CO2 Leakage Marine Dispersion Modelling for an Offshore Depleted Gas Field for CO2 Storage

M. R. Amir Rashidi, Edgar Peter Dabbi, A. I. Azahree, Zainol Affendi Abu Bakar, Dylon Tan Jen Huang, C. Pedersen, Pankaj K. Tiwari, M. T. M Sallehud-Din, M. Shamsudin, M. K. Hamid, R. Tewari, Parimal A. Patil
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引用次数: 2

Abstract

A depleted gas field situated in offshore Sarawak has been identified by PETRONAS as a potential CO2 storage development site. As part of the monitoring program, CO2 seepage risk and impact on the marine environment needs to be investigated and predicted. This study focuses on understanding the environmental risks associated with the potential seepage of CO2 gas at the depleted field within the 140 m water column through methods of numerical modelling. Leakage scenarios involving existing plugged and abandoned (P&A) wells as CO2 leakage pathways were modelled with leakage rates of 6 tonnes/year, representing a realistic rate and 500 tonnes/year which represents a more improbable and conservative scenario. The modelling period covers three representative climatic periods for the prevailing monsoons in the South China Sea (northwest, southwest and inter-monsoon). Simulation results showed that with the lower rate, changes to the seawater acidity within the far field region were negligible or undetectable. Under the high seepage rate, the pH plume footprint was predicted to extend beyond 200 m distance from the source point. However, the probability was estimated to be less than 1% while the vertical extent of the plume was limited up to 2 m above the seabed. For both scenarios, the CO2 gas were predicted to be fully dissolved within 5 m above the seabed. Therefore, it can be concluded that there is relatively low risk of impact at the storage field in terms of potential increase in seawater acidity if CO2 seepage occurs during the storage period.
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海上枯竭气田二氧化碳封存CO2泄漏海洋扩散模型
马来西亚国家石油公司已确定位于沙捞越近海的一个枯竭天然气田为潜在的二氧化碳储存开发地点。作为监测计划的一部分,需要调查和预测二氧化碳渗漏对海洋环境的风险和影响。本研究的重点是通过数值模拟的方法,了解枯竭油田140 m水柱内CO2气体潜在渗漏的环境风险。泄漏情景涉及现有封堵弃井(P&A)作为二氧化碳泄漏途径,泄漏率为6吨/年,代表了一个现实的速率,500吨/年代表了一个更不可能和保守的情景。模拟期涵盖了南海盛行季风的三个代表性气候期(西北、西南和季风间期)。模拟结果表明,在较低速率下,远场区域的海水酸度变化可以忽略不计或检测不到。在高渗流速率下,预测pH羽流足迹会延伸到离源点200 m以外的地方。然而,由于烟羽的垂直范围被限制在海床上方2米,估计这种可能性小于1%。在这两种情况下,预计二氧化碳气体将在海床上方5米内完全溶解。因此,可以得出结论,如果在储存期间发生CO2渗漏,海水酸度的潜在增加对储存场的影响风险相对较低。
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