...
首页> 外文期刊>Hydrometallurgy >The biogeochemistry and microbiology of sulfidic mine waste and bioleaching dumps and heaps, and novel Fe(II)-oxidizing bacteria
【24h】

The biogeochemistry and microbiology of sulfidic mine waste and bioleaching dumps and heaps, and novel Fe(II)-oxidizing bacteria

机译:硫化矿山废料和生物浸出堆肥场以及新型Fe(II)氧化细菌的生物地球化学和微生物学

获取原文
获取原文并翻译 | 示例

摘要

More than 70 microbiological studies of sulfidic mine dumps and heaps have been published. The microbiology and the relevant biogeochemical processes in the dumps and heaps are reviewed and have to be understood for improving copper heap leaching operations and to develop and control countermeasures for the formation of acid mine drainage (AMD). Pyrite or pyrrhotite oxidation is themost relevant biogeochemical process in sulfidicmine waste dumps and heaps and different techniques have been applied to measure reaction rates: column experiments, humidity cells, heat flowmeasurements, or oxygen consumptionmeasurements.Acidophilic Fe(II)- and sulfur-oxidizing microorganisms are most relevant for metal sulfide oxidation. Anaerobic biogeochemical processes in sulfidic mine dumps and heaps are Fe(III)- and sulfate reduction, but little is known about the reaction rates. Fe(III)-reducing microorganisms dissolve Fe(III)(hydr)oxides and may thereby release adsorbed or precipitated metals. Sulfate-reducing microorganisms precipitate and immobilize many metals. Mainly culturing approaches were used to study the microbial communities in sulfidic mine dumps and heaps. More recently,molecular biological techniques have been applied to investigate themicrobial diversity and to quantify andmonitor particular microorganisms. Since acidophilic Fe(II)-oxidizing bacteria and archaea aremost relevant for metal sulfide oxidation, several novel cultures were enriched from sulfidic mine dumps from 10 different countries and maintained in the geomicrobiology laboratory of the Bundesanstalt fur Geowissenschaften und Rohstoffe (BGR). Of 68 analyzed acidophilic Fe(II)-oxidizing cultures, 40 almost full (>1300 bp) 16S rRNA gene sequenceswere obtained and subjected to phylogenetic analysis.Most of the cultivated Fe(II)-oxidizers belonged to four genera. The Gram-positive strains related to Acidimicrobium or Ferrimicrobium were phylogenetically more diverse than the strains of the Gram-negative genera Acidithiobacillus and Leptospirillum and partly represent so far undescribed bacteria. Several cultures also contained novel representatives of the heterotrophic genus Acidiphilium, often previously found in co-culture with Acidithiobacillus ferrooxidans.
机译:已经发表了关于硫化矿堆场和堆肥的70多项微生物学研究。对堆场和堆场的微生物学和相关的生物地球化学过程进行了审查,必须加以理解,以改善铜堆场的浸出操作,并制定和控制形成酸性矿山排水(AMD)的对策。黄铁矿或黄铁矿氧化是硫代次氯酸盐废物堆和堆中最相关的生物地球化学过程,已采用不同的技术来测量反应速率:柱实验,湿度池,热流测量或耗氧量测量。嗜酸性Fe(II)和硫氧化微生物与金属硫化物的氧化最相关。硫化矿排土场中的厌氧生物地球化学过程是Fe(III)和硫酸盐的还原,但对反应速率知之甚少。还原Fe(III)的微生物溶解Fe(III)(氢氧化)氧化物,从而释放出吸附或沉淀的金属。减少硫酸盐的微生物沉淀并固定许多金属。主要采用培养方法来研究硫矿堆和堆肥中的微生物群落。最近,分子生物学技术已被用于研究微生物多样性并定量和监测特定微生物。由于嗜酸性的Fe(II)氧化细菌和古细菌与金属硫化物的氧化最相关,因此从10​​个不同国家的硫化矿堆中富集了数种新颖的培养物,并保存在德国联邦地质与生物基金会(BGR)的地球微生物实验室中。在68种经分析的嗜酸性Fe(II)氧化培养物中,获得了40个几乎完整(> 1300 bp)的16S rRNA基因序列,并进行了系统发育分析。大多数培养的Fe(II)氧化剂属于四个属。与酸性微生物或亚铁细菌有关的革兰氏阳性菌株在系统发育上比革兰氏阴性嗜酸性硫杆菌和钩端螺旋菌的菌株更加系统化,部分代表了迄今未描述的细菌。几种文化还包含异养嗜酸菌属的新代表,这种菌通常以前在与酸性氧化硫杆菌共培养时发现。

著录项

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