Submitting Institution
University of CambridgeUnit of Assessment
Earth Systems and Environmental SciencesSummary Impact Type
TechnologicalResearch Subject Area(s)
Earth Sciences: Geochemistry, Geology, Physical Geography and Environmental Geoscience
Summary of the impact
Geological storage of CO2 requires prediction of the fate of
stored CO2 for ~ 10,000 years
after injection, a period much longer than can be observed in injection
experiments or
modelled. The only way to directly observe the behaviour of CO2
in crustal reservoirs over such
time periods is to study accumulations of natural CO2. This
case study developed from
research undertaken in the Department of Earth Sciences by Bickle between
2006 and 2011
on one such natural accumulation at Green River, Utah, USA. As a result of
this research,
Shell Global Solutions International BV, identified Green River as a
location where they
could evaluate the long-term response of caprocks to CO2accumulations.
In 2011 they
commenced a major drilling and research program to recover and study
caprock,
reservoir rocks and fluids. The data we have generated from this work
is being used to
evaluate large-scale CCS projects including the proposed Goldeneye
project in the UK
North Sea.
Underpinning research
The key research and insights which have led to the impact and commercial
investment
described have been underpinned by Bickle's research since the 1980's into
the modelling of
fluid movement in rocks, in particular the development of methods to infer
past fluid
movements in crustal settings using natural geological examples.
An important step in this research was the modelling of CO2
degassing from Himalayan hot
springs in the early 2000s (published in 2008). This led onto work, which
commenced in 2006,
on the natural CO2 system at Green River, Utah. Our work on
Green River entailed careful
documentation and interpretation of all the geological aspects that were
available for study at
the surface; these included fluids sampled from the CO2 geysers
as well as exhumed outcrop
which had previously held similar CO2 reservoirs. A key paper
on the Green River system,
published in 2009, demonstrated that it was possible to:
a) recover both the nature and rates of the fluid-mineral reactions in
the underlying CO2-
charged reservoir by sampling, analysing and modelling the fluid
compositions of cold
CO2 geysers sampled at surface;
b) show that reaction rate was critically dependent on the proximity of
the fluids to
chemical equilibrium with the reservoir minerals.
This and other work on the natural CO2 system gave the
Cambridge group an international
reputation for research on natural analogues for geological carbon
storage. Funding for our
CCS research came from a NERC national consortium CCS grant in 2005, a
Marie Curie
Training network (2006-2010) and a £3.2 million NERC consortium grant
(2008-2015), led by
Cambridge.
The work was brought to the attention of Shell Global Solutions
International BV as a result
of a presentation of our research at a meeting of our Industrial
Associates Scheme in 2009
(see our impact template for information about this scheme) attended by
key company
employees. This led to their subsequent invitation to join an academic
consortium researching
geological analogues for CO2 storage. Shell recognised that
available studies of the caprocks
overlying geological CO2 reservoirs were totally inadequate for
addressing the key questions of
long-term reservoir integrity. On the basis of our earlier research, as
well as a review and a
field visit led by Cambridge, Shell chose the Utah site for a drill hole
to sample caprock.
The drilling was carried out by DOSECC, the US continental drilling
facility, and had 100%
core recovery through the critical caprock and reservoir intervals. Fluid
sampling was carried
out by Cambridge and led to the successful recovery of samples at
formation pressure
enabling the critical pH and dissolved CO2 concentration
measurements to be carried out at
pressure, the first such measurements in a drill hole to study geological
carbon storage.
Members of the group working on this project and acting as co-authors on
publications have
included: Professor Bickle, (Cambridge 1983-present and Professor of
Tectonics since 2000),
Dr Holland (Cambridge 1979-present, Reader in Petrology since 2001), Dr
Galy (Cambridge
2000-present, University Senior Lecturer since 2007), and Research
Associates Dr Chapman
(Cambridge 1984-present), Dr Becker (Cambridge 2001-2007), Dr Kampman
(Cambridge
2006-present) and Dr Dubacq (Cambridge 2010-2012). Dr Assayag (Cambridge
2008-2009 as
Marie Curie Experienced Researcher) was part of the research group as were
two young
researchers, Wigley and Nicholl).
External Collaborators include:
Prof Ballentine (of Manchester University, now at Oxford, who has carried
out noble gas
geochemistry), Dr Sherwood Lollar (University of Toronto who has carried
out stable isotope
geochemistry), Prof Ellam (SUERC, East Kilbride who carried out U-series
dating), Prof
Shipton (Strathclyde), and Dr Burnside (Edinburgh) who have been involved
with the U-series
dating.
References to the research
Those which best indicate the quality of the underpinning research are
indicated (*),
Cambridge co-authors are shown in bold.
1/ Becker, J. A., Bickle, M. J., Galy, A., and Holland, T. J.
B., 2008, Himalayan
metamorphic CO2 fluxes: Quantitative constraints from
hydrothermal springs: Earth and
Planetary Science Letters, v. 265, p. 616-629,
doi:10.1016/j.epsl.2007.10.046
2/ Bickle, M. J., 2009, Geological carbon storage: Nature
Geoscience, v. 2, no. 12, p. 815-
818, doi:10.1038/ngeo687.
3/ * Kampman, N., Bickle, M., Becker, J., Assayag, N., and Chapman,
H., 2009, Feldspar
dissolution kinetics and Gibbs free energy dependence in a CO2-enriched
groundwater
system, Green River, Utah: Earth and Planetary Science Letters, v. 284,
no. 3-4, p. 473-
488, doi:10.1016/j.epsl.2009.05.013.
4/ * Dubacq, B., Bickle, M. J., Wigley, M., Kampman, N.,
Ballentine, C. J., and Sherwood
Lollar, B., 2012, Noble gas and Carbon isotopic evidence for CO2-driven
silicate dissolution
in a recent natural CO2 field: Earth and Planetary Science
Letters, v. 341-344, p. 10-19,
doi:10.1016/j.epsl.2012.05.040.
5/ * Kampman, N., Burnside, N. M., Shipton, Z. K., Chapman,
H. J., Nicholl, J. A., Ellam, R.
M., and Bickle, M. J., 2012, Pulses of carbon dioxide emissions
from intracrustal faults
following climatic warming: Nature Geoscience, v. 5, p. 352-358,
doi:10.1038/ngeo1451.
6/ Wigley, M., Bickle, M., Kampman, N., and Dubacq, B., 2012,
Fluid-Mineral Reactions in
an Ancient CO2 Reservoir, Green River, Utah.: Geology, v. 40,
p. 555-558, doi:
10.1130/G32946.1.
Peer reviewed Grants:
• 2005-2008: NERC, `The UK Carbon Capture and Storage Consortium'
(£130,000 to
Cambridge).
• 2006-2010: EU Marie Curie Training Network `GRASP', (£213,673 to
Cambridge).
• 2008-2013: NERC Consortium Grant led by Cambridge: `Predicting the fate
of CO2 in
geological reservoirs for modelling geological carbon storage'.
(£2,957,549 total
Cambridge, Manchester, Leeds, BGS; £901,212 to Cambridge).
• 2012-2015: DECC "£20 million Innovation grant": `The Long Term
Performance of
Geological Seals to Carbon Storage'. (£735,533 total Cambridge,
Manchester, BGS,
£401,000 to Cambridge).
Details of the impact
The main impact of this research has been to enable a multi-national oil
company (Shell) to
apply evidence-based research results to the major problem of
predicting the long-term
integrity of geological storage sites.
Our detailed and ground breaking research on the Green River site clearly
demonstrated to
Shell the value of research on a geological analogue for CO2
storage and was critical in
establishing the site's suitability for extensive investment. Shell Global
Solutions International
reallocated internal budgets to fund work on the Green River site and to
redeploy company
scientific staff to work on the project. Their commercial investments to
develop and research this
bore-hole site, providing them with a geological analogue for CO2
storage, have already
amounted to direct expenditure of over £1M, including £330k on the
drilling and £750k on
associated research. The work has allowed a new and improved assessment
for use in the
evaluation of risk in storage sites. In particular, the results of
the research have been used
to test and verify Shell's in-house reactive-transport modelling codes
which have
increased understanding of long-term CO2
plume migration e.g. for storage in the
Goldeneye field from the Peterhead project being assessed in the UK
North Sea as part
of the DECC-funded £1 billion CCS Commercialisation Competition.
The unquantified risks of ensuring that `that the stored CO2
will be completely and
permanently contained' (DIRECTIVE 2009/31/EC) have been previously
cited as key obstacles
to implementation of geological carbon storage. The costs of such risks
include the significantly
enhanced insurance premiums against leakage from storage, a high cost/low
risk event, the
costs of mitigating such leaks, as well as public opposition, engendered
by the concern that the
CO2 stores may leak. All the major reports on implementing CCS
published in the UK during
2011 and 2012 identify security of storage including caprock (geological
seal) behaviour as a
key uncertainty which should be a high priority for research. The DECC CCS
Roadmap, 20122
lists `Improve understanding of geological seal integrity and
subsurface CO2 behaviour' as a
high priority under R&D needs for storage. The APGTF Report, 20117
(Table 4) cites caprock
integrity as a high priority for immediate research. The FEED Report
(20118 ,Table 7.1.4-2),
the most authoritative assessment of a commercial storage site to date,
lists `post-closure
consent uncertainties' as risk No. 4, `adverse public reaction'
as risk No 9 and `migration of
CO2 from storage site' as risk No. 17, in
the list of the top 50 Post-FEED risks. Each of these
depend on demonstration of caprock and seal integrities. The outcomes of
the FEED report
are particularly important as this establishes that the long term risks
were one of the causes of
the failure of the first DECC £1 billion CCS program.
The eventual importance of carbon capture and storage to the UK economy
has been
estimated at £42 billion a year by 2050 (DECC interim report `The
potential for reducing the
costs of CCS in the UK', DECC, November 2012). Shell now leads one
of the two proposals for
major government-subsidised storage schemes currently being evaluated in
the UK under
DECC's £1 billion CCS Commercialisation Competition. Our
work on caprock integrity is
a fundamental element in the risk assessments necessary for this
scheme to go ahead
and these new and improved methods of risk assessment and management have
been crucial
to ensuring the mitigation of potential future losses.
The Manager for CO2 Storage Technologies at
Shell Global Solutions
International will verify that "the extensive field and
laboratory work on natural CO2 analogues
in Utah, together with an advanced process understanding, has led to the
decision by Shell
management to invest into drilling a research well into the CO2-charged
formations in Green
River" and that the data generated "will be used to test and
verify in-house modelling codes"
for industrial scale CCS operation. He will also corroborate the level of
the company's financial
investment.
The initial dissemination of our research, which impacted on Shell, was a
presentation at
the Department of Earth Sciences in Cambridge to the Earth Sciences
Industrial Associates at
our annual meeting. This was followed by several meetings and
presentations to Shell Global
Solutions International BV in Rijswijk, the Netherlands.
A further impact of this research is the contribution to the UK
industrial sector of an on-
going, regular supply of highly trained post-doctoral students and
researchers. Three of the
post-doctoral researchers are now either employed by major oil companies
(Becker, Exxon) or
have permanent academic research positions, in the UK (Kampman) and France
(Dubacq).
Sources to corroborate the impact
The Manager for CO2 Storage Technologies at Shell Global
Solutions International.