干湿循环作用下eicp增强海砂的力学性能及崩解行为

Kai Xu , Ming Huang , Zijian Liu , Mingjuan Cui , Shuang Li
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引用次数: 1

摘要

酶诱导碳酸盐沉淀(EICP)在各种岩土工程应用中都很有前景,并被认为是传统水泥基材料地基改良方法的替代方案。然而,对EICP增强海砂在干湿循环下的力学性能和崩解行为的研究有限。本研究研究了EICP增强海砂在干湿循环影响下的力学性能和崩解行为。进行了单轴抗压强度(UCS)试验,讨论了干湿循环对EICP处理海砂力学性能的影响。在EICP处理的海砂上进行了崩解试验,以研究不同胶结水平的生物胶结样品的崩解阻力。对崩解前后样品的微观结构进行了检测,揭示了EICP增强海砂的崩解机理。D-W循环显著影响EICP增强海砂的力学性能,在经历15次D-W循环后,UCS降低了63.7%。胶结水平较低的试样在D-W处理的作用下,其抗崩解指数显著下降。胶结度较高的试样具有较高的抗崩解性,这可归因于试样内砂粒之间的接触点形成了更多结晶度较好的晶体。大豆壳脲酶形成的晶体主要是方解石,随着生物灌浆的深入,球形方解石的结晶度会逐渐转变为较大的菱形方解石。结晶度差的晶体易受D-W处理的影响,导致EICP增强海砂明显崩解。总之,本研究有望为EICP增强海砂的长期稳定性和干湿崩解机制提供有用的指导。
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Mechanical properties and disintegration behavior of EICP-reinforced sea sand subjected to drying-wetting cycles

Enzyme-induced carbonate precipitation (EICP) has emerged promising in various geotechnical applications, and has been presented as an alternative to the traditional cementitious materials-based ground improvement method. However, the study on mechanical properties and disintegration behavior of EICP-reinforced sea sand subjected to drying-wetting cycles are limited. This study investigated the mechanical properties and disintegration behavior of EICP-reinforced sea sand against the impact of drying-wetting (D-W) cycles. The uniaxial compressive strength (UCS) tests were performed to discuss the effect of drying-wetting cycles on the mechanical behavior of EICP-treated sea sand. The disintegration tests were conducted on EICP-treated sea sand to investigate the disintegration resistance of bio-cemented samples with various cementation levels. The microstructures of samples before and after disintegration were examined to disclose the disintegration mechanisms of EICP-reinforced sea sand. D-W cycles significantly affect the mechanical properties of EICP-reinforced sea sand, with UCS decreasing by 63.7% after undergoing 15 D-W cycles. The disintegration resistance index of specimens with a lower cementation level decreases significantly under the effect of D-W treatment. The higher disintegration resistance of specimens with higher cementation can be attributed to more crystals with better crystallinity formed in the contact point between sand particles within specimen. The crystals formed by soybean husk urease are mainly calcite and the crystallinity of spherical calcites would gradually change into larger rhombic calcite with further bio-grouting. The crystal with poor crystallinity is susceptible to the effect of D-W treatment, resulting in the obvious disintegration of EICP-reinforced sea sand. Overall, this study is expected to provide useful guidance on the long-term stability and drying-wetting disintegration mechanisms of EICP-reinforced sea sand.

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