Institute of Environmental Assessment and Water Research, CSIC , Jordi Girona 18, 08034 Barcelona, Spain.
Department of Geology, University of Huelva , Campus "El Carmen" s/n, 21071 Huelva, Spain.
Environ Sci Technol. 2016 Aug 2;50(15):8255-62. doi: 10.1021/acs.est.6b02084. Epub 2016 Jul 12.
Rare earth elements and yttrium (REY) are raw materials of increasing importance for modern technologies, and finding new sources has become a pressing need. Acid mine drainage (AMD) is commonly considered an environmental pollution issue. However, REY concentrations in AMD can be several orders of magnitude higher than in naturally occurring water bodies. With respect to shale standards, the REY distribution pattern in AMD is enriched in intermediate and valuable REY, such as Tb and Dy. The objective of the present work is to study the behavior of REY in AMD passive-remediation systems. Traditional AMD passive remediation systems are based on the reaction of AMD with calcite-based permeable substrates followed by decantation ponds. Experiments with two columns simulating AMD treatment demonstrate that schwertmannite does not accumulate REY, which, instead, are retained in the basaluminite residue. The same observation is made in two field-scale treatments from the Iberian Pyrite Belt (IPB, southwest Spain). On the basis of the amplitude of this process and on the extent of the IPB, our findings suggest that the proposed AMD remediation process can represent a modest but suitable REY source. In this sense, the IPB could function as a giant heap-leaching process of regional scale in which rain and oxygen act as natural driving forces with no energy investment. In addition to having environmental benefits of its treatment, AMD is expected to last for hundreds of years, and therefore, the total reserves are practically unlimited.
稀土元素和钇(REY)是现代技术日益重要的原材料,寻找新的来源已成为当务之急。酸性矿山排水(AMD)通常被认为是一种环境污染问题。然而,AMD 中的 REY 浓度可比自然水体中的浓度高出几个数量级。就页岩标准而言,AMD 中的 REY 分布模式富含中等和有价值的 REY,如 Tb 和 Dy。本工作的目的是研究 REY 在 AMD 被动修复系统中的行为。传统的 AMD 被动修复系统基于 AMD 与基于方解石的渗透基质反应,然后是澄清池。用两个模拟 AMD 处理的柱实验表明,水铁矿不会积累 REY,而是被保留在底绿泥石残渣中。在西班牙西南部伊比利亚黄铁矿带(IPB)的两个现场处理中也观察到了同样的现象。基于这个过程的幅度和 IPB 的范围,我们的发现表明,所提出的 AMD 修复过程可以作为一个适度但合适的 REY 来源。从这个意义上说,IPB 可以作为一个巨大的区域规模的堆浸过程,其中雨水和氧气作为自然驱动力,无需能源投入。除了具有处理 AMD 的环境效益外,AMD 预计将持续数百年,因此,总储量实际上是无限的。