A downhole CO2 sensor can continuously collect real-time data about CO2
movement and concentration changes at subsurface conditions. These data
are very valuable for better understanding of subsurface uncertainties
and quality-controlling theoretical studies such as reaction, transport,
and mechanics in oil and gas formations. This paper describes the
development of a downhole CO2 sensor tested under high pressure and
reservoir conditions to monitor aqueous CO2 concentration change.
The CO2 sensor developed is a Severinghaus-type sensor, which includes a
metal-oxide electrode, a gas-permeable membrane, a porous steel cup,
and a bicarbonate-based internal electrolyte solution. The CO2 sensor
thus prepared 0.7 in. in diameter and 1.5 in long. A linear correlation
was observed between a change in sensor output potential and dissolved
CO2 in water under 1,000 psi pressure. CO2/brine coreflooding tests were
performed to simulate the CO2 storage process and the sensor was
deployed to monitor CO2 movement. The results indicated that the CO2
sensor could monitor CO2 movement in-situ in CO2 storage processes.
Introduction
Geologic sequestration of CO2 involves putting CO2 into long-term
storage in geologic zones at subsurface conditions. Such sites as deep
saline aquifers and unmined coal seams onshore, and depleted oil or gas
formations both onshore and offshore have been recommended for further
serious consideration. Thus far, in various regions of the world
(Pacific Ocean, Gulf of Mexico, North Sea, Chinese East sea, and the
Atlantic Ocean), a large part of research studies and pilot projects
have looked at the feasibility of geological sequestration of CO2. The
first commercial project occurred in Norway in 1996, in which CO2 was
captured from natural gas streams and around 1 million tons of CO2 per
year were into the Utsira formation and to provide insight into CO2
migration. All these pilot studies, located in Kansas, Virginia, West
Virginia and Canada, are either under consideration or have been
initiated.
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