Home PhD thesis: Sub surface storage of CO2 in depleted gas fields in the Netherlands? “No problem” says Suzanne HangxThesis Overview
Sub surface storage of CO2 in depleted gas fields in the Netherlands? “No problem” says Suzanne Hangx
On Monday 14 September Suzanne Hangx defended her thesis Geological storage of CO2: Mechanical and chemical effects on host and seal formations. She did not find any negative effects of subsurface stored CO2. Results demonstrated very slow mineralisation reactions which depend strongly on the mineral contents of the reservoir. Suzanne Hangxs also researched CO2 removal from the atmosphere by (coastal) weathering of sand grade olivine.
Thesis Suzanne Hangx: Sub surface storage of CO2 in depleted gas fields in the Netherlands? “No problem” says Suzanne Hangx
The socio-economic impact of global warming resulting from anthropogenic CO2 emissions has led to much attention for carbon mitigation strategies in recent years. One of the most promising ways of disposing of CO2 is through Carbon Capture and Storage (CCS), entailing CO2 capture at source, followed by long-term geological storage. Possible storage sites include depleted oil and gas reservoirs, saline aquifers and unmineable coal seams. The former is relevant for countries with an extensive hydrocarbon production and transport infrastructure such as the Netherlands. However, long-term sub surface storage of CO2 in depleted reservoirs may induce a range of chemical and mechanical processes in response to disturbances in existing chemical equilibria and in the state of stress within the reservoir-cap rock system. Such processes include, but are not limited to, mineralisations reactions, reservoir creep induced by CO2-water-rock interreactions, and mechanical failure of and permeability development in the seal formations. While some of these processes, such as mineralization, may enhance the CO2 storage capacity of a reservoir, others may potentially reduce reservoir and cap rock integrity, causing leakage of CO2 tot the geological environment and ultimately to the atmosphere. Today, many of these processes are still poorly constrained.