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

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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Publication Details

Journal
Journal of Geophysical Research Solid Earth
Published
2026-09-30
DOI
https://doi.org/10.1029/2026jb034544
Primary Topic
Calcium Carbonate Crystallization and Inhibition
Type
article
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article

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

Bate Bate, Chi Zhang, Yi-Xin Yang, Sheng Zhou et al.
Journal of Geophysical Research Solid Earth
Calcium Carbonate Crystallization and Inhibition
article

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

Bate Bate, Chi Zhang, Yi-Xin Yang, Sheng Zhou, Yun‐Ming Chen, Ke‐Xin Chen, Lin‐Han Wang, Long‐Long Meng
article en

Abstract

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.

Journal of Geophysical Research Solid EarthVol. 131(10)
University of Vienna (AT), Zhejiang University (CN)
Life in Land
Openalex Percentile: Top 23%
Calcium Carbonate Crystallization and Inhibition
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