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碘(V)-碘化物-吖啶橙缔合体系褪色光度法测定磷矿中碘 被引量:3

Fading spectrophotometric determination of iodine in phosphate rock with Ⅰ(V)-iodide-acridine orange complex system
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摘要 在0.048mol/L H3PO4中,碘(V)与过量的I^-反应生成I3^-,加入NaAc后,I3^-再与吖啶橙(AO)生成1:1的离子缔合物.使AO发生褪色反应,据此建立了褪色光度法测定碘的新方法。可见光区最大褪色波长为491nm.碘(V)质量浓度在0-0.48μg/mL范围内服从比尔定律,表观摩尔吸光系数ε为1.72×10^5L/mol·cm,检出限为7.47μg/L。MnO4^-等氧化性离子的干扰可加入盐酸羟胺消除.Ca^2+和Fe^2+等金属离子的干扰经阳离子交换树脂预分离去除。方法用于测定磷矿中碘,结果与国标法一致,相对标准偏差小于1.32%(n=5).加标回收率为100.3%~101.0%。 A new fading spectrophotometric method for determination of trace iodine was developed. I(V) reacts with excess I - in 0. 048 mol/L H3PO4 to produce I3^-. After adding NaAc, I3^-, further reacts with acridine orange (AO) to form an ionassociation complex ( 1 : 1 ), leading to the fading of AO. Beer' s law for 0 - 0.48/μg/mL I(V) with the maximum fading wavelength locating at 491 nm in the visible region. The apparent molar absorption coefficient (ε) was 1.72 ×10^5 L·mol^-1 ·cm^-1 and the detection limit was 7.47 μg/L. The interferences of oxidants including MnO4^- were eliminated by adding hydrazine hydrochloride. The interferences of metal ions such as, Ca^2+ and Fe^2+ were separated by cation exchange resin. The method was applied to determine iodine in phosphate ore samples. The results well agreed with those obtained using national standard method. RSDs of 5 determinations for iodine were less than 1.32 %, and recoveries after I(V) standard solution addition varied from 100.3 % to 101.0 %.
出处 《化工矿物与加工》 CAS 北大核心 2009年第6期15-18,共4页 Industrial Minerals & Processing
基金 国家自然科学基金项目(20603018) 连云港市科技项目(SH0816 CN0646)资助
关键词 褪色光度法 碘化物 吖啶橙 离子缔合物 fading spectrophotometry iodine iodide acridine orange (AO) ion-association complex
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