Jm. Pearce et al., NATURAL OCCURRENCES AS ANALOGS FOR THE GEOLOGICAL DISPOSAL OF CARBON-DIOXIDE, Energy conversion and management, 37(6-8), 1996, pp. 1123-1128
Citations number
11
Categorie Soggetti
Energy & Fuels",Mechanics,"Physics, Nuclear",Thermodynamics
It is now generally accepted that anthropogenic CO2 emissions are cont
ributing to the global rise in atmospheric CO2 concentrations. One pos
sibility for reducing carbon dioxide emissions is to remove it from th
e flue gases of coal-fired power stations and dispose of it in undergr
ound geological reservoirs, possibly offshore in the North Sea. The fe
asibility of this option has been studied in detail by a consortium of
European partners. As part of this study, natural occurrences of carb
on dioxide were identified and preliminary information from these was
obtained. The best characterised are found in the United Stales where
the carbon dioxide reserves are exploited for use in tertiary enhanced
oil recovery (EOR) programs in the Texas oilfields. The carbon dioxid
e reserves occur in geological structures and lithologies which are si
milar to those present in the North Sea. As such, these fields offer a
n ideal natural analogue for the disposal of carbon dioxide, since the
interactions with groundwaters and reservoir lithologies have occurre
d on both spatial and temporal scales relevant to geological processes
. Those carbon dioxide fields currently being exploited have already b
een studied to a limited extent by the oil companies involved. However
, further study is required to provide information on the potential ef
fects that disposing of large quantities of carbon dioxide might have
on groundwaters and reservoir quality. In addition, more detailed info
rmation will be obtained on the interactions which occur during EOR us
ing carbon dioxide. This paper presents data on some of the natural ca
rbon dioxide fields, and compares the effects of these natural fluid-r
ock interactions with those observed in laboratory experiments perform
ed to establish what reactions occur during the geological disposal of
carbon dioxide.