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Wallula Basalt Project

Basalt cliffs overlooking the Columbia River at the Wallula Gap, Wash. Oct. 2020
Basalt cliffs overlook the Columbia River at the Wallula Gap in southeast Washington state. (Photo by Andrea Starr | Pacific Northwest National Laboratory)

Continued global use of fossil fuels places a premium on developing technology solutions to minimize increases in atmospheric carbon dioxide (CO2) levels. One such solution may be storing CO2 in reactive basalts by permanently converting injected gaseous CO2 into solid carbonates.

In 2013, PNNL researchers began a field demonstration of carbon storage by injecting ~1,000 metric tons of CO2 into a natural basalt formation in Eastern Washington State.

After two years of post-injection monitoring, the researchers obtained cores from within the injection zone and subjected them to detailed physical and chemical analysis. Nodules found in vesicles throughout the cores were identified as the carbonate mineral ankerite, which includes calcium, iron, magnesium, and manganese. Further carbon isotope analysis revealed that the nodules were chemically distinct from natural carbonates present in the basalt and in clear correlation with the isotopic signature of the injected CO2.

Calcium Carbonate Nodules
Calcium carbonate nodules.
Source: Odeta Qafoku | PNNL

These findings provided field validation of rapid mineralization rates observed from years of laboratory testing with basalts.

Since the project ended in 2015, PNNL scientists have used data gleaned from the project to identify other basalt-rich sites in the Pacific Northwest.

 

 

 

Layered basalt flow WEB
Illustration of layered basalt flow. Source: Todd Schaef | PNNL

Contacts

Casie Davidson
Manager, Carbon Management and Fossil Energy Market Sector
casie.davidson@pnnl.gov
509-372-6259
Todd Schaef
Subsector Manager, Subsurface Energy Systems
todd.schaef@pnnl.gov
509-371-7102

Research topics

Carbon Storage
Carbon Management
Fossil Energy
Energy Resiliency
Subsurface Science
Subsurface Energy Systems

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