ABSTRACT:The past year has been one of continued high productivity and technical innovation for research conducted under support of this contract. We report here on the successful completion of development of a deep-ocean laser Raman spectrometer, and the use of this novel system for direct in situ measurement of the dissolution rate of CO 2 from a N 2 /CO 2 gas mixture at 300m ocean depth. We have carried out the deepest ever ocean CO 2 injection experiment at 3960m depth, and have observed the behavior of the plume of low pH/high CO 2 water emanating from this source. This was made possible by the design, construction, and operation of a novel flume to contain the liquid CO 2 and to force flow in a controlled manner over the liquid CO 2 surface. In carrying out this experiment we observed for the first time the extraordinarily rapid hydration kinetics of CO 2 with water at high pressure. This initial observation was later confirmed in a carefully controlled series of acid and CO 2 injection studies at varying depths. In carrying out this research we are aware of the environmental concerns, and we have been in the forefront of identifying the challenges resulting from the far greater quantities of CO 2 being passively absorbed from the atmosphere. This quantity now is approximately 1 million metric tons CO 2 per hour, and reasonable projections for the 21 st century project ocean pH changes of 0.3 or more by mid-century. The PIs have played a key role in organizing a major international meeting on this topic, and on reporting the results. We are now engaged in developing the novel techniques required to investigate this problem.
INTRODUCTIONThe primary mechanism preventing very fast accumulation of CO 2 in the atmosphere is ocean absorption through the sea surface. This absorption, driven by the accumulated mean pCO 2 difference between air and sea, now proceeds at a rate of about 1 million metric tons CO 2 per hour. Thus ocean passive "disposal" of fossil fuel CO 2 is the primary greenhouse gas control technique used by all nations at all times, and the accumulated oceanic fossil fuel burden is now ≅ 500 billion tons CO 2 . In the few years that CO 2 is resident in the atmosphere it affects the planetary radiation balance and contributes to global warming. Thus some 25 years ago it was first suggested that direct injection of CO 2 into the deep ocean, thus bypassing the atmospheric disposal step with its attendant global warming, would be a useful greenhouse gas control technology. We have investigated this process in a series of studies carried out in part through the support of this award. These have involved creation of advanced experimental techniques for injection of CO 2 into the deep ocean, the measurement of the fate and behavior of the injected liquid, the formation and dissolution of a solid hydrate, and the environmental consequences of both direct and indirect CO 2 injection into the ocean.
EXECUTIVE SUMMARYIn this report we detail research carried out in the period October 1, 2003 through Septemb...