Geological Storage of Carbon Dioxide (Geological Society of by Baines, Worden

By Baines, Worden

Carbon dioxide (CO2) is the most compound pointed out as affecting the steadiness of the Earth's weather. an important relief within the quantity of greenhouse fuel emissions to the ambience is a key mechanism for mitigating weather swap. Geological garage of CO2, or the injection and long term stabilization of huge volumes of CO2 within the subsurface in saline aquifers, in current hydrocarbon reservoirs or in unmineable coal seams, is among the extra technologically complex thoughts on hand. a couple of reports were performed and are suggested the following. they're aimed toward knowing the security, actual and chemical behaviour and long term destiny of CO2 whilst saved in geological formations. until eventually effective, replacement power recommendations might be built, geological garage of CO2, the topic of this quantity, presents a mechanism to lessen carbon emissions considerably while carrying on with to fulfill the worldwide call for for strength. additionally on hand: the way forward for Geological Modelling in Hydrocarbon improvement - targeted booklet no 309 - ISBN 1862392668 Underground fuel garage: around the globe reports and destiny improvement within the united kingdom and Europe - designated e-book no 313 - ISBN 1862392722 The Geological Society of LondonFounded in 1807, the Geological Society of London is the oldest geological society on the planet, and one of many greatest publishers within the Earth sciences.The Society publishes quite a lot of high quality peer-reviewed titles for teachers and execs operating within the geosciences, and enjoys an enviable foreign recognition for the standard of its work.The many components during which we put up in include:-Petroleum geology-Tectonics, structural geology and geodynamics-Stratigraphy, sedimentology and paleontology-Volcanology, magmatic reviews and geochemistry-Remote sensing-History of geology-Regional geology courses

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Eds) GHGT-5 Greenhouse Gas Control Technologies, CSIRO, Australia, 349-354. CHADWICK, R. , KIRBY, G. , LINDEBERG, E. & ZWEIGEL, P. 2004. 4D seismic imaging of a CO2 bubble at the Sleipner Field, central North Sea. , UNDERHILL, R. & LAPPIN, M. (eds) 3D Seismic Technology: Application to the Exploration of Sedimentary Basins. Geological Society, London, Memoirs 29, 311-320. , PEARCE, J. & BLACKWELL, P. 1996. Analysis of the geochemical aspects of the underground disposal of CO2. In: APPS, J. A. & TSANG, C.

1. The distribution of CO2 springs and gas pools in relation to the Alpine Fold belt and volcanicity (base map after Ziegler 1994). 1, Betic Cordillera (Ceron et al 2000); 2, Massif Central (Pauwels et al. 1997); 3, Eiffel (May 2001); 4, Bekes sub-basin (Clayton et al 1990); 5, West Pannonian Basin (this study and (Koncz 1983); 6, Derecske sub-basin (Lollar et al. 1994); 7, Latera (this study and (Gianelli and Scandiffio 1989); 8, Karlony Vary (Vrba 1996; Moller et al 1998); 9, Pannonian basin (Cornides 1993); 10, West Carpathians (Lesniak 1985); 11, Mura sub-basin (Kralj 2000); 12, SE Carpathians (Vaselli et al 2002); 13, Eger rift (Weinlich et al 1999); 14, Eger rift (Weise et al.

Chemical and isotopic determinations on the many carbonated springs found throughout the Massif Central and Southeast Basin area indicate that the CO2 and associated noble gases are predominantly (though not entirely) of mantle or deep-crustal origin (Matthews et al. 1987; Pauwels et al. 1997). Reservoirs are in Lower Jurassic and Triassic limestones, dolomites and sandstones at depths of between 2000 and 5000m. Among them, only the Montmiral site is currently exploited (Fig. 6), with production having started in 1990.

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