Symposium on the Application of Geophysics to Engineering and Environmental Problems 1998 1998
DOI: 10.4133/1.2922504
|View full text |Cite
|
Sign up to set email alerts
|

Use of Terrain Electromagnetic Geophysical Methods to Map Saline‐Water Contamination, East Poplar Oil Field, Northeastern Montana

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1

Citation Types

0
3
0

Year Published

2018
2018
2023
2023

Publication Types

Select...
4

Relationship

0
4

Authors

Journals

citations
Cited by 4 publications
(3 citation statements)
references
References 0 publications
0
3
0
Order By: Relevance
“…A conceptual model for far‐field brine leakage from a storage formation was synthesized from a number of field studies of brine leakage in analog systems to CGS (e.g., Jacobs, 2009; Keating et al., 2010, Keating, Hakala, et al., 2013; Keating, Newell, et al., 2013, 2014; Llewellyn, 2014; Thamke & Craig, 1997; Thamke & Midtlyng, 2003). In this model, a far‐field brine plume is leaking from a CO 2 storage formation (denoted as Zone 1) through fractured caprock, in turn migrating via advection and dispersion through the intermediate overburden layers (denoted as Zone 2) and eventually propagating in the shallow aquifer (denoted as Zone 3).…”
Section: Experimental Materials and Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…A conceptual model for far‐field brine leakage from a storage formation was synthesized from a number of field studies of brine leakage in analog systems to CGS (e.g., Jacobs, 2009; Keating et al., 2010, Keating, Hakala, et al., 2013; Keating, Newell, et al., 2013, 2014; Llewellyn, 2014; Thamke & Craig, 1997; Thamke & Midtlyng, 2003). In this model, a far‐field brine plume is leaking from a CO 2 storage formation (denoted as Zone 1) through fractured caprock, in turn migrating via advection and dispersion through the intermediate overburden layers (denoted as Zone 2) and eventually propagating in the shallow aquifer (denoted as Zone 3).…”
Section: Experimental Materials and Methodsmentioning
confidence: 99%
“…Due to field data paucity, Keating et al. (2010) suggested three research strategies to investigate CO 2 /brine leakage related issues: (a) relying on data from the engineered and well‐characterized CGS pilot sites, such as Frio or Ketzin sites (Doughty et al., 2008; Kharaka et al., 2006, 2009, 2013; Nowak et al., 2013; Zeidouni et al., 2014), (b) utilizing data from analog systems, such as leakage of re‐injected produced water (Jacobs, 2009; Thamke & Craig, 1997; Thamke & Midtlyng, 2003) or natural brine leakage from deep formations (Keating et al., 2010, 2014; Keating, Hakala, et al., 2013; Keating, Newell, et al., 2013; Llewellyn, 2014), and (c) generating data under controlled laboratory experiments (Agartan, 2015; Luyun et al., 2011; Trevisan et al., 2017).…”
Section: Introductionmentioning
confidence: 99%
“…The regional shallow aquifer includes Quaternary glacial deposits of Wiota gravels, Sprole silts, till, and alluvium varying in thickness (Figure S1a) and composition that overlie the Bearpaw shale bedrock (Thamke and Craigg 1997). There is a low hydraulic conductivity zone on the western portion of the Site (Jacobs 2013; Thamke and Smith 2014) because some areas where there is clay on top of shale (e.g., PNR‐16; Figure 2) have no saturated sands or gravel thickness where the aquifer pinches out.…”
Section: Introductionmentioning
confidence: 99%