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Role of Ripening in the Deposition of Fragments: The Case of Micro- and Nanoplastics
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Researchers used transparent two-dimensional porous media to directly observe how irregularly shaped micro- and nanoplastic fragments deposit and accumulate in soil-like environments. They found that a process called ripening, where previously deposited particles promote the capture of additional particles, plays a significant role in how plastic fragments are retained. The study provides new understanding of why real-world microplastic fragments behave differently than the uniform spherical particles typically used in laboratory experiments.
Particulate contaminants, such as microplastics (1 μm to 5 mm) and nanoplastics (<1 μm), are disseminated in many terrestrial environments. However, it is still unclear how particles' properties drive their mobility through soils and aquifers due to (i) poor environmental relevance of the model particles that are studied (e.g., spherical and monodisperse) and (ii) the use of packed bed experiments which do not allow a direct observation of deposition dynamics. Using transparent 2D porous media, this study analyzes deposition dynamics of rough polystyrene fragments with irregular shapes and with a size continuum (≈10 nm to 5 μm). Using in situ and ex situ measurements, particle deposition as a function of size was monitored over time under repulsive conditions. In the absence of natural organic matter (NOM), micrometric particles rapidly deposit and promote the physical interception of smaller nanoparticles by creating local porous roughness or obstacles. In the presence of NOM, differences according to particle size were no longer observed, and all fragments were more prone to being re-entrained, thereby limiting the growth of deposits. This work demonstrates the importance of pore surface roughness and porosity of the pore surface for the deposition of colloidal particles, such as microplastics and nanoplastics, under repulsive conditions.
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Researchers compared the transport, deposition, and re-entrainment behavior of microplastic particles versus natural mineral particles in porous media, finding key differences driven by density, surface charge, and shape that affect how microplastics migrate through soils and sediments.
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Real-time pore-scale visualization using a microscope-coupled flow cell was used to track how fragmented microplastics move and deposit in saturated and unsaturated porous media, revealing distinct transport and retention patterns depending on water saturation conditions. The findings improve mechanistic understanding of how microplastics migrate through soils toward groundwater.
Real-Time Visualization of Infiltration and Retention of Microplastics with Different Shapes in Porous Media
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Researchers used an improved refractive index matching method to visualize in real time how microplastics of different shapes infiltrate and become retained in porous media under water flow. They found that spherical microplastics penetrated deepest with the most vertical trajectories, while cylindrical and flaky particles showed more lateral movement and frequent deceleration. The study reveals how microplastic shape significantly influences their transport behavior in soil-like environments.
The Re-distribution of Pristine and Aged Microplastics (<50 µm) in Soil Aggregate Fractions
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Researchers investigated how pristine and aged microplastics smaller than 50 micrometers redistribute among soil aggregate fractions during aggregation in two soil textures amended with organic matter, finding that aggregate formation actively partitions microplastics in ways influenced by soil texture and particle aging.
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Pore-scale imaging and experiments revealed how microplastic fibers move through and get retained in soil and sediment pores, showing that fiber shape and size strongly influence transport distance and accumulation zones. Understanding these dynamics is key to predicting where microplastics accumulate in terrestrial and subsurface environments.
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