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利用中红外激光光谱反向稳定同位素标记分析监测微生物矿化作用。

Monitoring Microbial Mineralization Using Reverse Stable Isotope Labeling Analysis by Mid-Infrared Laser Spectroscopy.

机构信息

Biofilm Centre, University of Duisburg-Essen , Universitätsstrasse 5, 45141 Essen, Germany.

Institute of Groundwater Ecology, Helmholtz Zentrum München , Ingolstädter Landstrasse 1, 85764 Neuherberg, Germany.

出版信息

Environ Sci Technol. 2017 Oct 17;51(20):11876-11883. doi: 10.1021/acs.est.7b02909. Epub 2017 Sep 27.

DOI:10.1021/acs.est.7b02909
PMID:28903553
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5647565/
Abstract

Assessing the biodegradation of organic compounds is a frequent question in environmental science. Here, we present a sensitive, inexpensive, and simple approach to monitor microbial mineralization using reverse stable isotope labeling analysis (RIL) of dissolved inorganic carbon (DIC). The medium for the biodegradation assay contains regular organic compounds and C-labeled DIC with C atom fractions (x(C)) higher than natural abundance (typically 2-50%). The produced CO (x(C) ≈ 1.11%) gradually dilutes the initial x(C) allowing to quantify microbial mineralization using mass-balance calculations. For C-enriched CO samples, a newly developed isotope ratio mid-infrared spectrometer was introduced with a precision of x(C) < 0.006%. As an example for extremely difficult and slowly degradable compounds, CO production was close to the theoretical stoichiometry for anaerobic naphthalene degradation by a sulfate-reducing enrichment culture. Furthermore, we could measure the aerobic degradation of dissolved organic carbon (DOC) adsorbed to granular activated carbon in a drinking water production plant, which cannot be labeled with C. Thus, the RIL approach can be applied to sensitively monitor biodegradation of various organic compounds under anoxic or oxic conditions.

摘要

评估有机化合物的生物降解性是环境科学中常见的问题。在这里,我们提出了一种灵敏、廉价且简单的方法,通过反向稳定同位素标记分析(RIL)监测溶解无机碳(DIC)中的微生物矿化作用。生物降解测定的培养基含有常规有机化合物和 C 标记的 DIC,其 C 原子分数(x(C))高于自然丰度(通常为 2-50%)。产生的 CO(x(C) ≈ 1.11%)逐渐稀释初始 x(C),允许使用质量平衡计算定量微生物矿化作用。对于 C 富集的 CO 样品,引入了一种新开发的同位素比中红外光谱仪,其精度为 x(C) < 0.006%。作为极难降解和缓慢降解化合物的示例,硫酸盐还原富集培养物的厌氧萘降解产生的 CO 接近理论化学计量。此外,我们还可以测量饮用水生产厂中颗粒活性炭吸附的溶解有机碳(DOC)的好氧降解,这些碳不能用 C 标记。因此,RIL 方法可用于灵敏监测缺氧或好氧条件下各种有机化合物的生物降解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f2d/5647565/5d0380f9e53d/es-2017-02909u_0004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f2d/5647565/5fb3705baa92/es-2017-02909u_0001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f2d/5647565/50f49ef84dfe/es-2017-02909u_0002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f2d/5647565/d6780c7202fd/es-2017-02909u_0003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f2d/5647565/5d0380f9e53d/es-2017-02909u_0004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f2d/5647565/5fb3705baa92/es-2017-02909u_0001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f2d/5647565/50f49ef84dfe/es-2017-02909u_0002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f2d/5647565/d6780c7202fd/es-2017-02909u_0003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f2d/5647565/5d0380f9e53d/es-2017-02909u_0004.jpg

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