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评价土壤矿物库中铝的迁移:同时受曲霉属菌株酸性和螯合外代谢产物的影响。

Evaluation of aluminium mobilization from its soil mineral pools by simultaneous effect of Aspergillus strains' acidic and chelating exometabolites.

机构信息

Institute of Laboratory Research on Geomaterials, Faculty of Natural Sciences, Comenius University in Bratislava, Mlynská dolina, Ilkovičova 6, 84215 Bratislava, Slovakia.

Institute of Laboratory Research on Geomaterials, Faculty of Natural Sciences, Comenius University in Bratislava, Mlynská dolina, Ilkovičova 6, 84215 Bratislava, Slovakia.

出版信息

J Inorg Biochem. 2018 Apr;181:162-168. doi: 10.1016/j.jinorgbio.2017.09.006. Epub 2017 Sep 13.

Abstract

This contribution investigates aluminium mobilization from main aluminium pools in soils, phyllosilicates and oxyhydroxides, by acidic and chelating exometabolites of common soil fungi Aspergillus niger and A. clavatus. Their exometabolites' acidity as well as their ability to extract aluminium from solid mineral phases differed significantly during incubation. While both strains are able to mobilize aluminium from boehmite and aluminium oxide mixture to some extent, A. clavatus struggles to mobilize any aluminium from gibbsite. Furthermore, passive and active fungal uptake of aluminium enhances its mobilization from boehmite, especially in later growth phase, with strong linear correlation between aluminium bioaccumulated fraction and increasing culture medium pH. We also provide data on concentrations of oxalate, citrate and gluconate which are synthesized by A. niger and contribute to aluminium mobilization. Compared to boehmite-free treatment, fungus reduces oxalate production significantly in boehmite presence to restrict aluminium extraction efficiency. However, in presence of high phyllosilicates' dosages, aluminium is released to an extent that acetate and citrate is overproduced by fungus. Our results also highlight fungal capability to significantly enhance iron and silicon mobility as these elements are extracted from mineral lattice of phyllosilicates by fungal exometabolites alongside aluminium.

摘要

本研究探讨了土壤中主要铝库(如层状硅酸盐和水合氧化物)中铝的迁移,这是通过常见土壤真菌黑曲霉和棒曲霉的酸性和螯合外代谢产物实现的。在孵育过程中,它们的外代谢产物的酸度以及从固体矿物相中提取铝的能力存在显著差异。虽然这两种菌株都能够在一定程度上从勃姆石和氧化铝混合物中迁移铝,但棒曲霉难以从三水铝石中迁移任何铝。此外,真菌对铝的被动和主动摄取会增强其从勃姆石中的迁移能力,尤其是在后期生长阶段,铝的生物累积分数与培养液 pH 值的增加呈强线性相关。我们还提供了由黑曲霉合成并有助于铝迁移的草酸盐、柠檬酸盐和葡萄糖酸盐的浓度数据。与不含勃姆石的处理相比,真菌在存在勃姆石的情况下显著减少了草酸盐的产生,以限制铝的提取效率。然而,在高含量层状硅酸盐存在的情况下,铝被释放到一定程度,以至于真菌会过度产生乙酸盐和柠檬酸盐。我们的研究结果还强调了真菌显著增强铁和硅迁移的能力,因为这些元素是通过真菌的外代谢产物从层状硅酸盐的矿物晶格中提取出来的,与铝一起。

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