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微生物代谢过程诱导的蒙脱石层间结合有机物质的变化。

Variation of preserving organic matter bound in interlayer of montmorillonite induced by microbial metabolic process.

机构信息

School of Environment and Resource, Southwest University of Science and Technology, Mianyang, Sichuan Province, 621010, China.

Key Laboratory of Solid Waste Treatment and Resource Recycle, Ministry of Education, Mianyang, Sichuan Province, 621010, China.

出版信息

Environ Sci Pollut Res Int. 2018 Aug;25(23):22348-22355. doi: 10.1007/s11356-017-9806-7. Epub 2017 Jul 25.

Abstract

This paper aimed to investigate the variation of preserving organic matter bound in the interlayer space of montmorillonite (Mt) induced by a microbe metabolic process. We selected Bacillus pumilus as the common soil native bacteria. The alteration of d value, functional group, and C,N organic matter contents caused by bacteria were analyzed by XRD, FTIR, and elementary analyzer, respectively. XRD results showed that the d value of montmorillonite increased with the concentration decreasing and decreased with the culture time increasing after interacting with bacteria indicating the interlayer space of montmorillonite was connected with the organic matter. The findings of long-term interaction by resetting culture conditions implied that the montmorillonite buffered the organic matter when the nutrition was enough and released again when the nutrition was lacking. The results of the elementary analyzer declared the content of organic matter was according to the d value of montmorillonite and N organic matter which played a major impact. FTIR results confirmed that the Si-O stretching vibrations of Mt were affected by the functional group of organic matter. Our results showed that the montmorillonite under the influence of soil bacteria has a strong buffering capacity for preserving organic matter into the interlayer space in a short-term. It might provide critical implications for understanding the evolution process and the preservation of fertilization which was in the over-fertilization or less-fertilization conditions on farmland.

摘要

本文旨在研究微生物代谢过程引起的蒙脱石(Mt)层间空间中有机物质保存的变化。我们选择短小芽孢杆菌作为常见的土壤本土细菌。通过 X 射线衍射(XRD)、傅里叶变换红外光谱(FTIR)和元素分析仪分别分析了细菌引起的 d 值、官能团和 C、N 有机物质含量的变化。XRD 结果表明,蒙脱石的 d 值随着与细菌相互作用的浓度降低而增加,随着培养时间的增加而降低,表明蒙脱石的层间空间与有机物质相连。重新设定培养条件的长期相互作用结果表明,当营养充足时,蒙脱石缓冲有机物质,当营养缺乏时再释放有机物质。元素分析仪的结果表明,有机物质的含量与蒙脱石的 d 值和 N 有机物质的含量有关,而 N 有机物质的含量影响较大。FTIR 结果证实,Mt 的 Si-O 伸缩振动受到有机官能团的影响。我们的结果表明,在土壤细菌的影响下,蒙脱石在短期内对保存有机物质进入层间空间具有很强的缓冲能力。这可能对理解农田在过度施肥或施肥不足条件下的施肥演变过程和保存具有重要意义。

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