Zhang Ning, Zhang Dong-Dong, Ji Hong-Da, Yu Xin-Wei, Zhang Zhi-Chao, Yang Sheng-Mao, Zhang Chun-Fang
Institute of Marine Biology, Ocean College, Zhejiang University, Hangzhou, China.
Wuxi Dongfang Environmental Engineering Design and Research Institute, Wuxi, China.
Front Microbiol. 2018 Jun 8;9:1225. doi: 10.3389/fmicb.2018.01225. eCollection 2018.
Herein, we investigated the chemical, electrochemical, and spectroscopic characteristics of humic acids (HAs) extracted from sediments of different origin [Ling Qiao river, Xi Xi wetland, Qi Zhen lake (QZ), and Hu Zhou pond in Zhejiang province, China], paying particular attention to their role in the enhancement of nitrate and FeOOH reduction. Notably, the highest C/N ratio (16.16), O/C ratio (1.89), and Fe content (11.57 g kg sample) were observed for HAs extracted from QZ sediment. Cyclic voltammetry analyses confirmed that all HAs contained redox-active groups and exhibited redox potentials between -0.36 and -0.28 V vs. the standard hydrogen electrode. All HAs showed similar Fourier transform infrared spectra with variable absorption intensity, the spectra verified the presence of aromatic C=C, C-H, and C=O of quinone ketones group in HAs. Electron spin resonance suggested that quinone moieties within HAs are the redox-active centers. All HAs promoted the microbial reduction of nitrate and amorphous FeOOH by strain MR-1, achieving high nitrate reduction extents of 79-98.4%, compared to the biotic and abiotic control values of 29.6 and 0.006%, respectively. The corresponding extents of Fe(II) production equaled 43.25-60.5%, exceeding those of biotic and abiotic controls (28.5 and 0.005%, respectively). In addition to the highest C/N, O/C ratio, and Fe content, HA extracted from QZ sediment also exhibited the highest nitrate and FeOOH reduction performances. Although the proportion of organic redox-active carbon is small, the potential electron-mediating ability is not ignorable. HAs are redox active for enhancing microbial reduction of nitrate and amorphous FeOOH regardless of the location or texture of parent sediments, implying their great potential for acting as redox mediator in enhancing multiple microbial reduction, thereby affecting various biogeochemical processes (i.e., iron cycle, nitrogen cycle, etc.) as well as remediation in anaerobic environment.
在此,我们研究了从不同来源(中国浙江省的灵桥河、西溪湿地、栖真湖(QZ)和湖州池塘)沉积物中提取的腐殖酸(HAs)的化学、电化学和光谱特性,特别关注它们在促进硝酸盐和FeOOH还原中的作用。值得注意的是,从QZ沉积物中提取的HAs的C/N比最高(16.16)、O/C比最高(1.89)以及铁含量最高(11.57 g/kg样品)。循环伏安法分析证实,所有HAs都含有氧化还原活性基团,相对于标准氢电极,其氧化还原电位在-0.36至-0.28 V之间。所有HAs都显示出相似的傅里叶变换红外光谱,只是吸收强度不同,光谱证实了HAs中存在芳香族C=C、C-H以及醌酮基团的C=O。电子自旋共振表明,HAs中的醌部分是氧化还原活性中心。所有HAs都促进了菌株MR-1对硝酸盐和无定形FeOOH的微生物还原,与生物对照值29.6%和非生物对照值0.006%相比,实现了79 - 98.4%的高硝酸盐还原程度。相应的Fe(II)生成程度等于43.25 - 60.5%,超过了生物对照和非生物对照(分别为28.5%和0.005%)。除了具有最高的C/N、O/C比和铁含量外,从QZ沉积物中提取的HA还表现出最高的硝酸盐和FeOOH还原性能。尽管有机氧化还原活性碳的比例较小,但其潜在的电子介导能力不可忽视。无论母体沉积物的位置或质地如何,HAs都具有氧化还原活性,可增强微生物对硝酸盐和无定形FeOOH的还原,这意味着它们在增强多种微生物还原方面具有巨大的潜力,从而影响各种生物地球化学过程(如铁循环、氮循环等)以及厌氧环境中的修复。