干-湿循环大气暴露条件下海相沉积岩有害金属(loid)释放特性研究

Yuto Yoshida, H. Sakanakura, T. Miura, M. Katoh
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引用次数: 0

摘要

现代高速铁路和公路建设中大量挖掘海相沉积岩,释放有害金属(loid),造成环境风险。因此,了解有害金属是如何从开挖的岩石中释放出来是很重要的。研究了干湿循环大气暴露下开挖岩体蚀变表面结构对有害金属(样物质)释放的影响。大气暴露与干湿循环导致颗粒尺寸减小,而不是碳化。此外,它还诱发了草莓状黄铁矿的氧化,导致开挖岩石中硫酸盐离子释放量增加,pH值降低。无定形铁含量随暴露时间的延长而减少。砷、铅、氟离子释放量随大气暴露时间的增加而减少,硒离子释放量逐渐增加。硼的释放量在大气暴露期间是稳定的。在此基础上,本研究认为干湿循环的大气暴露增强/抑制了开挖岩石中有害金属(样物质)的释放。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Behavior of hazardous metal(loid)s release from excavated marine sedimentary rock under atmospheric exposure with drying-wetting cycles
Large amounts of marine sedimentary rock are excavated for the construction of modern high-speed railways and roads, and they pose environmental risk due to the release of hazardous metal(loid)s. It is therefore important understand how hazardous metal(loid)s are released from excavated rock. This study investigated the influences of alteration surface structure of excavated rock induced by atmospheric exposure with drying-wetting cycles on the release of hazardous metal(loid)s. The atmospheric exposure with the drying-wetting cycles caused the particle size reduction, but not carbonation. In addition, it induced the oxidation of framboidal pyrite, resulting in the increase in the sulfate ion release and decrease in the pH in the excavated rock. The amount of amorphous iron content decreased with the increase in the period of atmospheric exposure. The amounts of arsenic, lead, and fluoride ion release were decreased with the increase in the period of atmospheric exposure, while those of selenium was gradually increased. The amount of boron release was stable during the atmospheric exposure. On the basis of these results, this study suggests that the atmospheric exposure with the drying-wetting cycles enhances/suppresses the release of hazardous metal(loid)s from the excavated rock.
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