Characterization of Manganese Oxide Modified Activated Carbon for Remediation of Redox-Sensitive Contaminants

IF 2.9 3区 化学 Q2 CHEMISTRY, MULTIDISCIPLINARY
Edwin Rivas Meraz*, Samuel J. Traina, Marc W. Beutel and Peggy A. O’Day, 
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Abstract

Manganese oxide modified activated carbon (MOMAC) was synthesized as a novel in situ sediment and soil amendment for treatment of redox-sensitive contaminants, such as mercury (Hg), through buffering of reduction–oxidation (redox) potential and sorption. This study characterized MOMAC synthesis products at three different Mn concentrations on activated carbon (AC) surfaces and compared them with homogeneously precipitated Mn oxide (MnOx) and unmodified AC for properties influencing redox buffering and sorption capacity. Bulk spectroscopic analyses (XAS and XPS), XRD, and electron microscopy showed that homogeneous MnOx matched the local structure of vernadite (δ-Mn(IV)O2), while MOMAC formed aggregates on the AC surface composed mostly of vernadite with fractions of manganite (γ-Mn(III)OOH) (17–46%) and sorbed Mn(II) (11–21%). Higher bulk surface area and lower Mn average oxidation state were associated with MOMAC and are attributed to the reduction of Mn(IV) by Mn(II) adsorbed on AC or diffused into AC pores. Cation exchange reactions of Na+ and Ca2+ also contributed to Mn oxidation state changes by driving disproportionation of Mn(III) to Mn(II) and Mn(IV). In batch slurry experiments with and without Hg-contaminated sediment from Oak Ridge National Laboratory (TN, U.S.A.), addition of MOMAC and MnOx resulted in higher solution redox potential and lower pH compared to AC and no-amendment controls. MnOx poised solution redox at higher potential than MOMAC, but MOMAC was more effective at sorbing Hg released by the oxidation of sediment HgS(s), Hg0, and/or organic-associated Hg. By combining redox buffering with sorption, MOMAC is a promising in situ amendment that may efficiently target redox-sensitive contaminants in aquatic sediments.

Abstract Image

氧化锰改性活性炭对氧化还原敏感污染物的修复性能研究
锰氧化物改性活性炭(MOMAC)是一种新型的原位沉积物和土壤改改剂,通过缓冲还原-氧化电位和吸附来处理汞(Hg)等氧化还原敏感污染物。本研究在活性炭(AC)表面表征了三种不同Mn浓度下的MOMAC合成产物,并将其与均匀沉淀的Mn氧化物(MnOx)和未改性的AC进行了比较,比较了它们对氧化还原缓冲和吸附能力的影响。体谱分析(XAS和XPS)、XRD和电镜分析表明,均相的MnOx在AC表面形成的团聚体主要由vernadite和部分锰矿(γ-Mn(III)OOH)(17-46%)和吸附Mn(II)(11-21%)组成。较大的体积表面积和较低的Mn平均氧化态与MOMAC有关,这是由于Mn(II)被吸附在AC上或扩散到AC孔中而对Mn(IV)进行了还原。Na+和Ca2+的阳离子交换反应也通过驱动Mn(III)歧化成Mn(II)和Mn(IV)来促进Mn氧化态的变化。在美国橡树岭国家实验室(Oak Ridge National Laboratory, TN, U.S.A.)进行的含和不含汞污染沉积物的料浆试验中,添加MOMAC和MnOx的溶液氧化还原电位更高,pH值更低。MnOx平衡溶液的氧化还原电位高于MOMAC,但MOMAC更有效地吸收由沉积物HgS(s)、Hg0和/或有机相关汞氧化释放的汞。通过将氧化还原缓冲与吸附相结合,MOMAC是一种很有前途的原位修正剂,可以有效地靶向水生沉积物中氧化还原敏感污染物。
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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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