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从饮用水分配系统中不同层的铸铁腐蚀层中富集的 Cr(III)和 Cr(VI)后释放的 Cr:pH 值、温度、硫酸盐和氯化物的影响。

Cr release after Cr(III) and Cr(VI) enrichment from different layers of cast iron corrosion scales in drinking water distribution systems: the impact of pH, temperature, sulfate, and chloride.

机构信息

Department of Environmental Engineering, School of Environmental Science and Engineering, Tianjin University, Tianjin, 300072, China.

出版信息

Environ Sci Pollut Res Int. 2022 Mar;29(13):18778-18792. doi: 10.1007/s11356-021-15754-w. Epub 2021 Oct 26.

Abstract

Chromium accumulated from source water and pipeline lining materials in corrosion scales could potentially be released into bulk water in drinking water distribution systems (DWDS). This study examined the influence of pH (pH 4, pH 5.5, pH 7, pH 8.5, pH 10), temperature (5 °C, 15 °C, 25 °C), sulfate (50 mg/L, 150 mg/L, 250 mg/L), and chloride (50 mg/L, 150 mg/L, 250 mg/L) on chromium accumulation and release between iron corrosion scale phase and the surrounding water phase. For the first time, the accumulation and release behaviors of chromium were assessed and compared in two distinct layers of iron corrosion scales based on the speciation distributions of heavy metals. Results showed that in the outer and inner layers of corrosion scales, chromium exhibited an almost similar trend but significant differences in quantity, with the outer layer accumulating less and releasing more. In particular, the average difference of chromium released after Cr(VI) enrichment from the outer and inner layers was 50.53 μg/L under the same conditions. Further studies conclusively showed that in Cr(VI) accumulation process, a portion of Cr(VI) would be reduced to Cr(III) by Fe(II) in iron corrosion scales. The mechanisms of chromium retention based on different iron (oxyhydr)oxides were discussed.

摘要

铬可从源水和腐蚀层中的管道衬里材料中积累,并有可能在饮用水分配系统(DWDS)中释放到水体中。本研究考察了 pH 值(4、5.5、7、8.5、10)、温度(5°C、15°C、25°C)、硫酸盐(50、150、250mg/L)和氯化物(50、150、250mg/L)对铁腐蚀层相与周围水相之间的铬积累和释放的影响。首次根据重金属的形态分布,评估并比较了在铁腐蚀层的两个不同层中的铬的积累和释放行为。结果表明,在外层和内层腐蚀层中,铬表现出几乎相似的趋势,但在数量上存在显著差异,外层积累的铬较少,释放的铬较多。特别是,在相同条件下,Cr(VI)富集后从内外层释放的铬的平均差异为 50.53μg/L。进一步的研究明确表明,在 Cr(VI)积累过程中,一部分 Cr(VI)会被铁腐蚀层中的 Fe(II)还原为 Cr(III)。讨论了基于不同铁(氧)氢氧化物的铬保留机制。

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