelength-spectrophotometry, using 460 nm (λ1) as the measuring wavelength and 650 nm (λ2) as the reference wavelength. Linear relationship between values of ΔA and respective mass concentrations of molybdenum was kept within 6.0 mg·L-1, with value of detection limit (3s/k) of 8.1×10-3mg·L-1. The proposed method was used to determine molybdenum in 2 ore CRMs (GBW 07238, GBW 07285), giving results in consistency with the certified values, and RSD′s (n=9) of the 2 CRMs found were 2.8%, 1.2% respectively.
中图分类号 O657.32 DOI 10.11973/lhjy-hx201610029
所属栏目 专题报道(矿产品及金属材料分析)
基金项目
收稿日期 2015/7/20
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备注王海军(1983-),男,陕西西安人,工程师,主要从事 岩石矿物化学分析工作。
引用该论文: WANG Hai-jun,WEI Zeng,CHENG Wen-kang,NING Xin-xia. Thiocyanate Dual Wavelength Spectrophotometric Determination of Molybdenum in High Lead Ores[J]. Physical Testing and Chemical Analysis part B:Chemical Analysis, 2016, 52(10): 1234~1236
王海军,魏增,程文康,宁新霞. 硫氰酸盐双波长分光光度法测定高铅矿石中钼量[J]. 理化检验-化学分册, 2016, 52(10): 1234~1236
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【3】王香婷,樊雪梅,王书民.亚甲基蓝-高碘酸钾催化动力学光度法测定钼尾矿中钼[J].冶金分析, 2015,35(6):57-60.
【4】樊雪梅,王书民,周美,等.抑制动力学分光光度法测定钼尾矿中痕量钼[J].分析试验室, 2012,31(11):94-96.
【5】张宁,刘海波,江泓,等.EDTA差减滴定法测定钼精矿中的钼[J].中国钼业, 2010,34(4):28-30.
【6】薛静.极谱法测定钼矿石中的总钼氧化钼硫化钼[J].岩矿测试, 2012,31(6):989-991.
【7】朱青青.火焰原子吸收光谱法测定土壤中钼[J].理化检验-化学分册, 2005,41(5):351-352.
【8】贺攀红,龚治湘.火焰原子吸收光谱法测定矿石中微量钼[J].理化检验-化学分册, 2012,48(3):360-361.
【9】唐本玲,胡晓燕,王海舟.柱前衍生-高效液相色谱法测定钢及合金中钨和钼[J].理化检验-化学分册, 2003,39(8):445-447.
【10】冯信平,田家金.ICP-MS法测定土壤中有效钼不确定度的研究[J].安徽农业科学, 2010,38(36):20698-20700.
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