Volume Pulsation of Small Gas Bubbles in the Surface Layer of Coastal Sands Caused by Surface Gravity Waves

In the uppermost millimeters of shallow submerged coastal sediments, photosynthesis by microalgae and cyanobacteria during daylight hours can cause oxygen supersaturation of sediment porewater, leading to bubble formation. In shallow water depths, the seabed is affected by the pressure m...

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Bibliographic Details
Other Authors: Russell, Lee (authoraut)
Format: Others
Language:English
English
Published: Florida State University
Subjects:
Online Access:http://purl.flvc.org/fsu/fd/FSU_2015fall_Russell_fsu_0071E_12931