University of Vienna

18
Numerical study of acoustic waves around and inside an underground cavity CTBTO Young Scientist Research Award 2014 WWTF project 2015 Sofi Esterhazy , Ilaria Perugia, Joachim Sch¨ oberl, G¨ otz Bokelmann

Transcript of University of Vienna

  • Numerical study of acoustic wavesaround and inside an underground cavity

    CTBTO Young Scientist Research Award 2014

    WWTF project 2015

    Sofi Esterhazy, Ilaria Perugia, Joachim Schoberl, Gotz Bokelmann

  • Wave animation

    Scattered wave field Zoom

    Sofi Esterhazy University of Vienna 2 / 13

  • Objectives

    Contribution to the scientific groundwork for OSI

    Numerical investigation

    Development of new method for elastic-acoustic problemsImprovement of computational algorithms

    Applied investigation

    Define characteristics of wave field interactionsImprove and design methods and experiments

    Sofi Esterhazy University of Vienna 3 / 13

  • On-Site Inspection

    Launch Pre-Inspection Inspection Post-InspectionRequest of OSI

    Equipment - Training/Field tests - OSI Action Plan

    Techniques IFE08 IFE14 Techniques IFE08 IFE14

    Visual Observations Environmental measurements

    Seismological aftershock monitoring Electrical conductivity measurements

    Gamma radiation monitoring Air-borne gamma spectroscopy

    Magnetic field mapping Active seismic survey

    Gravitational field mapping Resonance seismometry

    Multi-spectral imaging Drilling

    Argon-37 and radioxenonmeasurement

    Key: Tested, Partly tested, Not tested

    Sofi Esterhazy University of Vienna 4 / 13

  • Seismic Methods

    Subsurface structure after an UNE

    (Adushkin

    &Spivak,2004)

    !"# $"#

    Simplified model

    2

    1

    ?

    Sources:

    Passive seismic sources: Body waves, Surface waves, Noise

    Active seismic sources: Vibroseis, Explosions

    Sofi Esterhazy University of Vienna 5 / 13

  • Underling physics

    Acoustic wave equation in medium 1 2

    1

    ?

    Elastic wave equation in medium 2

    Focus on compressional waves

    Time harmonic cases:

    Spherical point source?

    Plane wave sources

    Sofi Esterhazy University of Vienna 6 / 13

  • Underling physics

    Acoustic wave equation in medium 1 2

    1

    ?

    Elastic wave equation in medium 2 Focus on compressional waves

    Time harmonic cases:

    Spherical point source?

    Plane wave sources

    Sofi Esterhazy University of Vienna 6 / 13

  • In/Out Scattering

    Separation into the incident and scattered wave field:

    p = pinc + pscat

    pinc

    pscat

    Better inside to the wave field interaction

    Sofi Esterhazy University of Vienna 7 / 13

  • Numerical results (1)

    Scattered wave field from a plane wavefrom the bottom left with f = 16Hz

    Cavity at depth D = 600m and diameter d = 60m

    Material parameters:v1 = 300m/s, 1 = 1kg/m

    3

    v2 = 3000m/s, 2 = 1000kg/m3 Incident wave field

    Without Cavity With cavity

    Sofi Esterhazy University of Vienna 8 / 13

  • Numerical results (1)

    Scattered wave field from a plane wavefrom the bottom left with f = 16Hz

    Cavity at depth D = 600m and diameter d = 60m

    Material parameters:v1 = 300m/s, 1 = 1kg/m

    3

    v2 = 3000m/s, 2 = 1000kg/m3

    Netgen/Ngsolve

    Automatic 2D/3D adap-tive mesh generator

    High-order Finite Element Method Applicable for Heat-flow, Acous-

    tics, Elasticity, Navier-Stokes,Maxwell, etc.

    Open-source, C++, MPI parallel,Python Plugin

    Without Cavity With cavity

    Sofi Esterhazy University of Vienna 8 / 13

  • Numerical Results (2)

    Scattering profile

    No surface

    Total field Scattered field

    Geometrywith PML

    Plane wave from the bottom with f = 16Hz

    Cavity at depth D = 600m and diameter d = 60m

    Material parameters:v1 = 3000m/s, 1 = 1000kg/m

    3, v2 = 300m/s, 2 = 1kg/m3

    kR = 1

    Sofi Esterhazy University of Vienna 9 / 13

  • Numerical Results (2)

    Scattering profile

    No surface

    Total field Scattered field

    Zoom

    Plane wave from the bottom with f = 16Hz

    Cavity at depth D = 600m and diameter d = 60m

    Material parameters:v1 = 3000m/s, 1 = 1000kg/m

    3, v2 = 300m/s, 2 = 1kg/m3

    kR = 1

    Sofi Esterhazy University of Vienna 9 / 13

  • Analytic Approach (Felix M. Schneider)

    Express the incident and the scattered wave field by linearcombinations of spherical vectors and solve a system of linearequations

    For each index l find the coefficients to match at the boundary r = R

    Sofi Esterhazy University of Vienna 10 / 13

  • Scattering cross sections(Valeri Korneev, Geophys. J. Int. (1993))

    S = Ein/Escat . . . Ratio between scattered and incoming energy flow

    kR = U/ . . . Ratio between cavity circumference and incident wavelength

    Vacuum inclusion Acoustic inclusion

    Modeling the cavity as an acoustic inclusion is crucial to resonanceseismometry

    Sofi Esterhazy University of Vienna 11 / 13

  • Summary & Outlook

    Project distinguished by the Young Scientists Research Award

    Wave propagation with focus on acoustic case

    Identification of underlying physics

    Investigation of characteristics (analytically and numerically)

    Set up of an efficient numerical code

    Extension to full elastic wave field

    Extension to 3D

    Numerical improvement and Post-processing

    Incorporation of our findings into the practices of an OSI

    Thank you!

    Sofi Esterhazy University of Vienna 12 / 13

  • Summary & Outlook

    Project distinguished by the Young Scientists Research Award

    Wave propagation with focus on acoustic case

    Identification of underlying physics

    Investigation of characteristics (analytically and numerically)

    Set up of an efficient numerical code

    Extension to full elastic wave field

    Extension to 3D

    Numerical improvement and Post-processing

    Incorporation of our findings into the practices of an OSI

    Thank you!

    Sofi Esterhazy University of Vienna 12 / 13

  • In/Out Separation

    Ansatz p = pinc + pscat

    pinc solves

    2pinc + k1pinc = (x x0) + rad. cond. for x x0

    The remaining unknown pscat is then the solution of

    (

    1

    1pscat

    )+

    k11

    pscat = 0 in 2

    (

    1

    2pscat

    )+

    k22

    pscat =1

    2(k1 k2)pinc in 1

    pscat = pinc on

    + radiation condition for r

    Sofi Esterhazy University of Vienna 12 / 13

  • Numerical method

    High-Order Finite Element Method

    Can handle highly complex, irregularly shaped geometriesTends to exponentially increase the accuracy of the computations

    Software

    Netgen: Automatic 2D/3D tetrahedral adaptive mesh generatorNgsolve: Applicable for Heat-flow, Acoustics, Elasticity,Navier-Stokes, Maxwell, etc.Open-source, C++, MPI parallel, Python Plugin

    Hardware

    Internal server with 48 coresVienna Scientific Cluster 3 - 140/2020 dual nodes a 8 cores

    Sofi Esterhazy University of Vienna 13 / 13

    ObjectivesApproachResults