Adsorption/Desorption Characteristics of Metal Ions on Ferric Oxyhydroxide During a Freeze–Thaw Cycle

IF 2.9 3区 化学 Q2 CHEMISTRY, MULTIDISCIPLINARY ACS Earth and Space Chemistry Pub Date : 2024-01-16 DOI:10.1021/acsearthspacechem.3c00270
Yoshiki Fukuda, Makoto Harada and Tetsuo Okada*, 
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Abstract

Iron is a key element that affects bioactivity in the global environment as a nutrient and also as an adsorbent that controls the circulation of other elements in the hydrosphere. This element is abundant in sea ice and is released into the aquatic environment during the thawing process. Due to the low solubility of iron compounds, they exist as solid materials, such as oxides and oxyhydroxides, which effectively adsorb transition metal ions and affect their circulation in the hydrosphere. This process occurs not only in the hydrosphere but also in the cryosphere. In this study, adsorption of first-row transition metal cations on ferric oxyhydroxide (FeOxH) under frozen conditions is evaluated by ex-situ measurements with sample thawing and also by in situ X-ray fluorescence (XRF) measurements without thawing. The adsorption and desorption characteristics of transition metal cations on FeOxH are discussed from the difference in the adsorption ratio between these two measurements. For in situ XRF measurements, linear regression analysis assuming two states of analytes, i.e., adsorbed on FeOxH and dissolved in the freeze-concentrated solution (FCS) is efficient in estimating adsorption ratios. While complete adsorption is found for all metal cations studied here (Mn2+, Co2+, Ni2+, Cu2+, and Zn2+) at pH > 8, the adsorption ratio determined by in situ XRF is larger than the corresponding value obtained with the ex situ method with thawing at lower pH. This strongly suggests that metal cations are well adsorbed on FeOxH when concentrated in the FCS under frozen conditions but are desorbed upon thawing. The comparison of the adsorption ratios obtained by in situ and ex situ methods reveals specific adsorption of Mn2+ and Co2+. Interestingly, the specific adsorption of Mn2+ is irreversible, and desorption does not occur upon thawing. In contrast, thawing causes the desorption of specifically adsorbed Co2+, suggesting that different mechanisms are responsible for the specific adsorption.

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金属离子在冻融循环期间在氧氢氧化铁上的吸附/解吸特性
铁是影响全球环境中生物活性的关键元素,它既是一种营养物质,也是一种吸附剂,控制着水圈中其他元素的循环。这种元素在海冰中含量丰富,并在解冻过程中释放到水生环境中。由于铁化合物的溶解度较低,它们以氧化物和氧氢氧化物等固体物质的形式存在,能有效吸附过渡金属离子并影响其在水圈中的循环。这一过程不仅发生在水圈,也发生在冰冻圈。本研究通过样品解冻时的原位测量和不解冻时的原位 X 射线荧光 (XRF) 测量,评估了第一排过渡金属阳离子在冰冻条件下对氢氧化铁 (FeOxH) 的吸附情况。通过这两种测量方法的吸附率差异,讨论了过渡金属阳离子在 FeOxH 上的吸附和解吸特性。对于原位 XRF 测量,假设分析物有两种状态(即吸附在 FeOxH 上和溶解在冷冻浓缩溶液 (FCS) 中)的线性回归分析可有效估算吸附率。虽然本文研究的所有金属阳离子(Mn2+、Co2+、Ni2+、Cu2+ 和 Zn2+)在 pH 值为 8 时都能被完全吸附,但用原位 XRF 测定的吸附比要大于在较低 pH 值下解冻时用原位法测定的相应值。这有力地表明,在冷冻条件下,金属阳离子在 FCS 中富集时能很好地吸附在 FeOxH 上,但在解冻时会被解吸。通过比较原位和非原位方法获得的吸附率,发现了 Mn2+ 和 Co2+ 的特定吸附。有趣的是,Mn2+ 的特定吸附是不可逆的,解冻后不会发生解吸。相反,解冻会导致特异性吸附的 Co2+ 解吸,这表明特异性吸附是由不同的机制造成的。
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来源期刊
ACS Earth and Space Chemistry
ACS Earth and Space Chemistry Earth and Planetary Sciences-Geochemistry and Petrology
CiteScore
5.30
自引率
11.80%
发文量
249
期刊介绍: The scope of ACS Earth and Space Chemistry includes the application of analytical, experimental and theoretical chemistry to investigate research questions relevant to the Earth and Space. The journal encompasses the highly interdisciplinary nature of research in this area, while emphasizing chemistry and chemical research tools as the unifying theme. The journal publishes broadly in the domains of high- and low-temperature geochemistry, atmospheric chemistry, marine chemistry, planetary chemistry, astrochemistry, and analytical geochemistry. ACS Earth and Space Chemistry publishes Articles, Letters, Reviews, and Features to provide flexible formats to readily communicate all aspects of research in these fields.
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