Analysis of potential leakage pathways at the Cranfield, MS, U.S.A., CO2 sequestration site

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Abstract

A 1.5-million-ton CO2 sequestration project took place in a 3000-m-deep historical oilfield, combined with a CO2-EOR flood. The Cranfield reservoir is found within a multikilometer domal structure related to a deep-salt diapir and consists of fluvial sediments of the Tuscaloosa Formation. An earlier analysis determined that plugged and abandoned wells provide the most likely leakage pathways to aquifers and potentially to the ground surface. Fourteen Cement Bond Logs (CBL's) were used to assess the risk. The present quality of the cement bond ranges from excellent to poor.

Geological insights, stochastic numerical modeling of the pressure field, analysis of the CBL's, and application of a wellbore flow model were used to conclude that the limited pressure increase and mostly intact wellbores result in a low CO2- and brine-leakage risk. Statistical estimates of well properties suggest that at most two (and possibly none) could be capable of conveying a total of 1800 kg/yr CO2 to the surface (0.0002% of annual injection rate). Given that the oilfield is an active operation, it is improbable that well leakage to the surface will go unnoticed and certain that risks will be managed through active risk mitigation and remediation if necessary.

Highlights

► A leakage risk assessment was performed at the CO2-EOR Cranfield reservoir. ► Plugged and abandoned wells are the most likely leakage pathways. ► Pressure, driving force for leakage, was determined through a numerical model. ► Wellbore permeabilities were estimated with the help of cement bond logs. ► Potential leakage rates are small and of little concern.

Introduction

A risk assessment or analysis (RA) of processes and events that can derail an otherwise perfectly planned enterprise is often undertaken before the launching of any large industrial endeavor. Developing an enhanced oil recovery (EOR) operation to extract some of the remaining oil from a depleted oil reservoir that has historically produced is no different. When Denbury Onshore, LLC from Plano, TX (the operator), made the decision to invest in the Cranfield, Mississippi (MS), field in the mid-2000s, the operators performed standard technical, financial, and economic analysis of the project and brought with them their practical expertise, stemming from several similar operations across the southeast U.S. In agreement with Denbury and with its operational support, the site was also chosen by the Bureau of Economic Geology (BEG) to achieve some of the goals set forth by the DOE-sponsored SECARB partnership (Hovorka et al., 2013). Phase III of the collaborative project is geographically focused on the northeast section of Cranfield field. This limited section of the field has been called the HiVIT (high-volume injection test) and includes a smaller area, called the DAS (detailed area of study), on which BEG has performed many tests and research investigations (Fig. 1). The HiVIT area is the focus of this paper. There, the operator and BEG collaborated to inject 1.5 million tons of CO2 over 1.5 years (Choi et al., 2013), both within the historically determined boundaries of the field and into the downdip leg of the field, where the DAS is located.

Developing a CO2-storage operation next to a historical and active oil-production site introduces the issue of leakage through wells and prompted a risk-assessment study. However, the work presented here is not a risk assessment of the oil operation itself, which is handled by the operating company. The study followed the certification framework (CF) procedure (Oldenburg et al., 2009). CF focuses on events that are deemed the most likely to cause problems from past historical evidence, that is, wellbores and faults, as well as spill points (Fig. 2). The objective of the present analysis is to investigate the potential impact of these three categories of features on site integrity. We first describe the relevant attributes of the site and the volumes potentially impacted from the surface to the reservoir itself. We then present details of the methodology to estimate leakage potential and impacts and then apply the method to calculate risks semi-quantitatively. A discussion of the results follows that also includes likely attenuation factors limiting the negative impacts of some events.

Section snippets

Site description

The Cranfield oil and gas field is located in a rural area of southwestern Mississippi near the Louisiana border (Fig. 1). The area is heavily wooded with clearings and is moderately hilly with flat terrace areas near streams; elevations above mean sea level range from 60 to 120 m (200–400 ft). Surface drainage is provided by two small creeks. The closest large population center is Natchez (∼18,000 inhabitants) 25 km (15 miles) to the west, although isolated residences spread out over the area, and

Methodology

The approach presented in this paper follows the CF methodology (Oldenburg et al., 2009, Oldenburg et al., 2011). The CF conceptualizes the system as source, conduits and pathways (wells and faults), and compartments. It focuses on subsurface leakage risks, particularly leakage through new and historical wells, and leakage through faults. The CF is designed to be simple by (1) using a simple framework for calculating leakage risk and (2) using proxy concentrations or fluxes for quantifying

Results

Central to application of the CF for leakage-risk assessment is specification of the storage region, defined as the volume beyond which CO2 migration is considered leakage. In this study, the storage region is defined as the subsurface volume comprising the Tuscaloosa Fm. reservoir on the upthrown side of the fault. The lower boundary of the storage region consists of the uppermost confining unit of the Washita–Fredericksburg Group, in direct contact with the Tuscaloosa at depth of ∼3200 m (Fig.

Impact to compartments

From bottom to top, the compartments in the CF that are vulnerable are HMR, USDW, NSE, HS, and ECA (Fig. 2). Because the oilfield is under CO2-EOR and no other significant mineral resources are recognized in the area, we conclude that there are no potential negative impacts of CO2 on the hydrocarbon resource (HMR) at the site.

Significant USDWs in the area could be impacted if CO2 or brine were to leak up a P&A well and out of the storage region beyond the Wilcox Fm., There are 17 wells that may

Summary and conclusion

We applied the CF approach to assessment of the risk of CO2 and brine leakage from a deep reservoir to various compartments that could be impacted. The reservoir is located at a great depth (∼3050 m) in an interval of the Tuscaloosa Fm. of fluvial origin capped by a mudstone that has prevented further migration of hydrocarbon and, higher in the section, by an extensive thick marine-mudstone confining zone. The reservoir produced oil and gas from 1943 through ∼1965 and has been recently the

Acknowledgments

The authors would like to thank H. Lashgari, S. Coleman, T. Meckel, P. Jordan, A. Mazzoldi, S. Solano, C. Puerta, C. Yang, K. Romanak, and S. Hovorka for helping in the study. This work was supported by the Assistant Secretary for Fossil Energy, Office of Sequestration, Hydrogen, and Clean Coal Fuels, National Energy Technology Laboratory (NETL), and by Lawrence Berkeley National Laboratory under Department of Energy Contract No. DE-AC02-05CH11231. Additional support comes from the Bureau of

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