2018
DOI: 10.1007/s00603-018-1521-2
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Evaluating Micro-Seismic Events Triggered by Reservoir Operations at the Geothermal Site of Groß Schönebeck (Germany)

Abstract: Rock Mechanics and Rock Engineering manuscript No.

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Cited by 36 publications
(23 citation statements)
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References 47 publications
(56 reference statements)
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“…The maximum fluid pressure should be maintained below the critical effective stress state for fault activation. This can be estimated from slip tendency analysis of nearby faults (e.g., Blöcher et al 2018). If the confidence on in situ stress state and fault geometries is low, it is recommended to apply the lowest possible pressures that lead to a stimulation effect and to avoid excessive overpressures.…”
Section: Low Pressuresmentioning
confidence: 99%
“…The maximum fluid pressure should be maintained below the critical effective stress state for fault activation. This can be estimated from slip tendency analysis of nearby faults (e.g., Blöcher et al 2018). If the confidence on in situ stress state and fault geometries is low, it is recommended to apply the lowest possible pressures that lead to a stimulation effect and to avoid excessive overpressures.…”
Section: Low Pressuresmentioning
confidence: 99%
“…Break the core and recover it to the surface sufficient for the stress magnitude determination if (1) the rock is homogeneous and linearly viscoelastic, (2) the viscoelasticity of the rock can be characterized by one viscoelastic parameter, (3) Poisson's ratio is not time-dependent, (4) the in situ stresses are removed instantaneously. In case of transversely isotropic cores, at least one additional viscoelastic parameter is required (Blanton 1983).…”
Section: Tests On Core Samples In Laboratorymentioning
confidence: 99%
“…Other examples of induced seismicity that affected commercial activities are the stoppage of gas production in the Groningen field (NOS: Nederlandse Omroep Stichting 2019) and repeated stoppages of hydraulic fracture stimulation conducted for shale gas production near Blackpool in the United Kingdom (Clarke et al 2014;Hicks et al 2019). In terms of mitigating these kinds of induced hazards, knowledge of 3-D stress state is required to estimate how far it is from a given failure criterion (Blöcher et al 2018;Morris et al 1996). The distance between the stress state and failure indicates how much stress changes are permitted due to induced or natural processes before reactivation of pre-existing faults or creation of new fractures occurs (Morris et al 1996;Schoenball et al 2018;Walsh and Zoback 2016).…”
Section: Introductionmentioning
confidence: 99%
“…Uncontrollable subsurface parameters include the initial state of stress and pore pressure, size and density of pre-existing faults/fractures, fault/fracture orientation and shear strength, and other geomechanics parameters [55]. Figure 5 shows the effect of the pressure increase on the fault reactivation in the deep doublet geothermal Groß Schönebeck project in the North German Basin, where fluid-injection-induced seismicity is recorded [56]. The stress state at the injection depth of 4035 m is a normal faulting regime with S v = 100 MPa, S Hmax = 98 MPa, S hmin = 55 MPa, and P p = 43 MPa [56].…”
Section: δSmentioning
confidence: 99%