He Wenmei, Kim Youjin, Ko Daegeun, Yun Seongtaek, Jun Seongchun, Yoo Gayoung
Department of Applied Environmental Science, Kyung Hee University, Republic of Korea.
Department of Environmental Engineering, Konkuk University, Republic of Korea.
Sci Total Environ. 2019 Nov 10;690:40-49. doi: 10.1016/j.scitotenv.2019.06.400. Epub 2019 Jun 24.
Potential CO leakage is a major concern for carbon capture and storage (CCS). The effects of high soil CO concentration on microbes is a major element of impact assessments of CO leakage on terrestrial ecosystems. We conducted a field experiment to investigate the responses of microbial functional groups of ammonia-oxidizers, methanogens, and methanotrophs in high soil CO conditions. A single-point injection gassing plot (2.5 m × 2.5 m in size), which had 52.2% CO in the center (radius = 0.5 m) and 5.5% in the edge (radius = 1.7 m) at 10 cm depth, was employed. NO and CH emissions increased after 1 day of injection because injected CO was instantly utilized by nitrifiers and methanogens. This suggests that the activities of the selected microbes could be stimulated by high soil CO concentrations. Prolonged CO injection has toxic effects on aerobic nitrifiers, but may favor anaerobic methanogens. However, the early stimulatory effects of high soil CO on NO and CH production did not last to the end of injection. These results imply that increased NO and CH emissions could be the minor side effects of high soil CO. Microbes responded faster than plants to high soil CO, with responses observed as late as 7 days after injection. The inhibition of plant absorption of soil water and nutrients by high soil CO concentrations may also influence microbial responses. Moreover, high soil water content could retard underground CO diffusion, which would magnify CO impacts on plants and microbes. Our results suggest that microbial response could be used as an early indicator of the impact assessments of CO leakage on soil ecosystems. An understanding of the interaction among soils, plants, and microbes would be helpful in assessing the biological risks of potential CO leakage.
潜在的一氧化碳泄漏是碳捕获与封存(CCS)的一个主要问题。土壤中高浓度一氧化碳对微生物的影响是一氧化碳泄漏对陆地生态系统影响评估的一个主要因素。我们进行了一项田间试验,以研究在高土壤一氧化碳条件下氨氧化菌、产甲烷菌和甲烷氧化菌等微生物功能群的响应。采用了一个单点注入式充气地块(尺寸为2.5米×2.5米),在10厘米深度处,地块中心(半径 = 0.5米)的一氧化碳含量为52.2%,边缘(半径 = 1.7米)为5.5%。注入1天后,一氧化氮和甲烷排放增加,因为注入的一氧化碳立即被硝化细菌和产甲烷菌利用。这表明高土壤一氧化碳浓度可能刺激所选微生物的活性。长时间注入一氧化碳对好氧硝化细菌有毒性作用,但可能有利于厌氧产甲烷菌。然而,高土壤一氧化碳对一氧化氮和甲烷产生的早期刺激作用并没有持续到注入结束。这些结果意味着一氧化氮和甲烷排放增加可能是高土壤一氧化碳的次要副作用。微生物对高土壤一氧化碳的响应比植物更快,在注入后7天仍可观察到响应。高土壤一氧化碳浓度对植物吸收土壤水分和养分的抑制作用也可能影响微生物的响应。此外,高土壤含水量可能会阻碍地下一氧化碳的扩散,这会放大一氧化碳对植物和微生物的影响。我们的结果表明,微生物响应可作为一氧化碳泄漏对土壤生态系统影响评估的早期指标。了解土壤、植物和微生物之间的相互作用将有助于评估潜在一氧化碳泄漏的生物风险。