The  reflecivity gain  reported in *Royal Society of Chemistry Advances* is 
quite phenomenal-- about 10 times the albedo of still water, and the bubble 
lifetime is two orders of magnitude greater than the longest-lived marine 
microbubbles  Johnson and Cooke noted in their 1981* Science *paper 

On Tuesday, March 17, 2015 at 9:27:55 PM UTC-4, andrewjlockley wrote:
>
> Poster's note : interesting concept, but major questions remain regarding 
> wave action, biodegradation, and the effect on marine life. 
>
> http://pubs.rsc.org/en/content/articlelanding/2014/ra/c4ra08714c
>
> Long-term stabilization of reflective foams in sea water
>
> Alex Aziz, Helen C. Hailes, John M. Ward and Julian R. G. Evans
> RSC Adv., 2014,4, 53028-53036 
> DOI: 10.1039/C4RA08714C
>
> Abstract
>
>  This work explores the challenge of making persistent foams in salt water 
> to provide high reflectance. While stable foam is essential in the food 
> industry and in fire fighting, this is the first work aimed at combining 
> foam persistence with reflectance. One application is the use of oceanic 
> foams to increase planetary albedo: extending foam lifetime moderates the 
> energy required to maintain large areas of ‘ocean mirror’. Two compositions 
> to produce such foams in seawater are described. The first is based on high 
> methyl ester pectin-type A gelatin complexes which produced foams with a 
> reflectance of 0.5. The second produces stable foams using cellulose ethers 
> and iota carrageenan gelling agents. These foams gelled in the presence of 
> sea water to give measured reflectance of 0.65–0.75. Both had lifetimes, 
> without wave action, beyond three months at which point the experiment 
> ended. In contrast, single protein species such as gelatin B, whey protein 
> isolate and albumin produced short-lived foams. Foam stability was measured 
> by recording liquid drainage and foam height as a function of time. In the 
> event that climate interventions are needed, such additives would be 
> appropriate for nutrient-deficient ocean regions that support low levels of 
> marine life.
>

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