Hi Folks,

This is a conceptual sketch on the use of a biological aerosol. It is a very 
raw concept, yet I found it an interesting thought.

*Tropospheric Injection of Micro Diatoms * 

*A Combined SRM/CCS Proposal with Long Term Implications for*

*Enhanced Hydrate Burial and General Ocean Acidification Mitigation*


 *A Brief Conceptual Sketch Offered to the Google Geoengineering Group*


 Diatoms are ubiquitous to the waters of this planet and they all have self 
regulating biological features which makes them ideal for GE use on a 
regional or global scale. It is estimated that there are approximately 2 
million species, yet only a fraction have been studied. This proposal does 
not call out for any particular species. I leave that determination to 
others. In general, they play an important role on many different levels. 
Diatoms offer O2 production, CO2 capture and sequestration along with long 
term hydrate burial. The potential for diatoms to produce biofuel is well 
known but that issue is outside of this proposal. 


 Through my discussions with M.V. Bhaskar, I have become aware that micro 
diatoms can be prepared in a dry form as a means to seed bodies of water to 
produce artificial diatom blooms for enhanced O2 saturation. This conceptual 
sketch proposes that this type of material be considered for atmospheric 
aerosol injection as a form of combined SRM/CCS/Enhanced Hydrate Burial and 
Ocean Acidification Mitigation.


 :A minimum of seven main technical issues concerning this type of 
biological aerosol medium can be anticipated.

 
   1. 
   
   *Will this form of aerosol stay suspended for a reasonable time?* The 
   size of micro diatoms are such that proper dispersal could produce an 
   aerosol which would stay suspended for a significantly reasonable periods of 
   time. The engineering of the dispersal method is similar to previous aerosol 
   concepts. The suspension time will depend on many factors ranging from 
   altitude of injection, latitude of injection (atmospheric cell 
   characteristics) and general tropospheric weather conditions. The rate (if 
   any) of atmospheric moisture absorption needs further understanding. If it 
   is found that this medium does absorb atmospheric moisture, this could 
   represent a means to reduce that primary green house gas, as well as, 
   possibly providing a means for cloud nucleation/brightening. 
   
   2. 
   
   *Will the diatom aerosol reflect SR?* Typically, this diatom preparation 
   is brown. I believe it may be possible that the diatom material can be 
   engineered to be reflective. This might be done through laminating the dried 
   preparation with biologically neutral reflective material (white powdered 
   sugar?). Finding the right laminating material which does not substantially 
   degrade suspension time, seed viability or produce accumulated environmental 
   adverse effects will need investigating along with the associated high 
   volume production needs. 
   
    3. 
   
   *Will the diatom material remain viable through the aerosol phase into 
   the aquatic environment?* Tropospheric injection avoids the higher 
   altitude environmental stress issues. Such as, high UV, low ambient pressure 
   and extreme low temperatures, which may effect seed viability. However, the 
   possibility of laminating the material to address the high altitude concerns 
   may also be possible in the future and will need further investigation. The 
   added complications, relative to seed survival, of stratospheric injection 
   indicates that tropospheric injection should be the initial deployment 
   consideration. Stratospheric injection may be avoided if coordinated and 
   tailored regional tropospheric efforts can be developed.
   
   4. 
   
   *Will this method address arctic ocean methane release?* ESAS based 
   tropospheric injection of this medium can have three significant benefits. 
   The first is the immediate SRM benefit (with proper seed lamination, 
   possible cloud nucleation/brightening). Second is the potential enhanced 
   dissolved methane oxidation rate. Third is the enhanced wide area increase 
   in the sediment build up rate over the shallow water hydrate fields.. The 
   ESAS is at a critical edge of the GHSZ envelope. A rapid build up of diatom 
   debris could expand the envelope significantly with just one added meter of 
   diatom sediment ooze (insulation against warming waters, as well as, 
   decreasing the porosity of the existing sediment). That will obviously take 
   a few years to achieve. However, no other practical means to achieve this 
   needed large area effect seems available. Also, can the resident AOM adapt 
   to a marked increase in diatom rain? 
   
    5. 
   
   *Will this method address tundra methane release?* Not completely, 
   however this method could seed even the smallest body of standing water 
   within a tundra region and thus provide added O2 saturation and the 
   associated methane oxidation. As the tundra continues to warm, more standing 
   water will emerge and thus this potential enhanced oxidation will become 
   more important.
   
   6. 
   
   *Will this method have a meaningful/measurable effect on ocean pH levels?
   * Diatoms consume dissolved CO2 and thus it is a matter of scale. There 
   is a need to determine the seed mass ratio to the total CO2 consumption that 
   can be attributed to that seed mass. This will determine the cost 
   effectiveness/scalability *of this aspect* of the concept. The current 
   use of this diatom seed material does not take into account the aerosol 
   phase being proposed. Seed survival rates during the aerosol phase might be 
   determined through table top experiments, yet field test would be needed to 
   verify any lab data. *Field trials for this overall concept should not 
   trigger significant protests as the diatom species which will be used pose 
   no known toxic hazards and are widely considered to be ecologically 
   beneficial.*
   
   7. 
   
   *Will this method be financially competitive with other aerosol concepts?
   * The cost of diatom medium preparation and injection can be expected to 
   be somewhat greater than sulfate/aluminum aerosols. This is due to the 
   potential beneficial aspects of this biological medium after precipitation. 
   The more material used, the greater the overall beneficial effect. That 
   aspect represents a principal departure from that of the prior art. The 
   prior methods seek to minimize cost through use of long lasting aerosols 
   (which have no secondary environmental benefit). The less aerosol used, the 
   less cost (and less potential adverse effects). This proposed method 
   represents a means which generates second and third order ecological 
   benefits once the aerosol precipitates. The added cost of the expected large 
   volume of material to be used should be justifiable due to these important 
   interrelated secondary benefits. This is not just a mitigation effort, it is 
   potentially also a general regional ecological enhancement.
   
 *This GE approach offers at least two *non* global warming mitigation 
related benefits to society. *First would be the overall water quality 
improvement in the operational area due to the increase in saturated O2 
levels provided by the seeded diatom blooms. Second would be that fisheries 
may improve due to the increase in the marine food production rates at the 
micro level. If only those two ancillary, yet fundamentally important 
benefits, can be proven, the debate surrounding GE can be expected to take a 
new direction. 


 *Note:* If this proposal finds any acceptance, M.V. Bhaskar deserves ample 
credit. I have simply tried to craft his input into conventional GE terms. 
If it finds no acceptance, I take full credit. 

Michael Hayes 6/21/11          

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