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Insights into asphaltene aggregation in the Na-montmorillonite interlayer.
Xinzhe Zhu1, Daoyi Chen2, Guozhong Wu2
1Division of Ocean Science and Technology, Graduate School at Shenzhen, Tsinghua University, Shenzhen, 518055, China; School of Environment, Tsinghua University, Beijing, 100084, China.
Asphaltene diffusion in Na-montmorillonite (MMT) interlayers is faster in fresh water but significantly reduced by humic substances, impacting heavy oil transport in soils.
Area of Science:
- Environmental Science
- Geochemistry
- Materials Science
Background:
- Asphaltenes, heavy fractions of crude oil, pose environmental challenges due to their persistence.
- Understanding asphaltene behavior in geological formations like Na-montmorillonite (MMT) is crucial for remediation.
Purpose of the Study:
- To investigate the diffusion and aggregation of asphaltenes within MMT interlayers under varying conditions.
- To elucidate the influence of water saturation, salinity, interlayer space, and humic substances on asphaltene transport.
Main Methods:
- Molecular dynamic simulations were employed to determine molecular configuration, density profiles, diffusion coefficients, and aggregation intensity.
- Atomic force microscopy was used to characterize the 3D topography and particle size of asphaltene aggregates.
Main Results:
- Asphaltene diffusivity was significantly higher in fresh water compared to saline water (35‰), though salinity minimally affected aggregation.
- Reduced pore water content and MMT interlayer space markedly decreased asphaltene mobility.
- Humic substances led to co-aggregation and sequestration of asphaltenes, reducing diffusion by an order of magnitude and increasing aggregation by 33%.
Conclusions:
- Humic substances play a critical role in immobilizing asphaltenes within MMT interlayers.
- Findings provide insights into the fate and transport of heavy oil residues in contaminated soils, aiding environmental risk assessment.
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