{"title":"Calcium Carbonate Precipitation Visualization on a Lab-on-a-Chip Model With Spectral Induced Polarization Monitoring","authors":"Bate Bate, Lin-Han Wang, Yi-Xin Yang, Ke-Xin Chen, Long-Long Meng, Chi Zhang, Yun-Ming Chen, Sheng Zhou","doi":"10.1029/2026JB034544","DOIUrl":null,"url":null,"abstract":"<p>Calcium carbonate (CaCO<sub>3</sub>) 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<sub>3</sub> crystals. Complementary spectral induced polarization measurements were carried out to monitor the content and morphology of CaCO<sub>3</sub> crystals. Dispersed CaCO<sub>3</sub> 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<sub>2</sub>CO<sub>3</sub> and CaCl<sub>2</sub> 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<sub>3</sub> 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<sub>3</sub> precipitation and clarify the applicability of SIP-based characterization.</p>","PeriodicalId":15864,"journal":{"name":"Journal of Geophysical Research: Solid Earth","volume":"131 10","pages":""},"PeriodicalIF":4.0000,"publicationDate":"2026-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geophysical Research: Solid Earth","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1029/2026JB034544","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
Calcium carbonate (CaCO3) 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 CaCO3 crystals. Complementary spectral induced polarization measurements were carried out to monitor the content and morphology of CaCO3 crystals. Dispersed CaCO3 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 Na2CO3 and CaCl2 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 CaCO3 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 CaCO3 precipitation and clarify the applicability of SIP-based characterization.
期刊介绍:
The Journal of Geophysical Research: Solid Earth serves as the premier publication for the breadth of solid Earth geophysics including (in alphabetical order): electromagnetic methods; exploration geophysics; geodesy and gravity; geodynamics, rheology, and plate kinematics; geomagnetism and paleomagnetism; hydrogeophysics; Instruments, techniques, and models; solid Earth interactions with the cryosphere, atmosphere, oceans, and climate; marine geology and geophysics; natural and anthropogenic hazards; near surface geophysics; petrology, geochemistry, and mineralogy; planet Earth physics and chemistry; rock mechanics and deformation; seismology; tectonophysics; and volcanology.
JGR: Solid Earth has long distinguished itself as the venue for publication of Research Articles backed solidly by data and as well as presenting theoretical and numerical developments with broad applications. Research Articles published in JGR: Solid Earth have had long-term impacts in their fields.
JGR: Solid Earth provides a venue for special issues and special themes based on conferences, workshops, and community initiatives. JGR: Solid Earth also publishes Commentaries on research and emerging trends in the field; these are commissioned by the editors, and suggestion are welcome.