Carbon Cycle Science & Technology Group
Carbon Capture & Storage
Principal Investigator
Jeff Fitts
Successful large-scale implementation of Carbon Capture and Sequestration
(CCS) requires clear demonstrations that it is possible to accurately
quantify the environmental and human health risks, and the cost, of geologic
carbon dioxide (CO2) storage. However, significant uncertainties
exist due to limited knowledge of the interaction between CO2
and geologic formations within the storage environment. These potential
interactions may positively or negatively impact reservoir performance. Brookhaven
researchers are developing modeling frameworks and experimental methods to
identify, quantify, and manage some of the most important uncertainties.
How much do we know about the geologic
and geochemical setting of prospective CO2 storage reservoirs?
Models of prospective geologic reservoirs are, in the best cases,
constructed using geostatistical methods that combine often sparse and
variable datasets to predict geologic storage formation characteristics
and the performance of the caprocks that must prevent the CO2 from
leaking into other subsurface resources or back into the atmosphere.
These models consider structural geology, mineralogy, permeability,
porosity, eventual CO2-brine chemistry, and fracture type and
frequency. We are building on the extensive databases developed by the
DOE Regional Carbon Sequestration Partnerships, state geological surveys
(e.g.,
Ohio State Survey) and university geologic repositories (e.g.,
Western Michigan University Geological Repository) to develop methods to
quantify uncertainties and heterogeneities of reservoir formations,
performance criteria and pore-water geochemistry that ultimately define how well we understand these critical processes. The databases and model
results will also provide boundary conditions for the
experimental research described below. (Figure: CCS Project Schematic;
Source: Alberta
Geological Survey)
How will geochemistry impact reservoir
capacity and long-term CO2 retention?
Current models used to predict CO2 behavior in reservoirs only
consider the hydrodynamics and physical characteristics of the geologic
formations, and assume that geochemistry will not impact reservoir
performance. We are developing experimental tools and methodologies to
identify the conditions under which CO2-saturated brines will
impact flow within migration pathways by reacting with reservoir formations, caprocks,
and well cements. In order to study the origin of any flowpath
changes, synchrotron-based microprobe and diffraction tomographic imaging
methods are being developed at Brookhaven’s
National Synchrotron Light Source (NSLS)
beamline X27A. These capabilities are being used to study pore-scale
precipitation and corrosion processes in core samples under pressure and
temperature conditions that mimic geologic storage reservoirs. The
3-dimensional in-situ imaging capabilities will benefit greatly from
improved spatial resolution and sensitivity upon completion of the
NSLS II. (Figure: X-ray diffraction microtomography at beamline X27A)
How accurately can we predict the environmental and
human health risks, and the cost of geologic CO2 storage?
Accurate risk assessments and costing models of site-specific geologic
storage projects and regional capacity assessments require the development
of a decision-making framework that integrates the
latest scientific understanding of pore-scale flowpath geochemistry. Major
collaborative efforts are required to tackle scaling issues and achieve this
level of integration. We have teamed up with
Princeton University and the
University of Minnesota to develop an integrated decision making
framework (see DOE Office of Fossil Energy NETL
project factsheet).

Last Modified: April 27, 2012 Please forward all questions about this site to:
Alistair Rogers
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