2006
DOI: 10.1190/1.2360619
|View full text |Cite
|
Sign up to set email alerts
|

The Atzbach-Schwanenstadt gas field—a potential site for onshore CO2 storage and EGR

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
2

Citation Types

0
10
0

Year Published

2009
2009
2021
2021

Publication Types

Select...
4
1

Relationship

1
4

Authors

Journals

citations
Cited by 7 publications
(10 citation statements)
references
References 0 publications
0
10
0
Order By: Relevance
“…Moreover, autochthonous fine-grained material from pelagic background sedimentation is included in the fine-grained endmembers of turbidites. These sediments act as potential source rock for bacterial methane as well as the more than 500 m thick overburden (lithostratigraphically A1-A3, Malzer et al, 1993) which is also the seal for the gas field (Polak et al, 2006).…”
Section: Geological Frameworkmentioning
confidence: 99%
See 2 more Smart Citations
“…Moreover, autochthonous fine-grained material from pelagic background sedimentation is included in the fine-grained endmembers of turbidites. These sediments act as potential source rock for bacterial methane as well as the more than 500 m thick overburden (lithostratigraphically A1-A3, Malzer et al, 1993) which is also the seal for the gas field (Polak et al, 2006).…”
Section: Geological Frameworkmentioning
confidence: 99%
“…Up to now, several aspects regarding reservoir modelling, baseline monitoring etc. have been analysed (Polak et al, 2006).…”
Section: Geological Frameworkmentioning
confidence: 99%
See 1 more Smart Citation
“…Reservoir simulations carried out in these models allowed to evaluate the feasibility of an injection at 0.3 Mt CO 2 /year for thirty years, starting from 2010, with and without EGR, and considering also new wells. The other project target was to investigate the effect of CO 2 injection on the mechanical stability of the site, and the risk for CO 2 migration to the groundwater or the atmosphere and the possibility of detecting CO 2 in such cases [ Polak et al , 2006]. This was guaranteed by soil gas measurements to provide background data for comparison to future soil gas monitoring, a feasibility study to assess the possibilities for seismic monitoring though the years, geochemical experiments and simulations to evaluate the effect of CO 2 ‐rich brine on the reservoir seal, and finally, geomechanical experiments and simulations to assess the mechanical stability of the site [ Polak et al , 2006; Le Thiez et al , 2009].…”
Section: Application To the Atzbach‐schwanenstadt Injection Sitementioning
confidence: 99%
“…The reservoir sandstone intervals, approximately 1600 m below the surface, were formed in the Puchkirchen Basin, a deep water trough parallel to the Alpine front. The geological model (Figure 4b) has been built on the basis of seismic interpretation, geological knowledge, and well log data [ Polak et al , 2006], including the topographic surface and one low velocity layer to simulate the overburden.…”
Section: Application To the Atzbach‐schwanenstadt Injection Sitementioning
confidence: 99%