College of Resources and Environment, Southwest University, Chongqing, 400715, China.
Environ Sci Pollut Res Int. 2020 Mar;27(7):7453-7462. doi: 10.1007/s11356-019-07454-3. Epub 2019 Dec 28.
Soil methane generation mainly driven by soil prokaryotic microbes can be coupled with the degradation of petroleum hydrocarbons (PHCs); however, the relationship between prokaryotic community structure and methane production activity in soil with the potential risk of PHC contamination is seldom reported. In this study, 3 soil samples (CS-1 to CS-3) in the area nearby an exploratory gas well and 5 soil samples (DC-1 to DC-5) in a drill cutting dump area were obtained from the Fuling shale gas field (Chongqing City, China). Then, the prokaryotic community structure was examined by Illumina Miseq sequencing, and the linkage between soil methane production rate (MPR) and prokaryotic community composition was analyzed. The results indicated that 2 samples (DC-4 and DC-5) collected from the drill cutting dump area had significantly higher MPR than the other samples, and a significant and positive relationship (r = 0.44, P < 0.05) was found between soil MPR and soil organic matter (OM) content. The prokaryotic community composition in the sample (DC-5) with the highest MPR was different from those in the other samples, and soil OM and MPR were the major factors significantly correlated with the prokaryotic community structure in this soil. The samples (DC-4 and DC-5) with higher MPR had a higher relative abundance of Archaea and different archaeal community structures from the other samples, and the MPR was the sole factor significantly correlated with the archaeal genus composition in this soil. Therefore, both the prokaryotic and archaeal community structures are essential in the determination of soil MPR, and the bacterial genus of Saccharibacteria and the archaeal genus of Methanolobus might be the key contributors for methane generation in this soil from the shale gas field.
主要由土壤原核微生物驱动的土壤甲烷生成可以与石油烃(PHC)的降解相耦合;然而,在具有 PHC 污染潜在风险的土壤中原核微生物群落结构与甲烷产生活性之间的关系很少有报道。在本研究中,从涪陵页岩气田(中国重庆市)获得了附近勘探气井区域的 3 个土壤样本(CS-1 到 CS-3)和钻井岩屑倾倒区的 5 个土壤样本(DC-1 到 DC-5)。然后,通过 Illumina Miseq 测序检测了原核微生物群落结构,并分析了土壤甲烷产生率(MPR)与原核微生物群落组成之间的联系。结果表明,从钻井岩屑倾倒区采集的 2 个样本(DC-4 和 DC-5)的 MPR 明显高于其他样本,并且土壤 MPR 与土壤有机质(OM)含量之间存在显著正相关关系(r=0.44,P<0.05)。具有最高 MPR 的样本(DC-5)的原核微生物群落组成与其他样本不同,土壤 OM 和 MPR 是与该土壤中原核微生物群落结构显著相关的主要因素。MPR 较高的样本(DC-4 和 DC-5)具有较高的古菌相对丰度和与其他样本不同的古菌群落结构,并且 MPR 是与该土壤中古菌属组成显著相关的唯一因素。因此,原核微生物和古菌群落结构都是确定土壤 MPR 的关键因素,而该页岩气田土壤中的 Saccharibacteria 细菌属和 Methanolobus 古菌属可能是甲烷生成的关键贡献者。