2.1.4 Risks related to CO2 stream pressure and temperature

CO2 phase changes may occur when it is depressurised, depending on the initial and final pressure and temperature conditions. The depressurisation of CO2 by design or by accident can result in the sublimation temperature of solid CO2. In addition, significant quantities of solid CO2 can be formed within systems and/or within any release which in addition to its low temperature could cause blockages, and subsequent hazard. Having an adequate understanding of the thermodynamics of the CO2 stream, including the effects of the impurities, is essential within the design and operation of CO2 stream handling systems. Low temperatures could lead to the embrittlement of materials causing fractures and cracks (DNV, 2013).

CO2 density is also sensitive to temperature changes especially close to critical point conditions (i.e., 31 °C and 74 bars, see Fig. 2-3). This can lead directly to system over pressurisation with a relatively small change in CO2 temperature. Appropriate system pressure relief should avoid this leading to a hazardous event (DNV, 2013).

O. Fig. 2-3

Fig. 2-3: CO2 phase diagram with typical transportation conditions (DNV, 2013).

A rupture of e.g a vessel containing large amounts of liquid CO2 could lead to rapid pressure reduction which under certain conditions could escalate to create a Boiling Liquid Expanding Vapour Explosion (BLEVE). The probability of this occurring is believed to be extremely low but CO2 system designers should be aware of the potential (DNV, 2013).

Induced seismic activity has mainly been recognized along previously faulted rocks at waste disposal sites, oil fields, and other sites. Supercritical CO2 liquid is less dense than water and may cause density-driven stress conditions at depth or interact with formation water and rocks, causing a reduction in permeability and pressure build-up leading to seismic activity. Seismic events are unlikely to occur due to injection in porous rocks unless very high injection pressures cause hydraulic fracturing. Thorough characterisation, testing, and monitoring of stress conditions at depth will prevent the risk of unexpected seismic events (Sminchak and Gupta, 2002).

Possible health and safety risks related to CO2 stream pressure and temperature include inhalation of, or exposure to, very cold air mixture, contact with solid CO2 or cooled surfaces, rapid expansions, explosions and projectiles.