- Location
- Washington Heights, NY
I was involved in a discussion about a week ago I found very interesting. A guy on RC posted a research paper that looked at the best type of flow for corals with actually video evidence. Probably not a big surprise to people but they found oscillating waves with shorter periods improved mass transfer. The paper explains that mass transfer rate is "the rate at which coral transfer nutrients, remove wastes, and exchange gas".
http://www.aslo.org/lo/toc/vol_51/issue_2/1134a1.html
Paper in pdf
http://www.stanford.edu/~vittorio/Reidenbachetal2006.pdf
Nice video of research<a href=showthread.php?s=&postid=10854003#post10854003 target=_blank>Originally posted</a> by MCsaxmaster
The abstract:
Rates of mass transfer in coral reefs are governed both by the physical flow environment and the morphology of the coral. Laboratory experiments were conducted to estimate mass transfer in unidirectional and oscillatory flows by measuring the rate of dissolution of gypsum cylinders (clods) placed within the branching structure of three morphologically distinct coral species. Unidirectional flows were varied between 2.9 and 14.1 cm s21 and, as expected, mass transfer rates increased with increasing flow and a more open branch spacing. Depending on morphology and flow, mass transfer rates within the interior of the branching structure were 50 to 75% of that measured outside the coral in free-stream conditions. Oscillatory conditions showed relative mass transfer rates 1.6 to 2.9 times greater than equivalent unidirectional currents. This ratio increased with increasing wave frequency, likely due to the corresponding decrease in the diffusive boundary layer thickness. The ratio also increased with a greater compactness in branch spacing, with mass transfer rates within the coral structure up to 130% of free-stream conditions. We used planar laser-induced fluorescence imaging to study the instantaneous structure of mass advection through the coral. Oscillatory flow acts as a dominant forcing mechanism to generate water motion within the coral structure at levels not attainable with comparable unidirectional currents.
From the discussion:
"For all the corals, the increase in relative mass transfer ranges between a factor of 1.6 for a T=5s wave period to
2.9 for a T=1s wave period. The increase for the free stream control under waves versus unidirectional currents was 1.3 to 1.4, though no statistical relation to wave period was found. This 30% to 40% increase in mass transfer under waves is the same as that found in field observations by Falter et al. (2005)."
So, the difference in mass transfer for the study corals between unidirectional and oscillatory flow was a factor of 1.6 - 2.9 depending on wave periodicity. For free gypsum blocks the factor was 1.3 - 1.4 without an obvious pattern due to wave periodicity.
Best,
Chris
http://www.aslo.org/lo/toc/vol_51/issue_2/1134a1.html
Paper in pdf
http://www.stanford.edu/~vittorio/Reidenbachetal2006.pdf