Consolidation of Sand Particles by Nanoparticles of Calcite after Concentrating Ureolytic Bacteria In Situ

S. Al-Thawadi, R. Cord-Ruwisch, M. Bououdina
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引用次数: 22

Abstract

ABSTRACT Ureolytic bacteria in the presence of high concentration of urea and calcium ions will precipitate calcite crystals in the form of nanocrystal aggregates. Those aggregates consolidate sandy materials by forming bridging points between sand particles. Bacterial cells that were isolated in a previous study, Bacillus sp. MCP11 (DSM 23526), were successfully concentrated in situ by up-loading 3-void volumes of cells followed by cementation solution (calcium/urea). Sandstone with UCS of 1200 kPa was formed with three applications of cells and cementation solution without clogging the void spaces resulting in a permeable consolidated sand core. ESEM images, EDS, and XRD analysis for the consolidated sandstone showed nanoparticles of rhombohedral calcite crystals aggregates of very fine particles at the nanoscale forming point-to-point contact between the sand particles.
溶尿细菌原位富集后方解石纳米颗粒对砂粒的固结作用
摘要:溶尿菌在高浓度尿素和钙离子存在下,会析出方解石晶体,以纳米晶聚集体的形式析出。这些集料通过在沙粒之间形成桥接点来巩固沙质物质。在先前的研究中分离的细菌细胞芽孢杆菌sp. MCP11 (DSM 23526),通过上载3空隙体积的细胞,然后用胶结液(钙/尿素)成功地原位浓缩。砂岩的UCS为1200 kPa,通过三次细胞和胶结液的应用形成,而不会堵塞空隙,从而形成渗透性固结砂芯。固结砂岩的ESEM图像、EDS和XRD分析显示,方解石晶体的纳米颗粒在纳米尺度上形成了非常细的颗粒聚集体,在砂粒之间形成了点对点接触。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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