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Chapter3 2012 Figures

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  • 7/30/2019 Chapter3 2012 Figures

    1/13

    Packing of uniform spheres

    Cubic packing

    least compact (f = 47%)

    Orthorhombic packing

    most compact (f = 26%)

    Diagonal

    cross-sectionFront view

    Diagonal

    cross-section

    Front view

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    Porosity relation with density

    and velocity

    Vb

    Vp

    Fluid

    Vm=Vb-Vp

    MatrixRock

    rb(f) = rff + (1-f) rm1 / ab(f) = f/af + (1-f) / ama: P-wave velocityr: Density

    f: Porosity

    b: whole rock (bulk)

    f: pore fluid

    m: solid matrix

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    Porosity Relation to Density and P-wave Velocity

    0

    1000

    2000

    3000

    4000

    5000

    6000

    0.0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1.0

    Porosity

    Den

    sity(kg/m3),P-waveVelocity(m/s)

    P-wave velocity

    Density

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    Estimation of VNMO

    After

    NMO

    True

    T-X

    High

    VNMO

    Low VNMO

    DTNMO(X) X2 / (2T0 VNMO2)

    T

    X

    T0

    Before

    NMO

    Best

    VNMO

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    Comparing velocities

    VRMS (tangent to true T2-X2

    curve at X2 = 0)T2

    X2

    True T2

    -X

    2

    curve

    Vs (best-fit line to true T2-X2

    curve )

    T

    X

    VRMS (tangent to true T2-X2

    curve at X2 = 0)

    True T-Xcurve

    Vs (best-fit hyperbola to true T-X)

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    Determination of layers interval velocity, thickness,

    and depth from true T-X data

    (1)There are three ways to find the interval velocity VN in the Nth layer given the true T-Xcurves of the top and bottom interfaces (N-1 and N):

    A.Using VS:1. Fit two separate hyperbolas to the small-offset traces of the N-1 and N th true T-X

    curves.

    2. This gives us the stacking velocities VSN-1 and VSN.3. Apply Dixs formula to calculate VN from VSN-1and VSNand T0N and T0N-1.

    B.Using VNMO:1. Perform NMO correction to the small-offset traces of the N-1 and Nth true T-X

    curves until these curves are completely horizontal.

    2. This gives us the NMO velocities VNMON-1 and VNMON.3. Apply Dixs formula to calculate VN from VNMON-1 and VNMON and T0N and T0N-1.

    C.Using VRMS:1. Fit high-order polynomials to the small-offset traces of the N-1 and Nth true T-X

    curves (e.g., fitting a 3-term polynomial: 42

    2

    10XCXCCT ++= ).

    2. Compute the RMS velocities VRMSN-1 and VRMSN C1 of the N-1 and Nth best-fitcurves.

    3. Apply Dixs formula to calculate VN from VRMSN-1 and VRMSN and T0N and T0N-1.(2)Determine the thickness of the i-th layer as: 2/

    0 iiiTVH D= , where i=1,2,,N.

    (3)Determine the depth to the bottom of the N-th layer as: =

    =

    N

    i

    iNHZ

    1

    .

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    y = 9.425E-08x + 7.080E-01

    R2

    = 9.947E-01

    y = -3.434E-16x2

    + 1.107E-07x + 6.662E-01

    R2

    = 9.994E-01

    0

    1

    2

    3

    4

    5

    6

    7

    0.0E+00 1.0E+07 2.0E+07 3.0E+07 4.0E+07 5.0E+07 6.0E+07 7.0E+07

    X22

    T2

    2

    ./3005

    10107.1

    1

    ./3257

    10425.9

    1

    72

    82

    smV

    smV

    RMS

    S

    =

    =

    =

    =

    -

    -

    Correct model parameters are:

    Layer

    (i)

    Vi

    (m/s) Hi (m) True RMS Velocity (m/s) Zi (m)

    1 2000 600 2000 600

    2 4000 400 2646 1000

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    X T(X) X/Z X2

    T2

    0 0.800 0.0 0 0.640

    49 0 .800 0.0 2390 0.640

    98 0 .801 0.0 9581 0.641

    147 0.802 0.1 21635 0.643

    197 0.803 0.1 38661 0.646

    247 0.805 0.1 60813 0.649

    297 0.808 0.1 88298 0.653

    348 0 .811 0.2 121380 0.657

    400 0 .814 0.2 160391 0.663

    454 0 .818 0.2 205741 0.669

    508 0 .823 0.3 257933 0.677

    564 0 .828 0.3 317585 0.685

    621 0 .833 0.3 385455 0.694

    680 0 .840 0.3 462474 0.705

    741 0 .847 0.4 549803 0.717

    806 0 .855 0.4 648894 0.731

    873 0 .864 0.4 761588 0.746

    944 0 .874 0.5 890256 0.764

    1019 0.88 5 0.5 1038 004 0.784

    1100 0.89 8 0.5 1208 984 0.807

    1187 0.91 3 0.6 1408 895 0.833

    1283 0.92 9 0.6 1645 788 0.864

    1390 0.94 9 0.7 1931 476 0.901

    1511 0.97 2 0.8 2284 090 0.945

    1653 1.00 1 0.8 2733 121 1.001

    1825 1.03 6 0.9 3330 301 1.074

    2044 1.08 3 1.0 4176 294 1.174

    2345 1.15 1 1.2 5499 020 1.324

    2821 1.26 1 1.4 7959 060 1.590

    3836 1 .50 4 1.9 1 471646 0 2.261

    4019 1 .54 8 2.0 1 615415 2 2.396

    4235 1 .60 0 2.1 1 793122 0 2.562

    4493 1 .66 4 2.2 2 018920 3 2.768

    4813 1 .74 2 2.4 2 316234 0 3.035

    5222 1 .84 3 2.6 2 726906 6 3.395

    5774 1 .97 9 2.9 3 333927 9 3.915

    6580 2 .17 8 3.3 4 329125 3 4.744

    7926 2 .51 2 4.0 6 281636 8 6.310

    y = 9.425E-08x + 7.080E-01

    R = 9.947E-01

    y = -3.434E-16x2 + 1.107E-07x + 6.662E-01

    R = 9.994E-01

    0

    1

    2

    3

    4

    5

    6

    7

    0.0E+00 1.0E+07 2.0E+07 3.0E+07 4.0E+07 5.0E+07 6.0E+07 7.0E+07

    T2

    2

    X22

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    CVS

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    Check-Shot Survey

    Layer 1

    (V1, H1)

    Layer 2

    (V2, H2)

    Layer 3

    (V3, H3)

    S

    R1

    R2

    R3

    Z1Z2Z3

    Z

    T

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    Vertical Seismic Profiling (VSP)

    Concept

    Layer

    (V, H)

    R1

    R2

    R3

    Z1

    Z2

    Z3

    Z

    TSX0

    Reflected

    Direct

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    Sonic Well Logging

    Tool

    Tool (sonde) used for

    conventional sonic well logging

    (after Sheriff and Geldart, 1995)


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