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Nitrite-Induced Activation of lodate into Molecular Iodine in Frozen Solution

机译:亚硝酸盐诱导的冷冻溶液中Loates活化为分子碘

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摘要

A new mechanism for the abiotic production of molecular iodine (I-2) from iodate (IO3-), which is the most abundant iodine species, in dark conditions was identified and investigated. The production of I-2 in aqueous solution containing IO3- and nitrite (NO2-) at 25 degrees C was negligible. However, the redox chemical reaction between IO3- and NO2- rapidly proceeded in frozen solution at -20 degrees C, which resulted in the production of I-2, I-, and NO3-. The rapid redox chemical reaction between IO3- and NO2- in frozen solution is ascribed to the accumulation of IO3-, NO2-, and protons in the liquid regions between ice crystals during freezing (freeze concentration effect). This freeze concentration effect was verified by confocal Raman microscopy for the solute concentration and UV-visible absorption spectroscopy with cresol red (acid-base indicator) for the proton concentration. The freezing-induced production of I-2 in the presence of IO3- and NO2- was observed under various conditions, which suggests this abiotic process for I-2 production is not restricted to a specific region and occurs in many cold regions. NO2--induced activation of IO3- to I-2 in frozen solution may help explain why the measured values of iodine are larger than the modeled values in some polar areas.
机译:鉴定并研究了在黑暗条件下由碘酸盐(IO3-)非生物生产分子碘(I-2)的新机理,碘酸盐是最丰富的碘物种。在25摄氏度下,含IO3-和亚硝酸盐(NO2-)的水溶液中I-2的产生可以忽略不计。但是,IO3-和NO2-之间的氧化还原化学反应在-20℃的冷冻溶液中迅速进行,这导致生成I-2,I-和NO3-。冷冻溶液中IO3-和NO2-之间的快速氧化还原化学反应归因于IO3,NO2-和质子在冷冻期间在冰晶之间的液体区域中的积累(冻结浓缩效应)。通过共焦拉曼显微镜对溶质浓度进行了验证,并使用了甲酚红(酸碱指示剂)对质子进行了紫外可见吸收光谱,验证了这种冻结浓缩效果。在各种条件下观察到在IO3-和NO2-存在下冷冻诱导的I-2产生,这表明这种I-2生产的非生物过程不限于特定区域,并且发生在许多寒冷地区。 NO2诱导的冷冻溶液中IO3-向I-2的活化可能有助于解释为什么在某些极地地区,碘的测量值大于模型值。

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  • 来源
    《Environmental Science & Technology》 |2019年第9期|4892-4900|共9页
  • 作者单位

    Korea Polar Res Inst KOPRI, Incheon 21990, South Korea|UST, Dept Polar Sci, Incheon 21990, South Korea;

    Hallym Univ, Dept Environm Sci & Biotechnol, Chunchon 24252, Gangwon Do, South Korea;

    Korea Polar Res Inst KOPRI, Incheon 21990, South Korea|UST, Dept Polar Sci, Incheon 21990, South Korea;

    Korea Polar Res Inst KOPRI, Incheon 21990, South Korea|UST, Dept Polar Sci, Incheon 21990, South Korea;

    Masaryk Univ, Fac Sci, Dept Chem, Kamenice 5, Brno 62500, Czech Republic|Masaryk Univ, Fac Sci, Res Ctr Tox Cpds Environm RECETOX, Kamenice 5, Brno 62500, Czech Republic;

    Masaryk Univ, Fac Sci, Dept Chem, Kamenice 5, Brno 62500, Czech Republic|Masaryk Univ, Fac Sci, Res Ctr Tox Cpds Environm RECETOX, Kamenice 5, Brno 62500, Czech Republic;

    CSIC, Inst Phys Chem Rocasolano, Dept Atmospher Chem & Climate, Madrid 28006, Spain;

    Pohang Univ Sci & Technol POSTECH, Div Environm Sci & Engn, Pohang 37673, South Korea;

    Hallym Univ, Dept Environm Sci & Biotechnol, Chunchon 24252, Gangwon Do, South Korea;

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