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A Flow-through Exposure System for Evaluating Suspended Sediments Effects on Aquatic Life
Published on: January 9, 2017
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Methane Bubble Growth and Migration in Aquatic Sediments Observed by X-ray μCT
Liu Liu1, Tim De Kock2, Jeremy Wilkinson1
1Institute for Environmental Sciences, University of Koblenz-Landau , 76829 Landau, Germany.
Environmental Science & Technology
|January 30, 2018
Summary
Sediment properties control methane bubble formation and movement in aquatic environments. Low strength sediments allow large bubble growth and migration, while high strength sediments favor microbubbles and restricted movement.
Area of Science:
- Geochemistry
- Environmental Science
- Sedimentology
Background:
- Methane bubble dynamics are crucial for carbon cycling in aquatic sediments.
- Understanding the influence of sediment mechanics on bubble behavior is essential.
Purpose of the Study:
- To investigate how sediment mechanical properties affect methane bubble growth and transport.
- To characterize bubble formation and migration in clay and sand sediments.
Main Methods:
- Laboratory incubation experiment (20 days) with homogenized clay and sand.
- High-resolution characterization of methane bubble development using micro-computed tomography (μCT).
- Measurement of sediment shear yield strength and observation of bubble migration under reduced hydrostatic pressure.
Main Results:
- Microbubble formation dominated initially, followed by large bubble growth via sediment deformation, enhancing macropore connectivity.
- Large bubble growth (>1 mm) occurred in low shear strength sediments (<100 Pa).
- High shear strength sediments (>360 Pa) resulted in microbubble predominance.
- Bubble migration was enhanced in clay, while in sand, it was limited to the upper 6 cm.
- Macropore networks served as primary pathways for bubble movement and release.
Conclusions:
- Sediment mechanical properties, particularly shear yield strength, significantly control methane bubble size and transport.
- Macropore connectivity plays a critical role in methane release from aquatic sediments.
- The findings improve models of carbon cycling in freshwater systems.
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