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ÇAĞRILI KONUŞMALAR / KEYNOTES Invited Speeches ... - TPJD

ÇAĞRILI KONUŞMALAR / KEYNOTES Invited Speeches ... - TPJD

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Cap Rock Integrity in Co 2 Storage<br />

Chantsalmaa Dalkhaa, Ender Okandan<br />

Middle East Technical University, Department of Petroleum and Natural Gas Engineering,<br />

Ankara<br />

One way to reduce the amount of CO 2 in the atmosphere for the mitigation of climate change is<br />

to capture the CO 2 and inject it into geological formations such as depleted oil and gas reservoirs,<br />

aquifers, oceans and unmined coal beds. The most important public concern about carbon<br />

capture and storage (CCS) is whether stored CO 2 will leak into groundwater sources and finally<br />

into the atmosphere or not, since CO 2 at high concentration is hazardous. During underground<br />

CO 2 storage, the containment of CO 2 will be crucially dependent on the cap rock integrity above<br />

the CO 2 . Thus, it is important to assess how the CO 2 might impact cap rocks, since this could<br />

control the ultimate longevity of CO 2 storage. Although supercritical CO 2 is normally inert, when it<br />

dissolves in water or brine, it makes water acidic. This acidic water can react with the surrounding<br />

rock minerals and thus geochemical reactions, dissolution of primary minerals and precipitation<br />

of secondary minerals, take place. These reactions can alter the porosity and the permeability<br />

and furthermore affect the sealing capacity of cap rocks. The objective of this research is to<br />

identify the geochemical reactions of the dissolved CO 2 in the synthetic formation water with<br />

the rock minerals of the Sayındere cap rock by laboratory experiments. It is also aimed to model<br />

and simulate the experiments using ToughReact software. Sayındere formation is the cap rock<br />

of the Caylarbasi, a southeastern petroleum field in Turkey. The mineralogical investigation and<br />

fluid chemistry analysis of the experiments show that calcite was dissolved from the cap rock<br />

core as a result of CO 2 - water- rock interaction. Using the reactive transport code TOUGHREACT,<br />

the modeling of the dynamic experiment is performed. Calcite, the main primary mineral in the<br />

Sayındere is dissolved first and then re-precipitated during the simulation process. The decreases<br />

of 0.01 % in the porosity and 0.03% in permeability of the packed core of the Sayındere cap rock<br />

are observed in the simulation. The simulation was continued for 25 years without CO 2 injection.<br />

However, the results of this simulation show that the porosity and permeability are increased by<br />

0.001 % and 0.004 %, respectively due to the CO 2 -water-rock mineral interaction. This shows that<br />

the Sayındere cap rock integrity must be monitored in the field if application is planned.<br />

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