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Seabed scars raise questions over carbon-storage plan

Unexpected fractures above the world’s biggest storage site could provide path for leaks.

At the Sleipner field in the North Sea, waste carbon dioxide is separated from natural gas and injected into a rock formation 800 metres below the seabed. Credit: Dag Myrestrand/Statoil

Like a porpoise on the prowl, the sleek submersible HUGIN tracks its prey with sonar chirps. But the hunter set loose in the waters of the North Sea is not pursuing fish — the robot is trawling for geological clues that could help to determine whether billions of tonnes of carbon dioxide can be stored below the sea floor for centuries, keeping it from warming the planet.

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Now, the latest data from the autonomous underwater vehicle and other tools deployed by the European Commission’s €10-million (US$13.8-million) ECO2 research project suggest that the plan might not be so simple. The seabed is fractured and scarred more than researchers had appreciated — providing potential routes for CO2 to leak from sub-seabed reservoirs where it is currently being stored. “We are saying it is very likely something will come out in the end,” says Klaus Wallmann, ECO2 coordinator and a marine geochemist at the GEOMAR Helmholtz Centre for Ocean Research in Kiel, Germany.

Such a conclusion could raise problems for the field of carbon capture and storage, especially in Europe, where any suggestion of leakage could reduce public support for the strategy. But ECO2 researchers say that evidence from oil-industry carbon-storage efforts already under way in the North Sea and Barents Sea suggests no hint of leakage, and that there would be little cause for concern even if there were. “We are very confident that if it were to occur, the rates would be low and the impact would be minimal,” says Wallmann, who presented the findings of the ECO2 team on 9 December at a meeting of the American Geophysical Union in San Francisco, California.

Oil companies have long injected CO2 into underground formations to enhance oil production, but the ECO2 project is studying sites where the gas is pumped below the sea floor to keep it out of the atmosphere. One of the biggest operations is in the Sleipner natural-gas field in the North Sea, run by the energy company Statoil, headquartered in Stavanger, Norway.

Since 1996, the company has separated CO2gas from the desired hydrocarbons and reinjected up to 1 million tonnes of CO2 a year into the Utsira formation, a layer of porous sandstone more than 800 metres below the sea floor (see ‘Gas tank’). The giantformation, which covers an area of 24,000 square kilometres, has the potential to hold 600 billion tonnes of disposed CO2. According to Statoil’s website, CO2 in the Utsira is safely contained under “gas-tight cap rock and cannot seep into the atmosphere”.

Credit: Jasiek Krzysztofiak/Nature

Although the company has rich data about the Utsira formation, less is known about the overlying sedimentary layers. ECO2 researchers have deployed HUGIN and other tools to fill in the details, using an advanced sonar system and a seismic profiler that sent strong acoustic pulses below the sea floor to reveal hidden geological structures.

The data reveal that the upper sedimentary layers hold many natural scars that might serve as conduits for CO2 release from the Utsira. At a site 25 kilometres north of the Sleipner injection well, HUGIN found a 3-kilometre-long fracture that is 10 metres wide in places, and runs 150–200 metres deep. Samples of fluids collected within the fracture suggest that methane and fresh water are leaking out from lower layers, says Karin Landschulze, a graduate student in geophysics at the University of Bergen, Norway.

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Leak impact

Because the fracture is so far from the injection site, the disposed CO2 is unlikely to reach it any time soon, say ECO2researchers: since 1996, the CO2 has spread in a plume and now reaches 3 kilometres north of the injection well. But finding such a large and unexpected fracture in the region raises questions, says Wallmann. “We don’t know how it formed, when it formed, and why it formed,” he says.

The researchers also discovered smaller vertical features, which they call chimneys and pipes, running through the sedimentary layers. One of these is only about 5 kilometres from the Sleipner CO2 plume, and it reaches all the way down into the Utsira formation.

The discovery of so many potential leakage paths in the few sites examined has scientists reconsidering how well-contained the Utsira reservoir really is. “We might have to appreciate that there is a much greater chance for some CO2 to leak out,” says Stefan Bünz, a marine geologist at the University of Tromsø in Norway, who participated in the ECO2 experiment.

Yet neither the ECO2 project nor Statoil has found any indications that CO2 has leaked from Sleipner in its 17 years of operation. Furthermore, the ECO2 team has tested the likely impact of leaks, should they occur, by injecting up to 150 kilograms of CO2 a day just above the sea floor near Sleipner. They found that the CO2 completely dissolved within the lower few metres of water, rapidly converting to bicarbonate and dispersing. Only a small amount of the injected gas may have reached the atmosphere, says Wallmann.

The researchers also studied a spot in the Mediterranean Sea where natural vents release about 1 tonne of CO2 a day. They found that the gas, which acidifies nearby waters, kills off many organisms within a small, 10-metre zone around the vent and reduces species diversity within a radius of about 100 metres, but that effects beyond that distance are limited.

A leak would be much more troubling from a public-relations standpoint, says Landschulze, because carbon capture and storage has been promoted in Europe as being safe. “It would be a disaster for public opinion,” she says.

Yet because offshore disposal happens far from population centres, it has some advantages over onshore storage. Germany, Spain and Norway are each running onshore pilot experiments in which they have injected tens of thousands of tonnes of CO2 into reservoirs underground, but some people have expressed concern about large-scale disposal on land. “I think it’s easier to work offshore in the sense that the public perception is not ready for CO2 storage in their backyards,” says hydrogeologist Pascal Audigane of the French Geological Survey in Orléans, who manages a €5-million carbon-storage project in an underground lab in Switzerland.

In the end, the biggest impediments to sub-seabed CO2 disposal are probably not leakage, but economics. Disposal makes sense at Sleipner, because the CO2 has to be separated from natural gas for commercial purposes anyway, and Norway would impose a tax on Statoil if the waste gas were released. But the price of carbon emissions would have to rise in other countries before it becomes worthwhile to pump waste CO2 from power plants and other sources on land to offshore injection sites. The chances of that happening soon may be slim, but carbon-storage researchers are carrying on with their work in case countries decide to push forwards with major cuts in greenhouse-gas emissions.


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Monastersky, R. Seabed scars raise questions over carbon-storage plan. Nature 504, 339–340 (2013).

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