Oscar, Ron et. al.,

*Oscar;* Thanks for bringing the paper to the table. Biodiesel does not 
contain sulfur and it would be convenient, on a number of levels, if the 
shipping industry would convert to marine based biodiesel ASAP.





*Ken/Ron,* (Ref: 
https://groups.google.com/d/msg/geoengineering/nncNYX7jS2U/kbQ7cT1cK4sJ); 
Does the term: "*through environmental mechanisms other than an intended 
reduction of excess anthropogenic aerosol or greenhouse gas 
concentrations." *mean that projects which are primarily CDR and CCS 
efforts are *non*-geoengineering projects? How would carbon negative 
biofuels be classified under Ken's definition? Also, relativistic terms and 
words, such as "*de minimis" or "scope" *seem to require further 
clarification. Size/Scope or Minimum/Maximum quantifiers can be highly 
subjective without pre-determined qualifying limits. Clarity on these 
points would be useful.






*Dr. Calvin,* (Ref: 
https://groups.google.com/d/msg/geoengineering/fm_mh_lUtlU/qnfRjye1JP0J); 
Your push/pull concept, and the need for a project to meet the *"Big, 
Quick, and Surefire Test", *can accomidate biochar/carbon negitive biofuel 
production. The processing of the biomass can keep up with any biomass 
production method as long as the cultivation is within bioreactors. Open 
water algae blooms have largely been rejected as being un-acceptable, thus 
the use of photobioreactors are the only option for large scale microalgal 
biomass production. The potential "out-year effect" (long term CO2 
sequestration activity of biochar/olivine/organic fertilizer etc) of algal 
biomass based soil amendments multiplies the CDR/CCS effects of straight 
algal/sequestration (push/pull) by at least one factor. In short, the 
carbon negative biofuel regiment maximizes the market/environmental 
potential of the biomass, can pay for itself and needs no further basic 
research level developments. It can be "*plug-n-play*".








Best,







Michael






On Wednesday, February 12, 2014 1:00:24 PM UTC-8, Oscar Escobar wrote:
>
> Strong acids formed from shipping emissions can produce seasonal ‘hot 
> spots’ of 
> ocean acidification, a recent study finds. These hot spots, in ocean areas 
> close to 
> busy shipping lanes, could have negative effects on local marine ecology 
> and 
> commercially farmed seafood species. 
>   
> Shipping emissions can lead to high local 
> ocean acidification 
>  
> Oceans have become more acidic since pre-industrial times. The average 
> global ocean pH – 
> which decreases with increasing acidity – has dropped by 0.1 because the 
> seas have 
> absorbed 30-40% of manmade CO2. However, it is not only CO2 that can 
> acidify oceans. 
> Shipping emissions, a significant source of atmospheric pollution, 
> annually release around 
> 9.5 million metric tons of sulphur and 16.2 million metric tons of nitric 
> oxides. 
>  
> When dissolved in seawater, these pollutants are converted into the strong 
> sulphuric and 
> nitric acids, adding to ocean acidification. Increasing acidity poses a 
> threat to marine 
> ecosystems, harming species such as coral and algae, as well as commercial 
> aquaculture 
> species, such as shellfish. 
>  
> The researchers used state of the art computer modelling techniques and 
> datasets to create 
> a high resolution simulation of global shipping emissions’ effects on 
> ocean acidity. The 
> simulation calculated the acidifying impacts of shipping sulphur and 
> nitric oxide emissions on 
> a month by month basis, over one year. In addition to shipping-related 
> influences on acidity, 
> the model also included many physical and environmental factors, such as 
> ocean surface 
> water mixing and atmospheric effects. 
>  
> The results agreed with previous studies of the average annual ocean 
> acidification, but, 
> importantly, revealed significant differences between regions and seasons. 
> Ocean 
> acidification was highest in the northern hemisphere, occurring in ‘hot 
> spots’ close to coastal 
> areas and busy shipping lanes during the summer months. These ‘hot spots’ 
> coincide with 
> peak activity of some biological processes, such as plankton blooms and 
> fish hatching, 
> where they may cause greater harm. On a local scale, the acidification – a 
> pH drop of 
> 0.0015-0.0020 – was equal to CO2’s global annual acidifying effects. 
>  
> The model did not include some coastal ocean areas, such as the 
> Mediterranean Sea, as 
> there were limitations in the oceanographic atlases used. However, 
> acidification is likely to 
> be high in these areas given the heavy shipping traffic from ports. 
>  
> International regulation is in place to reduce shipping atmospheric 
> sulphur emissions 
> through the International Maritime Organization’s Emission Control Areas 
> (ECA), which are 
> in force in four ocean areas, including the Baltic and North Seas. One 
> technology commonly 
> used to achieve ECA targets is ‘seawater scrubbing’, where exhaust 
> pollutants are removed 
> using seawater. 
>  
> This study drew on data from 2000 and 2002, prior to the enforcement of 
> ECAs. However, 
> the researchers note that seawater scrubbing, without additional steps to 
> neutralise the 
> acids that it produces, causes acidification in regions where biodiversity 
> or commercial 
> aquaculture may be most negatively affected. These previously overlooked 
> sources of ocean 
> acidification and policy impacts could be used to inform future 
> discussions of controls 
> relating to shipping emissions or ocean acidification
>
> The study:
>
> *Shipping contributes to ocean acidification*
> Ida-Maja Hassellöv et al DOI: 10.1002/grl.50521
> http://onlinelibrary.wiley.com/doi/10.1002/grl.50521/full
> http://onlinelibrary.wiley.com/doi/10.1002/grl.50521/abstract
>
> Abstract
>
> [1] The potential effect on surface water pH of emissions of SO*X* and NO
> *X* from global ship routes is assessed. The results indicate that 
> regional pH reductions of the same order of magnitude as the CO2-driven 
> acidification can occur in heavily trafficked waters. These findings have 
> important consequences for ocean chemistry, since the sulfuric and nitric 
> acids formed are strong acids in contrast to the weak carbonic acid formed 
> by dissolution of CO2. Our results also provide background for discussion 
> of expanded controls to mitigate acidification due to these shipping 
> emissions.
>
>

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