The recent oil spill in the Gulf of Mexico is a catastrophe whose consequences will be felt for years to come. Prince William Sound, Alaska, still shows the presence of oil from the Valdez oil spill in 1989. Nevertheless, my intent in this blog entry is not to castigate the parties responsible for it or to lament the damage to the environment, but rather to discuss the chemistry that led to the initial explosion and subsequent tragedy. The problems began on 10 PM on April 20 when a surge of gas (apparently CH4) and oil shot up the drill pipe. Much mention has been made of hydrates, which seem to have contributed to this initial surge and which have subsequently impeded several attempts to cap the well.

Molecular model of gas hydrate, from Leibniz Institut fuer Meereswissenschaften
Hydrates (as explained by the Leibniz Institut fuer Meereswissenschaften) are “non-stoichiometric compounds. Water molecules form cage-like structures in which gas molecules are enclosed as guest molecules” (see image). These structures occur naturally in many deep ocean sites. Any number of gases can be found in the lattice, but the one of interest here is methane, which is produced by “zymotic decomposition of organic components or by bacterial reduction of CO2 in sediments.” These are stable over a specific range of temperatures and pressures as described here, and shown in the image below. There is a limited zone of stability for the hydrates: they extist at high pressures and relatively low temperatures. The weight of the ocean induces a pressure of roughly 1 atm for every 10 meters. Temperature initially drops with ocean depth, but then increases beneath the sea floor. Once you get deep enough – and hot enough – the hydrates are no longer stable. Consequently, their occurrence is limited to a relatively narrow band beneath the ocean floor. The operation was taking place in 1500 m (5,000 ft) of water, and drilling to a depth of 5000 m (18,000 ft).

Stability diagram for gas hydrates in marine environment, from Leibniz Institut
As reported in the Financial Times energysource blog, “It has been suggested that they [hydrates] may have been responsible for the leakage of gas into the Deepwater Horizon’s drill riser…” Why did the gas appear then? The crew of Deepwater Horizon was in the process of capping off the well, which involves pumping concrete into the top to seal it (nice graphic of that process in the FT). It is known that this process can destabilize hydrates: a 2009 report by Halliburton, reported again in the FT’s energysource blog, warned that “gas flow may occur after a cement job in deep-water environments that contain major hydrate zones.” As the FT blog summarizes, gas might stop flowing from the hydrates in a few hours or days, or – if you’re unlucky – it might notstop. The chemistry of concrete is explained on this site maintained by WHD Microanalysis Consultants Ltd, who mention that the curing of concrete is an exothermic process, with the period of maximum heat evolution occurring typically between about 10 and 20 hours after mixing. I can’t help wondering whether heat released by the setting concrete can contribute to destabilization of the gas hydrates. Anybody got any thoughts on that?
Subsequently, gas hydrates played a role in hindering attempts to stop the flow of oil. Remember the 100-ton steel and concrete box they tried to move on top of the hole? As reported in the FT (again): ‘When gas leaks out [from the well], its pressure drops and it cools… In the presence of water, light hydrocarbon liquids can react with water to form a … hydrate. This happens quite often in gas pipelines, but the circumstances 5000 ft down on the sea bed … make this very difficult to control.‘ This says that the leak from the well is creating even more hydrates. The hydrates clogged the container and forced a halt to the operation.
Incidentally, methane hydrates would be a great source of energy. Unfortunately, that’s not a carbon-neutral process: there’s a tremendous amount of CO2 that would be released. Still, it’s really fascinating to see ice burn as the CH4 is released.
Fascinating chemistry. As a theoretical chemist, I’ve been thinking about how modeling could help. Modeling could predict (T,P) phase diagrams for CH4 in H2O lattices. Monte-Carlo simulations can predict loading curves for these structures, while molecular dynamics or DFT could predict thermodynamic and kinetic stability of the methane absorption. Ultimately, you’d like to be able to use such approaches to identify ways to stabilize these structures, or to destabilize them in a controlled manner: imagine pumping in a chemical that causes the CH4 to be released sloooowly. The advantage of computational methods, of course, is that models won’t blow up no matter how much pressure you apply to them or how much methane ‘escapes.’
Such a study might help prevent future tragedies, but the main focus of scientists & engineers now needs to be on the cleanup. More on that in a future blog.