Spatiotemporal variations of sand hydraulic conductivity by microbial application methods

IF 9.4 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Journal of Rock Mechanics and Geotechnical Engineering Pub Date : 2024-01-01 DOI:10.1016/j.jrmge.2023.04.024
Viroon Kamchoom , Thiti Khattiwong , Treesukon Treebupachatsakul , Suraparb Keawsawasvong , Anthony Kwan Leung
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Abstract

The spatiotemporal distributions of microbes in soil by different methods could affect the efficacy of the microbes to reduce the soil hydraulic conductivity. In this study, the specimens of bio-mediated sands were prepared using three different methods, i.e. injecting, mixing, and pouring a given microbial solution onto compacted sand specimens. The hydraulic conductivity was measured by constant-head tests, while any soil microstructural changes due to addition of the microbes were observed by scanning electron microscope (SEM) and mercury intrusion porosimetry (MIP) tests. The amount of dextran concentration produced by microbes in each type of specimen was quantified by a refractometer. Results show that dextran production increased exponentially after 5–7 d of microbial settling with the supply of culture medium. The injection and mixing methods resulted in a similar amount and uniform distribution of dextran in the specimens. The pouring method, however, produced a nonuniform distribution, with a higher concentration near the specimen surface. As the supply of culture medium discontinued, the dextran content near the surface produced by the pouring method decreased dramatically due to high competition for nutrients with foreign colonies. Average dextran concentration was negatively and correlated with hydraulic conductivity of bio-mediated soils exponentially, due to the clogging of large soil pores by dextran. The hydraulic conductivity of the injection and mixing cases did not change significantly when the supply of culture medium was absent.

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微生物应用方法对砂土水力导电性时空变化的影响
不同方法下微生物在土壤中的时空分布会影响微生物降低土壤导水性的效果。本研究采用三种不同的方法制备生物介导砂试样,即在压实的砂试样上注入、混合和浇注给定的微生物溶液。通过恒定水头试验测量水力传导性,同时通过扫描电子显微镜(SEM)和汞侵入孔隙度(MIP)试验观察添加微生物后土壤微观结构的变化。每种试样中微生物产生的葡聚糖浓度都用折射仪进行了量化。结果表明,在微生物沉淀 5-7 天后,随着培养基的供应,葡聚糖的产量呈指数增长。注射法和混合法在试样中产生的葡聚糖数量相似,分布均匀。然而,浇注法产生的右旋糖酐分布不均匀,靠近试样表面的浓度较高。随着培养基供应的停止,由于与外来菌落争夺养分,浇注法产生的靠近表面的葡聚糖含量急剧下降。由于右旋糖酐堵塞了大的土壤孔隙,平均右旋糖酐浓度与生物介导土壤的导水率呈指数负相关。在不提供培养基的情况下,注入法和混合法的水力传导率变化不大。
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来源期刊
Journal of Rock Mechanics and Geotechnical Engineering
Journal of Rock Mechanics and Geotechnical Engineering Earth and Planetary Sciences-Geotechnical Engineering and Engineering Geology
CiteScore
11.60
自引率
6.80%
发文量
227
审稿时长
48 days
期刊介绍: The Journal of Rock Mechanics and Geotechnical Engineering (JRMGE), overseen by the Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, is dedicated to the latest advancements in rock mechanics and geotechnical engineering. It serves as a platform for global scholars to stay updated on developments in various related fields including soil mechanics, foundation engineering, civil engineering, mining engineering, hydraulic engineering, petroleum engineering, and engineering geology. With a focus on fostering international academic exchange, JRMGE acts as a conduit between theoretical advancements and practical applications. Topics covered include new theories, technologies, methods, experiences, in-situ and laboratory tests, developments, case studies, and timely reviews within the realm of rock mechanics and geotechnical engineering.
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