Hello,

Some desert areas, notably near the southern Mediterranean coast, are indeed 
below sea-level. Letting sea water flow towards them is a rather old idea which 
has various rationales: triggering economical development, producing 
hydroelectric renewable energy, etc. Increasing water evaporation for 
geoengineering purposes is a new one. I'd like to emphasize a fourth one: 
producing very large quantities of renewable energy thanks to salt gradients.

This is because these sub-sea-level areas have already been flooded, in 
geological times, so that salt has accumulated there (they're called evaporites 
- others are located in the Danakil desert, also below sea-level, in eastern 
Eritrea and Ethiopia). As the reverse of sea water desalination, letting very 
concentrated brine (which can be produced by salt dissolution into sea water) 
and usually concentrated sea water melt with each other can produce renewable 
energy. See: http://en.wikipedia.org/wiki/Blue_energy

One technology (pressure retarded osmosis) is being developed by Norwegian 
society Statkraft:
http://www.statkraft.com/Images/Statkraft%20Osmotic%20Power_tcm4-5362.pdf. It 
uses the same osmosis membranes that are currently used for water desalination, 
however, for price competitiveness, further cost reductions should come from 
scale economies.

The other technology (reverse electro dialysis) is developed by Dutch Redstack: 
http://www.redstack.nl/RS-Pres01/RS-pres_bestanden/frame.htm

Both are mainly developed in order to yield the salinity gradient between fresh 
water and sea water, but, as they also notice, the gradient between seawater 
and saturated brine is one order of magnitude greater, so that exploiting 
evaporites would be a huge quasi-renewable energy source. They are also 
interested in salt gradient conversion when the "sea water to Dead Sea" Project 
is to be realized.

With Renaud de Richter, I am currently writing a book (in French) which will 
probably be named "20 energies renouvelables insolites" (20 unusual renewable 
energies). Salinity gradients will be the first of our 20 chapters.

Best regards,

Denis Bonnelle
[email protected]<mailto:[email protected]>




De : [email protected] [mailto:[email protected]] 
De la part de Ken Caldeira
Envoyé : dimanche 7 juin 2009 22:27
À : geoengineering
Cc : Johnnie Buttram
Objet : [geo] Flooding below sea-level: Siphonics Natural Engineering (c)

Folks,

I ran across this pdf recommending the benefits of flooding sub sea-level 
desert areas.

I believe the author of this document (cc'd) would enjoy your comments.

Best,

Ken


___________________________________________________
Ken Caldeira

Carnegie Institution Dept of Global Ecology
260 Panama Street, Stanford, CA 94305 USA

[email protected]<mailto:[email protected]>; 
[email protected]<mailto:[email protected]>
http://dge.stanford.edu/DGE/CIWDGE/labs/caldeiralab
+1 650 704 7212; fax: +1 650 462 5968




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