LIVERMORE, Calif.-- Lawrence Livermore National Laboratory researchers have broken the record for tracking the movement and concentration of carbon dioxide in a geologic formation using the world's deepest Electrical Resistance Tomography (ERT) system.
The research provides insight into the effects of geological sequestration to mitigate the impact of greenhouse gases.
The team led by LLNL's Charles Carrigan obtained time lapse electrical resistivity images during the injection of more than 1 million tons of carbon dioxide (CO2) more than 10,000 feet deep in an oil and gas field in Cranfield, Miss., which represents the deepest application of the imaging technique to date. The previous depth record of about 2,100 feet was held by the CO2SINK Project Consortium in Ketzin, Germany.
"The images provide information about both the movement of the injected CO2 within a complex geologic formation and the change with time of the distribution of CO2 in the porous sandstone reservoir," Carrigan said.
Deep geologic sequestration of CO2 is being evaluated internationally to mitigate the impact of greenhouse gases produced during oil- and coal-based energy generation and manufacturing. Natural gas producing fields are particularly appealing sites for sequestration activities because the same geologic barrier or cap rock permitting the subsurface regime to act as a long term natural gas reservoir also can serve to permanently contain the injected CO2.
ERT allowed Xianjin Yang, another member of the LLNL team, to make a movie of the expanding CO2 plume as it fills the sandstone region between the two electrode wells. To do this required analyzing months of data and using only the highest quality results to produce the images.
The team reports on the design, placement and imaging from the world's deepest ERT system in the June 1 online issue of the International Journal of Greenhouse Gas Control. The research also will appear in an upcoming print copy of the journal.
|See the movie made from time-lapse ERT images of injected CO2 that appears to form a growing plume within the 80-meter-thick porous sandstone reservoir situated at a depth of more than 10,000 feet. Impermeable rock layers bound (horizontal dashed lines) the top and bottom of the sandstone reservoir. The ERT images of the CO2 invading the sandstone layers were made from 100's of thousands of measurements of electrode voltages while passing electric currents between the electrodes (red squares) mounted on two vertical wells drilled through the layer. The movie shows the development of the plume in the sandstone layer during a period of about 100 days. This is the deepest known ERT imaging to date. Image courtesy of Lawrence Livermore National Laboratory|
ERT can potentially track the movement and concentration of the injected CO2 as well as the degree of geologic containment using time-lapse electrical resistivity changes resulting from injecting the fluid into the reservoir formation.
Installing each ERT array in the sequestration reservoir required designing all cabling and electrodes, which were externally mounted on the borehole casing, to survive the trip more than 10,000 feet down a crooked borehole with walls made jagged by broken rocks.
The team then used the ERT array in a challenging environment of high temperature (260 degrees Fahrenheit), high pressure (5,000 psi) and high corrosive fluids to effectively detect CO2 breakthroughs and CO2 saturation changes with time.
"This is a near-real time remote monitoring tool for tracking CO2 migration with time lapse tomographic images of CO2 concentration," Carrigan said.
When converted to CO2 concentration, the images provided information about the movement of the injected CO2 within a complex geologic formation as well as how the storage of the CO2 changed with time.
Carrigan said that given concerns about injection-induced fracturing of the cap rock seal causing leakage of CO2 from the reservoir, higher-resolution ERT also may have an application as an "early-warning" system for the formation of fracture pathways in cap rock that could result in environmental damage to overlying or nearby water resources. Another potential application involves monitoring the boundary of a sequestration lease to ensure that CO2 does not migrate across the boundary to an adjacent parcel.
The ERT team includes Carrigan and Yang as well as Abe Ramirez, Roger Aines, Julio Friedmann and Neil Felgenhauer of LLNL; Robin Newmark of National Renewable Energy Laboratory; Doug LaBrecque and Bill Daily of Multi-Phase Technologies; and Dennis Larsen of Promore.
The ERT project is part the U.S. Department of Energy sponsored Southeast Regional Carbon Sequestration Partnership (SECARB) Cranfield project near Natchez, Miss., which has become the fifth ERT system worldwide and the first in the United States to inject more than a million tons of CO2 into the sub-surface.
The Cranfield study, which was led by Susan Hovorka of the Bureau of Economic Geology at the University of Texas, was funded by Department of Energy, National Energy Technology Laboratory under contract to the Southern States Energy Board.
Like this article? Click here to subscribe to free newsletters from Lab Manager