Calcium Carbonate Precipitation Visualization on a Lab‐on‐a‐Chip Model With Spectral Induced Polarization Monitoring

电导率 材料科学 碳酸钙 碳酸盐 极化(电化学) 降水 分析化学(期刊) 球霰石 均质化(气候) 矿物学 化学物理 粒径 化学工程 方解石 电阻率和电导率 化学 Crystal(编程语言) 气溶胶
作者
Bate Bate,Lin‐Han Wang,Yi-Xin Yang,Ke‐Xin Chen,Long‐Long Meng,Chi Zhang,Yun‐Ming Chen,Sheng Zhou
出处
期刊:Journal Of Geophysical Research: Solid Earth [Wiley]
卷期号:131 (10)
标识
DOI:10.1029/2026jb034544
摘要

Abstract Calcium carbonate (CaCO 3 ) is ubiquitous in natural and engineering processes. Its dynamic morphological evolution is critical in geological carbon sequestration, environmental remediation, and geomaterial strengthening, but remains insufficiently visualized and monitored at the particle scale. In this study, a microfluidic model with a 20× optical objective lens was developed to visualize the dynamic growth process of inorganically generated CaCO 3 crystals. Complementary spectral induced polarization measurements were carried out to monitor the content and morphology of CaCO 3 crystals. Dispersed CaCO 3 precipitates formed during the early stage, and the mean crystal size increased to 3.4 μm at 2.0 PV. Afterward, precipitates accumulated, especially at the interface between Na 2 CO 3 and CaCl 2 solutions, while the morphology and size of the individual crystals were masked by the accumulation. The measured imaginary conductivity increased monotonically as the amount of the dispersed precipitates increased until 2.0 PV, and then declined as clusters formed. When dispersed precipitates dominated before 2.0 PV, normalized chargeability was more strongly correlated with CaCO 3 volumetric content than with estimated specific surface area, because volumetric content provided a more robust indicator of the abundance of polarizable material, while conductivity normalization reduced the influence of pore‐fluid conductivity on the measured polarization magnitude. Relaxation time followed the Schwartz relationship for discrete precipitates but deviated once aggregates and the precipitation band formed because their visible dimensions no longer represented the effective polarization length scale. These observations provide particle‐scale evidence for the dynamic evolution of CaCO 3 precipitation and clarify the applicability of SIP‐based characterization.
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