Aliso Canyon leakage as an analogue for worst case CO2 leakage and quantification of acceptable storage loss

被引:11
|
作者
Lindeberg, Erik [1 ]
Bergmo, Per [1 ]
Torsaeter, Malin [1 ]
Grimstad, Alv-Arne [1 ]
机构
[1] SINTEF Petr Res, POB 4763, NO-7465 Trondheim, Norway
关键词
TEMPERATURE; STATE;
D O I
10.1016/j.egypro.2017.03.1914
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Aliso Canyon gas well leakage is used as an analogue to study a possible accident from a CO2 storage site. Because the blowout is the second largest in USA, it can be used as a worst-case blowout analogue for a possible CO2 blowout from an underground CO2 storage. Reservoir modelling and well modelling of the Aliso Canyon case is used to determine the leakage pathway and leakage mechanisms that will mimic the escape history. This data are put in a new model where the gas is replaced by CO2 and a similar accident is simulated. Several factors are different between gas leakage from gas storage and potential leakage from a typical CO2 storage in an aquifer, due to differences in thermodynamic properties and flow properties both along in the leakage pathway and in the porous medium in the storage reservoir. The specific features of the two cases are compared and show that as the risk elements are very different, remediation measures will be different. The escape rate is significant lower for the CO2 scenario than the observed gas escape from Aliso Canyon gas well (4.9 Sm-3/s respectively 21.3 Sm-3/s). While 2.8 % of the stored gas was lost at the Aliso Canyon leak, the corresponding loss from a CO2 well if the facility was used for CO2 storage would be 0.37%. Due to the high density of CO2, the well pressure at the rupture was less than half than for CO2 compared to gas, which will make remediation easier. (C) 2017 The Published by Elsevier Ltd.
引用
收藏
页码:4279 / 4286
页数:8
相关论文
共 50 条
  • [31] Towards a method for leakage quantification and remediation monitoring in the near-surface at terrestrial CO2 geologic storage sites
    Romanak, Katherine
    Yang, Changbing
    Darvari, Roxana
    13TH INTERNATIONAL CONFERENCE ON GREENHOUSE GAS CONTROL TECHNOLOGIES, GHGT-13, 2017, 114 : 3855 - 3862
  • [32] Analysis on caprock and aquifer properties related with leakage during CO2 storage
    Park, Jooseon
    Park, Sung Soo
    Cho, Jinhyung
    Lee, Kun Sang
    GEOSYSTEM ENGINEERING, 2016, 19 (04) : 188 - 196
  • [33] On leakage and seepage of CO2 from geologic storage sites into surface water
    Oldenburg, C. M.
    Lewicki, J. L.
    ENVIRONMENTAL GEOLOGY, 2006, 50 (05): : 691 - 705
  • [34] The differential migration of noble gases as leakage proxy in CO2 geological storage
    Giannesini, Sophie
    Prinzhofer, Alain
    Moreira, Manuel
    Magnier, Caroline
    Schneider, Frederic
    GEOCHIMICA ET COSMOCHIMICA ACTA, 2009, 73 (13) : A433 - A433
  • [35] Potential CO2 leakage from geological storage sites: advances and challenges
    Mortezaei, Kimia
    Amirlatifi, Amin
    Ghazanfari, Ehsan
    Vahedifard, Farshid
    ENVIRONMENTAL GEOTECHNICS, 2021, 8 (01): : 3 - 27
  • [36] Quantitative assessment of CO2 leakage risk in geologic carbon storage management
    Jing, Meng
    Li, Qi
    Liu, Guizhen
    Xue, Quan
    GREENHOUSE GASES-SCIENCE AND TECHNOLOGY, 2024, 14 (06): : 1068 - 1091
  • [37] Diffusive leakage of Ebrine from aquifers during CO2 geological storage
    Dejam, Morteza
    Hassanzadeh, Hassan
    ADVANCES IN WATER RESOURCES, 2018, 111 : 36 - 57
  • [38] The assessment of leakage risk on the CO2 saline aquifer storage with presence of impurities
    Liu, Xingzhi
    Sun, Wenju
    Liang, Chenyu
    Sun, Qian
    Zhu, Yinghao
    Ampomah, William
    GEOENERGY SCIENCE AND ENGINEERING, 2025, 246
  • [39] Duke, NETL study CO2 storage impact: Leakage must be reckoned with
    不详
    AMERICAN CERAMIC SOCIETY BULLETIN, 2011, 90 (01): : 18 - 19
  • [40] CO2 leakage can cause loss of benthic biodiversity in submarine sands
    Molari, Massimiliano
    Guilini, Katja
    Lins, Lidia
    Ramette, Alban
    Vanreusel, Ann
    MARINE ENVIRONMENTAL RESEARCH, 2019, 144 : 213 - 229