An Experimental Study on Bio-Clogging in Porous Media during Geothermal Water Reinjection

Jianguo Feng, Yao Zhao, Deshuai Ji, Zong-jun Gao
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引用次数: 1

Abstract

To study the mechanism of bio-clogging in a porous medium during the reinjection of geothermal water and to improve reinjection efficiency, an indoor one-dimensional reinjection experiment was conducted based on the geological model of the geothermal reinjection demonstration project in Dezhou City. The biological process of porous media clogging was investigated by analyzing the variation of permeability within the medium, the main indexes of nutrient salts, and the content of extracellular polymeric substances (EPS). High-throughput sequencing, based on 16S rRNA, was used to analyze the characteristics and succession of microbial communities during the reinjection of geothermal water. The results of the study show that significant bio-clogging occurs during the reinjection of geothermal water, with an increase in the heterogeneity of the thermal reservoir medium, and a decrease in permeability. The extent of clogging gradually reduces with an increase in seepage path. Thus, thermal reservoir clogging is more serious closer to the water inlet. With an increase in the duration of reinjection, the permeability of the porous medium undergoes three stages: “rapid”, “decline-slow”, and “decrease-stable”. The results show that the richness and diversity of the bacterial community increase and decrease, respectively, during the reinjection process. Bacterial community succession occurs, and the bacterial communities mainly include the Proteobacteria and Bacteroidetes phyla. Pseudomonas and Devosia are respectively the dominant bacteria in the early and late stages of geothermal water reinjection.
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地热水回注过程中多孔介质生物堵塞的实验研究
为研究地热水回注过程中多孔介质中的生物堵塞机理,提高回注效率,以德州市地热回注示范工程地质模型为基础,进行了室内一维回注实验。通过分析多孔介质的渗透性变化、营养盐的主要指标和细胞外聚合物(EPS)的含量,研究了多孔介质堵塞的生物过程。采用基于16S rRNA的高通量测序技术,分析地热水回注过程中微生物群落的特征及演替。研究结果表明,地热水回注过程中存在明显的生物堵塞现象,热储介质非均质性增加,渗透率降低。随着渗流路径的增加,堵塞程度逐渐减小。因此,靠近进水口处的热储堵塞更严重。随着回注时间的延长,多孔介质渗透率经历了“快速”、“下降-缓慢”和“下降-稳定”三个阶段。结果表明,在回注过程中,细菌群落的丰富度和多样性分别增加和减少。细菌群落发生演替,细菌群落主要包括变形菌门和拟杆菌门。假单胞菌(Pseudomonas)和Devosia分别是地热水回注前期和后期的优势菌。
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