THE EFFECT OF RAIN ON INTERTIDAL ESTUARINE SEDIMENT TRANSPORT (VORTEX RINGS, OXYGENATION, DROP/SPLASH FEATURES, FECAL PELLETS)

<p>Storms are important aperiodic events, which intensify erosional processes over short time periods. The effect of rain on the shallow intertidal water column was the focus of this study. The literature was extensively reviewed to identify parallel research in other scientific disciplines, which could be used to understand how raindrops may be acting as a sediment resuspension mechanism. Single-drop and multi-drop laboratory studies were conducted on the initiation of motion of sediment. Results indicate single vortex rings in a quiescent environment can initiate motion of sand-sized noncohesive sediment in all water depths tested, up to and including 22.5 cm. Multidrop experiments (with estuarine muds) indicated that rain can resuspend cohesive sediment at an average rate of 2.8 gm/m('2)/hr in water depths to 8 cm. Insitu experiments were conducted to compare the magnitude of rain resuspension with wind wave and boat wake effects. Rain effects were observed in water depths less than 7 cm. In these water depths wind effects were decreasing, because the shallow water dampened out the larger waves. Observations during two storms illustrated the problem of isolating rain resuspension from wind wave resuspension.</p><p>The ability of drops to form vortex rings was utilized in a mixing test of aquaculture tanks used in toxicity testing. Drop-formed vortex rings were more effective in oxygenating the tanks than air bubbling at the strengths typically used for the tests.</p>

Name thesis:degree_name

Doctor of Philosophy

Level thesis:degree_level

Dissertation

Year

1986

Author dc:creator

• SHEVENELL, THOMAS CORTLAND

• Geology

Repository record dc:identifier

https://scholars.unh.edu/dissertation/1485

OAI identifier oai:identifier

oai:scholars.unh.edu:dissertation-2484