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Mass Confusion About Air-Water Mass Transfer Damon Turney Bren School of Environmental Science and Management Committee Members: Jeff Dozier, Sanjoy Banerjee, Sally MacIntyre, Jordan Clark. Fate and Transport - Carbon Toxins (DDT, Hg, Dieldrin, PCBs, many more)
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Mass Confusion About Air-Water Mass Transfer Damon Turney Bren School of Environmental Science and Management Committee Members: Jeff Dozier, Sanjoy Banerjee, Sally MacIntyre, Jordan Clark
Fate and Transport • - Carbon • Toxins (DDT, Hg, Dieldrin, PCBs, many more) • Aeration of Hypoxic Water • DeAeration of Water Below Dam Spillways • Industrial Cleaning of Water in Air Spargers • Bioreactors and Other Reactors in Industry • Steam Condensation in Power Plants
from Kelly 1997 from Wanninkhof et al. 1992 from Rosso 2006
advection diffusion
advection diffusion
Advection into the water is not possible Air Water
Advection into the water is not possible Air Diffusion Water
Diffusion is ~10-5 m2/s Advection into the water is not possible Air Diffusion Water Diffusion is ~10-9 m2/s
Air Water
Surface Renewal Theory No unambiguous way of determining a value for average t
Surface Divergence Theory 100 μm
How do we visualize (or measure) the velocities in the top ~100 microns of the water column accurately?
Surface Divergence Theory from Turney et al. 2005 from McKenna & McGillis 2004
Surface Divergence Theory from Turney et al. 2005 from Xu et al. 2006
Experimental Conditions No Wind, Channel Flow (Straight Channelized River) 4 water heights 3 water velocities Reynolds numbers ranging from 5000 to 30,000 Wind Waves, Microscale Wave Breaking 10 wind speeds fetch constant ~9 meters
Measurements No Wind, Channel Flow - Mean Velocity, Depth, Temperature, - PIV Turbulence in Middle of Water Column - Friction of Water on Channel Bottom - PIV of Surface Divergence Motions - Oxygen Transfer Measurements Wind Waves - Mean Velocity, Depth, Temperature, - PIV Turbulence in Middle of Water Column - Friction of Water on Channel Bottom - Wind Speeds (~1mm apart) at Locations Above Interface - Friction of Wind on Air-Water Interface - Stereo PIV of Surface Divergence Motions - Oxygen Transfer Measurements - Standard Water Height Measurements and Shadowgraphs
k 10-5 (cm/s) u* (cm/s)
k=3.3 x 10-5 m/s F=3.3 x 10-5 ΔC
Conclusions: • It’s possible that the Surface Divergence Models is too simple, i.e., it ignores organized flows such as waves. Perhaps it is time for a new theory. • Time-history effects are necessary for an adequate understanding of how the chemical is transported away from the interface. • Accurate knowledge of velocity near the interface is very valuable. These measurement techniques should be pushed forward.
from Sabine et al. 2004 Pg C: 3.2 (+/-0.2) = 6.3 (+/-0.4) + 2.2(+/-1.3) - 2.4(+/-1.2) – 2.9 atmosphere fossil fuel terrestrial oceanic error from Woods Hole Website