12:00 PM - 12:15 PM
[HSC07-12] Mechanisms inducing anomalously high pCO2 without CO2 leakage in coastal environment
Keywords:Sub-seabed CO2 storage, Marine monitoring, CO2 leakage, pCO2, Total alkalinity
When CO2 is stored in sub-seabed geological formations in Japan, marine monitoring is mandatory to detect CO2 leakage as soon as possible should it occur. In the Tomakomai CCS Demonstration Project, a threshold line based on a negative correlation between partial pressure of CO2 (pCO2) and dissolved Oxygen saturation in seawater is used to detect an anomalously high value of pCO2, which is suspected to be a sign of CO2 leakage. Although CO2 leakage has never occurred in Tomakomai, pCO2 values obtained in the monitoring have frequently exceeded the threshold line; that is, many false-positives have been produced. It is important to consider what can be causes of the false-positives. To discuss the causes, we analyzed data observed in the marine monitoring of the Tomakomai project, and meteorological data at Tomakomai. It is implied that weather conditions, such as wind speeds and precipitation, were related with false-positives. Also, we found that total alkalinity was remarkably low at a monitoring survey where many false-positives were observed. The low values of total alkalinity make pCO2 values higher than usual, and consequently they might produce many false-positives. Based on the results, we are going to present how to avoid or reduce false-positives.