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[硫酸盐还原菌在三峡库区消落带土壤汞甲基化中的作用]

[Role of Sulfate-Reducing Bacteria in Mercury Methylation in Soil of the Water-Level-Fluctuating Zone of the Three Gorges Reservoir Area].

作者信息

Chen Rui, Chen Hua, Wang Ding-Yong, Xiang Yu-Ping, Shen Hong

机构信息

College of Resources and Environment, Southwest University, Chongqing 400715, China.

Chongqing Engineering Research Center for Agricultural Non-point Source Pollution Control in the Three Gorges Reservoir Area, Chongqing 400716, China.

出版信息

Huan Jing Ke Xue. 2016 Oct 8;37(10):3774-3780. doi: 10.13227/j.hjkx.2016.10.014.

Abstract

Soil simulation experiments with or without addition of external mercury and a non-indigenous bacterium were conducted under laboratory conditions, in order to investigate whether sulfate-reducing bacteria (SRB) are the dominant mercury methylators in the water level fluctuation zone (WLFZ) of the Three Gorges Reservoir, which is a typical periodical wet and dry alternating environment, locating in the Shibaozai Xinzhen Village, Zhong County, Chongqing, China (E108°12'3″ and N30°24'36″). The original soil from the WLFZ was firstly sterilized and then inoculated with or without ( DSM-2603, commercially purchased from the Culture Preservation Center of Microorganisms in Germany, DSMZ) as the control (Test A). The sterilized soils were respectively mixed with 0, 1, or 5 mg·kg Hg soil under submerged and non-submerged conditions to simulate changes in the concentrations of total mercury, methylmercury and the growth of , and the effects of environmental factor on such changes. The results showed that under the submerged situation the release of total mercury (THg) from soils (Test B) increased with the increase of external Hg addition, and the higher the external Hg, the quicker the Hg release was. Meanwhile, displayed an ecological adaptability to mercury and its colony numbers were significantly correlated with the MeHg concentrations in the soil. In soil with 5 mg·kg of external Hg, the total number of reached the highest (3.65×10 cfu·g) while the highest MeHg concentration was 7.60×10 ng·kg. However, on the one hand, the averaged numbers of soil SRB in the test B was only 193 cfu·g. On the other hand, in soil with 5 mg·kgof external Hg, the MeHg concentration was as low as 5.54×10 ng·kg, while no significant relationships were observed between SRB and MeHg. As a result, our results indicated that SRB was not a predominant mercury methylator, while other bacterial groups, either aerobic or anaerobic bacteria, might play an important role in mercury methylation in the WLFZ of the Three Gorges Reservoir, China.

摘要

在实验室条件下进行了添加或不添加外源汞以及一种非本土细菌的土壤模拟实验,目的是研究硫酸盐还原菌(SRB)是否是三峡水库水位涨落带(WLFZ)中汞甲基化的主要细菌,三峡水库位于中国重庆忠县石宝寨新镇(东经108°12′3″,北纬30°24′36″),是典型的周期性干湿交替环境。首先对来自水位涨落带的原始土壤进行灭菌,然后接种或不接种(DSM-2603,从德国微生物菌种保藏中心DSMZ商业购买)作为对照(试验A)。将灭菌后的土壤在淹水和非淹水条件下分别与0、1或5 mg·kg汞土壤混合,以模拟总汞、甲基汞浓度的变化以及的生长情况,以及环境因素对这些变化的影响。结果表明,在淹水情况下,土壤中总汞(THg)的释放量(试验B)随着外源汞添加量的增加而增加,外源汞含量越高,汞释放越快。同时,对汞表现出生态适应性,其菌落数与土壤中甲基汞浓度显著相关。在添加5 mg·kg外源汞的土壤中,总数达到最高(3.65×10 cfu·g),而最高甲基汞浓度为7.60×10 ng·kg。然而,一方面,试验B中土壤SRB的平均数量仅为193 cfu·g。另一方面,在添加5 mg·kg外源汞的土壤中,甲基汞浓度低至5.54×10 ng·kg,而SRB与甲基汞之间未观察到显著关系。因此,我们的结果表明,SRB不是主要的汞甲基化菌,而其他细菌类群,无论是好氧菌还是厌氧菌,可能在中国三峡水库水位涨落带的汞甲基化过程中起重要作用。

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