首页> 外文期刊>Journal of Geochemical Exploration: Journal of the Association of Exploration Geochemists >Origin and distribution of low molecular weight organic acids and bacteria in a depth profile of a soil covered tailings impoundment in northern Sweden
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Origin and distribution of low molecular weight organic acids and bacteria in a depth profile of a soil covered tailings impoundment in northern Sweden

机译:低分子量有机酸和细菌在瑞典北部土壤覆盖的尾矿库深度剖面中的起源和分布

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摘要

The tailings at Kristineberg,northern Sweden,have a very low content of organic carbon,a feature common with many sulfidic tailing impoundments.Three different experiments were set-up to assess the role of carbon dioxide in a depth profile.Firstly,pore gas was collected in vials from ground water pipes at various points in the profile of a dry covered tailings impoundment and analyzed in the laboratory for CO2,O2,N2,H2,and CH4 contents.Secondly,pore water was extracted from tension lysimeters at various depths.This water was analyzed for numbers of bacteria (iron-oxidizing and sulfur-oxidizing,both by MPN),and low molecular weight organic acids.Thirdly,Acidithiobacillus ferrooxidans (Strain DSMZ No 1927) was grown on a mixture of irradiated tailings and sterile water.The amount of organic acids produced was monitored.The largest bacterial count of iron-oxidizing bacteria,4.7x10~5/g tailings,was at the oxidation front,while the heterotrophic sulfur-oxidizing bacteria were mainly found in the unsaturated,oxidized zone,2.65 x 10~4/g tailings.The oxidation front was also the location where the largest amount of organic acids was found in the field study (formate 0.83 mg/1 and acetate 0.51 mg/1).The acetic acid found coincides with the highest count of iron-oxidizing bacteria.The intrusion of O2 and CO2 at the studied location is enough for microbiological activity,although the overall effect on AMD production is not addressed.The results from laboratory incubations indicate that the microbial community produces organic carbon with CO2 as the sole carbon source,up to 1.35 mg/1 after 16 weeks measured as TOC.To conclude,we suggest that knowledge of the intrusion of both CO2 and O2 is vital for a full understanding of the microbial ecology,and thus the weathering processes,in a dry covered tailings impoundment.Hence,the CO2 produced in the till cover and entering the tailings ecosystem is crucial to the function of the ecosystem.
机译:瑞典北部克里斯汀堡的尾矿有机碳含量非常低,这是许多硫化物尾矿库所共有的特征。建立了三个不同的实验来评估二氧化碳在深度剖面中的作用。在干燥的有盖尾矿库的剖面图上从地下水管的各个点收集小瓶中的水,并在实验室中分析CO2,O2,N2,H2和CH4的含量。其次,从不同深度的张力测定仪中提取孔隙水。分析了水中的细菌数量(通过MPN氧化铁和氧化硫,以及低分子量有机酸)。第三,在辐射尾矿和无菌水的混合物上培养了铁二酸硫杆菌(Sidi DSMZ No 1927)。监测有机酸的产生。铁氧化菌的最大细菌数为4.7x10〜5 / g尾渣,位于氧化前沿,而异养硫氧化菌主要为在不饱和氧化区,尾矿含量为2.65 x 10〜4 / g。在田间研究中,氧化前沿也是有机酸含量最高的位置(甲酸盐0.83 mg / 1,乙酸盐0.51 mg / 1)。所发现的乙酸与最大数量的铁氧化细菌相吻合。虽然未解决对AMD产生的总体影响,但在研究的位置入侵O2和CO2足以实现微生物活性。实验室培养的结果表明,微生物群落以CO2为唯一碳源产生有机碳,以TOC计,其在16周后可达1.35 mg / 1。总而言之,我们建议了解CO2和O2的入侵对于全面了解微生物至关重要在干的覆盖的尾矿库中,其生态学和风化过程因此而发生。因此,在耕层中产生并进入尾矿生态系统的CO2对生态系统的功能至关重要。

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