首页> 外文期刊>Journal of Contaminant Hydrology >Short and long term release mechanisms of arsenic, selenium and boron from a tunnel-excavated sedimentary rock under in situ conditions
【24h】

Short and long term release mechanisms of arsenic, selenium and boron from a tunnel-excavated sedimentary rock under in situ conditions

机译:隧道开挖沉积岩中原位条件下砷,硒和硼的短期和长期释放机理

获取原文
获取原文并翻译 | 示例
           

摘要

Sedimentary rocks of marine origin excavated from tunnel construction projects usually contain background levels of hazardous trace elements, but when exposed to the environment, they generate leachates with concentrations of arsenic (As), selenium (Se) and boron (B) exceeding the WHO guideline for drinking water. In this study, the leaching of As, Se and B was evaluated under in situ conditions at various flow patterns, particle size distributions and column thicknesses. The results showed that these trace elements were leached out of the rock via short and long term mechanisms. In the short term, all three elements were rapidly and simultaneously released due to the dissolution of soluble evaporite salts formed from entrapped sea water of the Cretaceous. After their rapid release, however, these trace elements behaved differently as a result of their contrasting adsorption affinities onto minerals like clays and Feoxyhydroxides, which were further influenced by the pH, presence of coexisting ions and speciation of the trace elements. Selenium was quickly and easily transported out of the columns because it was mostly present as the very mobile selenate ion (Se[VI]). In comparison, the migration of As and B was hindered by adsorption reactions onto mineral phases of the rock Boron was initially the least mobile among the three because of its preferential adsorption onto clay minerals that was further enhanced by the slightly alkaline pH and high concentrations of Ca2+ and Na+. However, it was gradually re-mobilized in the latter part of the experiments because it was only weakly adsorbed via outer sphere complexation reactions. In the long term, the rock continued to release substantial amounts of As, Se and B via pyrite oxidation and adsorption/desorption reactions, which were regulated by the temperature and rainfall intensity/frequency on site. (C) 2015 Elsevier B.V. All rights reserved.
机译:从隧道建设项目中挖出的海洋沉积岩通常含有有害痕量元素的背景水平,但是当暴露于环境中时,它们会产生砷,砷,硼和硼的浓度超过世界卫生组织准则的渗滤液。喝水在这项研究中,As,Se和B的浸出在原位条件下以各种流动模式,粒径分布和柱厚进行了评估。结果表明,这些微量元素是通过短期和长期机制从岩石中浸出的。在短期内,由于从白垩纪夹带的海水中形成的可溶性蒸发盐的溶解,所有这三种元素迅速而同时释放。但是,这些微量元素在快速释放后,由于它们在矿物上的对比吸附亲和力不同而表现出不同,如粘土和Feoxyhydroxides,它们进一步受pH,共存离子的存在和微量元素的形态的影响。硒可以快速,轻松地从色谱柱中运出,因为它主要以非常易移动的硒离子(Se [VI])的形式存在。相比之下,砷和硼的迁移受到吸附反应的阻碍,从而阻碍了硼在岩石矿物相中的移动,因为硼优先吸附在粘土矿物上,而硼在三种碱中的迁移率最低。 Ca2 +和Na +。然而,由于它仅通过外球络合反应被弱吸收,因此在实验的后半部分逐渐被重新使用。从长远来看,岩石继续通过黄铁矿氧化和吸附/解吸反应释放大量的As,Se和B,这些反应受现场温度和降雨强度/频率的调节。 (C)2015 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《Journal of Contaminant Hydrology》 |2015年第apraama期|60-71|共12页
  • 作者单位

    Hokkaido Univ, Fac Engn, Div Sustainable Resources Engn, Sapporo, Hokkaido 060, Japan|Publ Works Res Inst, Civil Engn Res Inst Cold Reg, Sapporo, Hokkaido, Japan;

    Hokkaido Univ, Fac Engn, Div Sustainable Resources Engn, Sapporo, Hokkaido 060, Japan;

    Hokkaido Univ, Fac Engn, Div Sustainable Resources Engn, Sapporo, Hokkaido 060, Japan;

    Hokkaido Univ, Fac Engn, Div Sustainable Resources Engn, Sapporo, Hokkaido 060, Japan;

    Hokkaido Univ, Fac Engn, Div Sustainable Resources Engn, Sapporo, Hokkaido 060, Japan;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Arsenic; Boron; Selenium; Sedimentary rock; Leaching; In situ column experiments;

    机译:砷硼硒沉积岩浸出原位柱实验;

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号