认识到磷矿废物的地质微生物作用,减少采矿废物中的硫化物氧化——漫长的旅程1991-2014

M. Kalin, C. Paulo, W. N. Wheeler
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引用次数: 2

摘要

氧气被认为是采矿废物风化过程的主要驱动力,忽略了微生物的作用。在控制氧气进入废物的许多方法中,自八十年代末以来一直在尝试对矿物表面进行就地处理。加入了包括NPR(天然磷矿)在内的各种材料,期望找到一种磷酸铁涂层。采用NPR化学计量法对废水进行评价,结果不规则且不一致;然而,较低的剂量对出水有一定的改善。由于结果不一致地产生磷酸铁,因此对废水的任何积极影响都被认为是偶然的,因此放弃了该方法。基于基本的生态学考虑,我们怀疑是微生物在起作用。因此,1991年,我们开始在添加NPR的尾矿和废石上进行实验,假设如果矿物表面的化学岩石营养微生物加速氧化,那么异养(耗氧)微生物将减少氧化。8年后,从将NPR埋入地表的尾矿场采集的样本进行了孔隙水质量测试。对露天桶中暴露的废石流出物进行了2.7年的监测。反复地,一次性添加NPR会产生pH值升高和金属酸度降低的出水。后来,对岩石的微观研究发现,在矿物表面有一层有机层。6所不同大学的科学家进行的调查证实了生物膜的存在是酸产生减少的原因。2013年,根据pH值约为1的生物测试方案,异养生物被确定并量化,因为它们覆盖了德国褐煤表面。这些结果表明,异养生物膜的发育和硫化矿废物出水的改善是添加废物NPR的结果。我们的结论是,已经收集了足够的证据来证明地质微生物控制或硫化物氧化的原位控制是一个可行的概念。现在和将来都需要采取措施控制或减少酸性矿井的排放。在本文中,我们记录了在23年的研究中不断发展的生态思维过程,这一步一步地导致了对NPR对硫化物氧化还原的影响的理解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
REDUCING SULFIDE OXIDATION IN MINING WASTES BY RECOGNIZING THE GEOMICROBIAL ROLE OF PHOSPHATE MINING WASTES - A long journey 1991-2014 1
Oxygen has been considered the main driver of the weathering processes in mining wastes, omitting the role of microbes. Among many approaches to control oxygen access to the wastes, in situ treatment of the mineral surface has been tried since the late eighties. Various materials including NPR (Natural Phosphate Rock) were added with the expectation of finding an iron-phosphate coating. Irregular and inconsistent results were obtained when the effluents were evaluated according to NPR stoichiometry; however, the lower dosages showed some improvements in the effluents. Since the results did not consistently produce iron phosphate, any positive effects on effluents were considered accidental and the approach abandoned. We suspected microbes at work based on basic ecological considerations. Hence 1991, we began experimenting on tailings and waste rock with additions of NPR, postulating that if chemo-lithotrophic microbes on the mineral surface accelerate oxidation, then heterotrophic (oxygen-consuming) microbes would reduce oxidation. Samples from tailings plots where NPR was tilled into the surface were tested for pore-water quality after eight years. Effluents from waste rock exposed outdoors in drums were monitored for 2.7 years. Repeatedly, the one-time addition of NPR produced effluents with elevated pH and low metal acidity. Later, microscopic investigations of the rocks found an organic layer on the mineral surfaces. Investigations by scientists in 6 different universities confirmed the presence of a biofilm as the cause of the reduced acid generation. In 2013, heterotrophs were identified and quantified as they covered the surface of German lignite, following a bioleach testing protocol starting at pH around 1. These findings conclusively showed that the development of heterotrophic biofilms and improved effluents from sulfidic mine wastes are a consequence of adding waste NPR. We conclude that sufficient evidence has been gathered to prove that the geo- microbial control or in situ control of sulfide oxidation is a viable concept. It needs to be pursued to control or curtail acid mine drainage now and in the future. In this paper, we document the evolving ecological thought process over 23 years of research, which lead step by step toward understanding of the effects of NPR on the reduction of sulfide oxidation.
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