微生物诱导碳酸钙沉淀封存的高渗透性砂岩渗透性的应力敏感性

Chenpeng Song , Derek Elsworth
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引用次数: 0

摘要

巴氏杆菌催化的微生物诱导碳酸盐沉淀(MICP)作为一种既能加固又能密封土工材料的生物水泥引起了广泛关注。我们研究了最初高渗透性的贝里亚砂岩(初始渗透性∼110 mD)在不同持续时间的 MICP 灌浆处理下渗透性降低的应力敏感性。结果表明,与灌浆前相比,经过 2、4、6、8 和 10 个周期的 MICP 灌浆后,渗透率分别下降了 87.9%、60.9%、38.8%、17.3% 和 5.4%。随着 MICP 灌浆时间的延长,渗透率对应力变化的敏感性逐渐降低,滞后性减弱。渗透率的这种应力敏感性很好地体现了一种幂律关系,其系数代表了三个不同的阶段:最初是缓慢降低,随后是快速下降,最后是渐近响应。这种变化行为与石英骨架的运动和位错密切相关,而石英骨架的运动和位错又受晶间生物咬合强度的控制。扫描电子显微镜(SEM)成像揭示了 MICP 灌浆后与微结构演变相关的应力敏感性对渗透性的演变。最初的 CaCO3 沉淀物分散在石英框架表面,占据了孔隙空间,这在控制和减少颗粒间位移方面最初是有限的。随着沉淀物的不断积累,粒间槽形孔隙最初由生物 CaCO3 粘结,随着生物固结体积的扩大,粘结强度逐渐增强。在这一阶段,压实引起的晶间移动和位错减少,渗透率的应力敏感性显著降低。随着这些槽形孔隙逐渐被生物水泥填满,压实引起的移动和错位变得可以忽略不计,从而使渗透性的应力敏感性降到最低。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Stress sensitivity of permeability in high-permeability sandstone sealed with microbially-induced calcium carbonate precipitation

Microbially induced carbonate precipitation (MICP) catalyzed by S. pasteurii has attracted considerable attention as a bio-cement that can both strengthen and seal geomaterials. We investigate the stress sensitivity of permeability reduction for the initially high-permeability Berea sandstone (initial permeability ∼110 mD) under various durations of MICP-grouting treatment. The results indicate that after 2, 4, 6, 8 and 10 cycles of MICP-grouting, the permeabilities decrease incrementally by 87.9%, 60.9%, 38.8%, 17.3%, and then 5.4% compared to the pre-grouting condition. With increasing the duration of MICP-grouting, the sensitivity of permeability to changes in stress gradually decreases and becomes less hysteretic. This stress sensitivity of permeability is well represented by a power-law relationship with the coefficients representing three contrasting phases: an initial slow reduction, followed by a rapid drop, culminating in an asymptotic response. This variation behavior is closely related to the movement and dislocation of the quartz framework, which is controlled by the intergranular bio-cementation strength. Imaging by scanning electron microscopy (SEM) reveals the evolution of the stress sensitivity to permeability associated with the evolving microstructures after MICP-grouting. The initial precipitates of CaCO3 are dispersed on the surfaces of the quartz framework and occupy the pore space, which is initially limited in controlling and reducing the displacement between particles. As the precipitates continuously accumulate, the intergranular slot-shaped pore spaces are initially bonded by bio-CaCO3, with the bonding strength progressively enhanced with the expanding volume of bio-cementation. At this stage, the intergranular movement and dislocation caused by compaction are reduced, and the stress sensitivity of the permeability is significantly reduced. As these slot-shaped pore spaces are progressively filled by the bio-cement, the movement and dislocation caused by compaction become negligible and thus the stress sensitivity of permeability is minimized.

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