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Seismic Noise Tests: Bayou Corne, LA, USA Juan M. Lorenzo Louisiana State University Bayou Corne and environs Site 1 Site 2 Preliminary summary-analysis of seismic ... – PowerPoint PPT presentation

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1
    Seismic Noise Tests Bayou Corne, LA,
USA   Juan M. LorenzoLouisiana State
University
2
Bayou Corne and environs
Site 2
Site 1
3
Preliminary summary-analysis of seismic noise
tests at Bayou Corne, LA conducted9-22-12 to
9-23-12
  • Goal To locate aquifer sands, which could be
    charged with free gas.
  • What we know Shear-wave data indicate the tops
    of two prominent reflector bodies (A and B).
    The shallower body (top A) lies at 7-10 m below
    the surface and the deeper body (top B) at
    40-50 m below the land surface.
  • What we do not know gas content at the two
    sites.
  • What we think we know Reflector B corresponds
    to the top of aquifer sands and lies at a
    shallower depth (42 m) east of Bayou Corne than
    west of Bayou Corne ( 47 m).
  • Recommendations S-wave surveys (not sound-waves)
    will be more successful than P-wave (sound)
    surveys at imaging the shallow sand bodies in the
    area. Seismic results should be cross-checked
    with available geological and geotechnical
    information.
  • Warning (s) Buried sand bodies are likely to
    change their thickness and depth considerably
    across the area so that the two seismic borings
    shown here should not be linearly interpolated
    with complete confidence.

4
Representative shear wave (not sound wave)
dataSite 2- (Dugas Le Blanc-1 property)
Distance between source and geophones (m)
Reflector A 10 m depth
Reflector B 43 m depth
Technical note Field data are displayed with a
constant rms amplitude and using an all-pass
filter. Maximum source-receiver offset is 192 m.
Refracted SH
Love
TWTT (s)
5
Velocity-versus-depth profiles at Site 1, S of
route 70 and W of Bayou Corne (Triche-1 property)
Technical notes Velocity values, derived using
semblance velocity analysis (dashed line) help
confirm best-matched forward ray-trace models
(continuous bold line). WT marks the interpreted
top of the water table.
6
Velocity-versus-depth profiles at Site 2N of
route 70 (Dugas-Le Blanc-1 property)
Technical note Velocity values, derived using
semblance velocity analysis (dashed line) help
confirm best-matched forward ray-trace models
(continuous bold line). WT marks the interpreted
top of the water table.
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