- Environmental Impact Assessment and Leakage detection -

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- Environmental Impact Assessment and Leakage detection - Tomakomai CCS Demonstration Project - Environmental Impact Assessment and Leakage detection - Jun Kita (kita@kaiseiken.or.jp), Marine Ecology Research Institute 1. Tomakomai CCS Demonstration Project 3. 3. Example of threshold for ecological impact Off-gas supply: Hydrogen production facility at oil refinery plant Table. Summary of elevated-CO2 effects on various marine organisms estimated from recent papers. Tomakomai Demonstration Project Organisms pCO2 Effect Calcifiers Molluscs Echinoderms Corals Coccolithophores D200μatm < Calcification decrease Non-calcifiers Fish Copepods D2,000μatm < Physiological disturbance CO2 capture: Amine absorption Nagaoka Pilot Scale Project 800 km CO2 injection: Onshore Tokyo Reservoirs: under the seabed • Sandstone layer: 1100-1200m depth • Volcanic rocks layer: 2400-3000m depth Even in the extreme leakage scenario it was concluded that the impact on the ecosystem was negligible. 4. Monitoring program required in the ACT Conformance: Observed behavior of CO2 in the reservoir should fall into line with predictions. Containment: Secure retention of CO2 in the reservoir should be demonstrated. Distribution of CO2 in the reservoir needs to be tracked. No signs of leakage needs to be shown in the marine environment. Contingency: If leakage does occur, Amount of leakage needs to be quantified. Any environmental impacts need to be assessed. The onshore Nagaoka Pilot Scale Project was carried out from 2003 to 2005, with a total of 10,000 tonnes CO2 injected in a saline aquifer. The project successfully demonstrated that injected CO2 was safely stored in the reservoir. The offshore Tomakomai Demonstration Project was started by the Ministry of Economy, Trade and Industry, METI, for the period 2012 -2020 to demonstrate and verify the total CCS system. The operator of the project is Japan CCS Company. It is planned that 100,000 tonnes/year or more CO2 is to be stored under the seabed. CO2 injection started in early April 2016 and will continue to 2018. 4. 1. Required monitoring items CO2 injection: Volume (flow meter), concentration (gas chromatography), injection condition (pressure, rate, temperature) Wellbore condition: Pressure and Temperature of injection well and observation well Reservoir: Location and dimension of stored CO2 (time-lapse (4D) seismic) Marine environment: Seawater chemistry (pH, TCO2, Alkalinity, DO, etc.) Maine biota (micro-, meio-, macro-, mega-benthos) Marine activities (fisheries, maritime affairs, protected reserves, etc.) 2. Regulation for offshore CO2 storage in Japan Act for the Prevention of Marine Pollution and Maritime Disasters May 2007: The act was amended to allow a permitting procedure for dumping the CO2 stream into sub-seabed formations in accordance with London Protocol. Seeks to prevent marine environmental impacts from potential CO2 leakage Operator of Offshore CO2 storage, Shall receive permission from the environmental minister. Shall implement an Environmental Impact Assessment. Shall monitor the surrounding sea environment for assurance of no-leakage. 3. Environmental Impact Assessment (EIA) in the ACT Objective: Estimation of CO2 dispersion and assessment of environmental impact assuming that stored CO2 leaks out into the sea Process: Consideration of leakage scenarios and their simulation CO2 migration in the geological formation CO2 dispersion in the seawater column Base-line survey for the existing marine environment Impact assessment 4. 2. Tiered monitoring plan in the Act Three-tiered monitoring plan must be implemented depending on the severity of changes that could occur following CO2 storage Routine monitoring: When: No indication of leakage How: Distinguish leakage signal from natural variability Precautionary monitoring: When: Possible leakage How: Confirm existence or non-existence of leakage Emergency monitoring: When: Leakage has taken place How: Determine location and extent of the leakage and its impact 3. 1. Simulation for CO2 migration in the geological formation Scenario: Leakage through faults undetectable by seismic survey Simulator: TOUGH2 with ECO2M (LBNL) Output: CO2 flux at the seafloor 1.5 yrs 5 yrs 10 yrs Liquid phase Gas phase 16 yrs 30 yrs 40 yrs Liquid phase Gas phase 4. 3. Leakage detection by seawater quality The regulatory authority strongly urged the use of the relationship between concentrations of oxygen and carbon dioxide to detect leakage. Since the baseline data did not fully reflect the natural variation, false positive occurred. Ultimately, the observed value (false positives) were judged to be within the range of natural variation by the expert judge. In other words, no leakage was confirmed. Baseline data Monitoring data False positive Approximate curve of baseline data Upper 95% prediction interval of baseline data Fig. Simulations show that stored CO2 never reaches the seafloor through small faults that are undetectable by seismic surveys. These figures were only derived under extreme leakage scenarios. 3. 2. Simulation for CO2 dispersion in the seawater Input: CO2 flux at the seafloor Simulator: MEC-CO2 two-phase flow model (Kano et al., 2010, IJGGC, 3, 617-625. Output: CO2 concentration gradient in the seawater column Fig. Relationship between oxygen saturation (DO) and CO2 partial pressure (pCO2) of bottom seawater (2 m above the seafloor). 5. Lessons learned If the baseline data does not fully reflect the natural variation, occurrence of false positives or false negatives will be high. Further studies are needed for collecting appropriate baseline data to detect leakage by seawater quality analysis. Integrated review, i.e. not only analysis of seawater but also monitoring data of CO2 injection, wellbore and reservoir, should be considered for leakage detection. Fig. X axis shows seafloor and Y axis shows depth of seawater. Left and middle figures indicate leakage from 100m diameter circle area. Left is for a summer condition and middle is for a winter. Right figure indicates leakage from a 500m circle area in winter.