Bow-tie risk assessment combining causes and effects applied to gasoil storage in an abandoned salt cavern,

A semi-quantitative risk assessment is presented for the storage of gas oil in depleted salt caverns in the Twente region, the Netherlands. It is based on a bow-tie model, in which an incident, leakage of gas oil from the storage system (cavern and wells), is evaluated by assessing its possible causes and effects. The causes are all the events thatmay lead to leakage fromthe storage system. The effects are the consequences of the leakage. It is considered that themost serious of the subsurface risks is contamination of the groundwater due to upward migration of the gas oil to the surface. A unique aspect of our risk assessment is the combination of causes and effects. The effects of containment/failure are quantified at multiple time scales using a numerical flow model for multiphase flow through porous medium, based on the geohydrological properties of the subsurface of the Twente area. The probability of occurrence of loss of containment/failure (causes) is quantified semi-quantitatively, using the causal relationships between the causes and effects. Modelling of the leakage shows that, as expected, leakage from the well above the hydrogeological base in the phreatic aquifer produces an immediate risk of contamination of the upper groundwater. However, leakage at a deeper level does not pose a risk of contamination of groundwater, because the low porosity and permeability of the geological layers prevent the upward migration of leaking gas oil. The semi-quantitative approach to the probability of failure finds that for multiple scenarios (e.g. well failure, unstable cavern, high pressure) and in the absence of human intervention, the probabilities of failure are medium to high. If human intervention is assumed, these probabilities of failure diminish considerably, especially those associated with the well. These findings are consistent with those from other hazard studies on storage in salt caverns. The causes (probabilities of failure) and effects (modelling of leakage) together indicate that for most scenarios the risk is low when human intervention (e.g. monitoring of the well) is assumed. Notwithstanding our conclusion that the risk of leakage associated with gas oil injection and storage in salt caverns is low, an extensive monitoring plan should be formulated to monitor the containment of the gas oil in the storage system and its long-term stability, to ensure timely human intervention that reduces the risk considerably

[1]  J. Bear Dynamics of Fluids in Porous Media , 1975 .

[2]  J. Gerritse,et al.  Contaminant Behaviour of Micro‐Organics in Groundwater , 2009 .

[3]  Erik Lebret,et al.  The use of expert elicitation in environmental health impact assessment: a seven step procedure , 2010, Environmental health : a global access science source.

[4]  R. A. Chadwick,et al.  Underground gas storage : worldwide experiences and future development in the UK and Europe , 2009 .

[5]  Fabien Magri,et al.  Deep geothermal groundwater flow in the Seferihisar–Balçova area, Turkey: results from transient numerical simulations of coupled fluid flow and heat transport processes , 2010 .

[6]  Mark D. White,et al.  Modeling fluid flow and transport in variably saturated porous media with the STOMP simulator. 2. Verification and validation exercises , 1995 .

[7]  Brent Miyazaki,et al.  Well integrity: An overlooked source of risk and liability for underground natural gas storage. Lessons learned from incidents in the USA , 2009 .

[8]  R. Lenhard,et al.  Measurement and prediction of saturation-pressure relationships in three-phase porous media systems , 1987 .

[9]  Jack C. Parker,et al.  Multiphase flow with a simplified model for oil entrapment , 1992 .

[10]  Y. Mualem A New Model for Predicting the Hydraulic Conductivity , 1976 .

[11]  Pierre Berest,et al.  Safety of salt caverns used for underground storage: Blow out; mechanical instability; seepage; cavern abandonment , 2003 .

[12]  M. Thiercelin,et al.  Evaluation of Cement Systems for Oil and Gas Well Zonal Isolation in a Full-Scale Annular Geometry , 2005 .

[13]  Van Genuchten,et al.  A closed-form equation for predicting the hydraulic conductivity of unsaturated soils , 1980 .

[14]  Marc Thiercelin,et al.  Evaluation of Cement Systems for Oil and Gas Well Zonal Isolation in a Full-Scale Annular Geometry , 2005 .

[15]  D. Hendriks,et al.  Groundwater impact on environmental flow needs of streams in sandy catchments in the Netherlands , 2014 .

[16]  B. Kutchko,et al.  Degradation of well cement by CO2 under geologic sequestration conditions. , 2007, Environmental science & technology.

[17]  E. Kreft,et al.  Chapter 33 – Risk Assessment Methodology for CO2 Storage: The Scenario Approach , 2005 .

[18]  Michael A. Celia,et al.  Spatial characterization of the location of potentially leaky wells penetrating a deep saline aquifer in a mature sedimentary basin , 2004 .

[19]  Manuel Nepveu,et al.  FEP Analysis and Markov Chains , 2009 .

[20]  Martin O. Saar,et al.  Review: Geothermal heat as a tracer of large-scale groundwater flow and as a means to determine permeability fields , 2011 .

[21]  J. Mas-Pla,et al.  Hydrogeological interactions between fault zones and alluvial aquifers in regional flow systems , 2008 .

[22]  M. Person,et al.  Faults as conduit‐barrier systems to fluid flow in siliciclastic sedimentary aquifers , 2006 .

[23]  F. C. Dufour Grondwater in Nederland : Onzichtbaar water waarop wij lopen , 1998 .

[24]  Pierre Berest,et al.  Tightness Tests in Salt-Cavern Wells , 2001 .

[25]  T. Aigner,et al.  Production from Muschelkalk carbonates (Triassic, NE Netherlands): unique play or overlooked opportunity? , 2005 .

[26]  Mark D. White,et al.  Modeling fluid flow and transport in variably saturated porous media with the STOMP simulator. 1. Nonvolatile three-phase model description , 1995 .

[27]  H. Simmelink,et al.  Geodynamic and hydrodynamic evolution of the Broad Fourteens Basin (The Netherlands) in relation to its petroleum systems , 2002 .

[28]  G. O. Oude Essink,et al.  Fluid flow in the northern Broad Fourteens Basin during Late Cretaceous inversion , 2003, Netherlands Journal of Geosciences - Geologie en Mijnbouw.

[29]  S. Bachu,et al.  Review of integrity of existing wells in relation to CO2 geological storage: What do we know? , 2011 .