Gnandi K, Tobschall H J
Institute of Geology and Mineralogy, Chair of Applied Geology, Erlangen, Germany.
Sci Total Environ. 1999 Sep 15;236(1-3):181-90. doi: 10.1016/s0048-9697(99)00279-x.
A number of laboratory experiments were carried out to assess the desorption of trace metals from sedimentary phosphorite samples into artificial seawater. Shaking and percolation experiments have been performed on phosphorite samples from the Cd-rich phosphorite deposits of Hahotoé-Kpogamé (Togo, West Africa) using artificial seawater in the ratio 1:10. The results show that elevated concentrations of trace elements Cd(17-256 micrograms/l), Ni (12-193 micrograms/l), Zn (21-200 micrograms/l) and major elements Al (6-1915 micrograms/l) and Fe (30-1264 micrograms/l) are released into seawater by desorption processes. Maxima of trace metals with high mobility are reached within 4 h indicating the fast desorption kinetics in seawater. Thus, the direct disposal of potentially toxic metal-rich mine tailings may lead to regional coastal water pollution.
进行了多项实验室实验,以评估痕量金属从沉积磷块岩样品中解吸到人工海水中的情况。使用比例为1:10的人工海水,对来自哈霍托埃 - 克波加梅(多哥,西非)富含镉的磷块岩矿床的磷块岩样品进行了振荡和渗滤实验。结果表明,通过解吸过程,痕量元素镉(17 - 256微克/升)、镍(12 - 193微克/升)、锌(21 - 200微克/升)以及主要元素铝(6 - 1915微克/升)和铁(30 - 1264微克/升)的浓度升高并释放到海水中。具有高迁移率的痕量金属在4小时内达到最大值,表明在海水中解吸动力学很快。因此,直接处置富含潜在有毒金属的尾矿可能会导致区域沿海水体污染。