Basalt—A Better Sequester?
Scientists Attempt to Permanently Trap Carbon Dioxide in Deep Basalt
Laboratory studies by researchers at the Battelle-operated Pacific
Northwest National Laboratory (PNNL) indicate basalt formations
may quickly and effectively sequester carbon dioxide (CO2), the
predominant gas implicated in global warming.
Researchers hope to test their findings when they inject 3,000
tons of carbon dioxide—approximately the amount of CO2 that a
150-megawatt, coal-fired power plant emits daily—3,000 feet into
Washington State’s Columbia River basalt formation. Their goal is to
determine if the massive lava layers can permanently store the CO2.
“If the process is viable, we think basalts in the Pacific Northwest
could sequester more than a century’s worth of the CO2
generated in the region and create a major opportunity for
zero-emission power generation in the Northwest,” said Dr. Pete
McGrail, project manager.
 | | This stratigraphic map (above) shows
the layers of basalt beneath the injection
site. The large zone of interest (middle
pink) is located about 1,000 meters
below the ground surface. The project
will utilize six preexisting monitoring
wells within 100 meters of the injection
site to provide detailed information
about the vertical migration of the
carbon dioxide plume.
| “Experimental data from our laboratory studies show that carbon
dioxide injected into the volcanic rock should begin interacting
with the minerals in the basalt to form calcite, which is the primary
carbonate mineral in limestone, in four to six weeks,” McGrail said.
“This carbonate mineralization will permanently
and safely sequester the CO2 within the basalt formation
—if it works in the field like it has in the
laboratory.”
To help determine how much of the injected CO2 has been
mineralized, McGrail’s team plans to drill down at an angle to the
injection shaft and retrieve core samples 6 to 8 months and then
18 months after injection. Using a variety of geophysical monitoring
methods, they also plan to track movement of the CO2
underground. They will use the experimental data to forecast the
timing and extent of the sequestration in basalts.
McGrail points out that the CO2 injection will occur only
after the site north of Richland, Washington, has been prepared
and the necessary permits have been obtained.
The work was enabled through a U.S. Department of Energy
award to the Big Sky Regional Carbon Partnership. The
Partnership, led by Montana State University, includes a host of
universities, national laboratories (such as PNNL), international
research institutes, and private companies as partners. The project
is part of the President’s Global Climate Change Initiative designed
to reduce the nation’s greenhouse gas emissions intensity 18 percent by 2012.
For additional information, contact Dr. Pete McGrail at
(509) 376-9193, pete.mcgrail@pnl.gov.
|