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M-OSRP: objectives, strategy and game-changing delivery Recent advances to on-shore, ocean bottom and towed streamer preprocessing for deghosting and ground roll removal Jing Wu and Arthur B. Weglein University of Houston February 7, 2017
General theory of Greenβs theorem wave separation Sβ π π π = π $ + π ) π β ' + π ) π» & ' = π $ π» & P 2 π π ' β π» & ' πΌβ²π 6 π π ) π β, π = 2 ππΌβ²π» & 8ππβ² ; < ' : Causal Greenβs function in the homogeneous whole world π» & 30
Marine experiment Air F.S. Water M.S.(Cable) O.B. Earth F.S. free surface, or air/water boundary O.B. ocean bottom M.S. measurement surface 31
Homogeneous whole-space of water Water 32
π π : Air gun Water π π 33
π π : Air perturbation π π Air F.S. Water π π 34
π π : Earth perturbation π π Air F.S. Water π π O.B. π π Earth 35
Predict a portion of total wave at π β contributed by π π Sβ π π Air F.S. Water π π π β O.B. π π Earth 36
Predict a portion of total wave at π β contributed by π π Sβ π π Air F.S. Water π π π β Up O.B. π π Earth 37
Predict a portion of total wave at π β contributed by π π Sβ π π Air F.S. Down Water π π π β Down Up O.B. π π Earth 38
Predict deghosted data at π β contributed by π π Sβ π π Air F.S. Water π π π β Deghosted O.B. π π Earth 39
Predict deghosted data at π β contributed by π π π π Air F.S. Water π π π β Sβ Deghosted O.B. π π Earth 40
Predict deghosted data at π β contributed by π π π π Air F.S. Water π π π β Sβ M.S.(Cable) Deghosted O.B. π π Earth π >? π ' β π» & ' πΌβ²π 6 π β, π = @ ππΌβ²π» & 8ππβ² A.C. 41
Advantage 1 π >? π ' β π» & ' πΌβ²π 6 π β, π = @ ππΌβ²π» & 8ππβ² A.C. π π Air β’ Can accommodate cable with an arbitrary shape F.S. π π ( Z. Zhang & Weglein, 2016 ) Water π β M.S.(Cable) Deghosted O.B. Earth π π 42
Advantage 1 π >? π ' β π» & ' πΌβ²π 6 π β, π = @ ππΌβ²π» & 8ππβ² A.C. π π Air β’ Can accommodate cable with an arbitrary shape F.S. π π ( Z. Zhang & Weglein, 2016 ) Water π β M.S.(Cable) Deghosted O.B. Earth π π 43
Advantage 1 π >? π ' β π» & ' πΌβ²π 6 π β, π = @ ππΌβ²π» & 8ππβ² A.C. π π Air β’ Can accommodate cable with an arbitrary shape F.S. π π ( Z. Zhang & Weglein, 2016 ) Water π β M.S.(Cable) Deghosted O.B. Earth π π 44
Advantage 1 π >? π ' β π» & ' πΌβ²π 6 π β, π = @ ππΌβ²π» & 8ππβ² A.C. π π Air β’ Can accommodate cable with an arbitrary shape F.S. π π ( Z. Zhang & Weglein, 2016 ) Water π β M.S.(Cable) Deghosted β’ Supersedes π β π E method that assumes cable O.B. Earth π π being horizontal 45
Advantage 2 π >? π ' β π» & ' πΌβ²π 6 π β, π = @ ππΌβ²π» & 8ππβ² A.C. π π Air β’ Needs no information about the βsourcesβ: F.S. π π ΓΌ wavelet, radiation pattern Water ΓΌ air property (shape and reflection at sea surface) π β ΓΌ earth property M.S.(Cable) Deghosted O.B. Earth π π 46
Advantage 2 π >? π ' β π» & ' πΌβ²π 6 π β, π = @ ππΌβ²π» & 8ππβ² A.C. π π Air β’ Needs no information about the βsourcesβ: F.S. π π ΓΌ wavelet, radiation pattern Water ΓΌ air property (shape and reflection at sea surface) π β ΓΌ earth property M.S.(Cable) Deghosted O.B. Earth π π 47
Progress v Deghosting data on a depth variable cable v Wave separation onshore for the removal of ground roll and ghosts v Deghosting data at the ocean bottom 48
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data Issue of current Greenβs theorem deghosting method π π Air F.S. π π Water π β M.S.(Cable) O.B. Earth π π 49
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data Issue of current Greenβs theorem deghosting method π π Air F.S. π π Water π β M.S.(Cable) O.B. Earth π π 50
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data Issue of current Greenβs theorem deghosting method π π Air β’ Can only output deghosted data at a depth F.S. π π above cable ( Weglein et al., 2013 ) Water π β π >? π ' β π» & M.S.(Cable) ' πΌβ²π 6 π β, π = @ ππΌβ²π» & 8ππβ² O.B. A.C. Earth π π 51
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data How to deghost the actual acquired data? π π Air β’ π β π E if cable being horizontal F.S. π π Water π β M.S.(Cable) O.B. Earth π π 52
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data How to deghost the actual acquired data? π π Air β’ π β π E if cable being horizontal F.S. π π Water β’ A new method without assuming cable being π β horizontal ( J. Wu & Weglein, 2016 ) M.S.(Cable) O.B. Earth π π 53
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data The new method π π Air Step 1: F.S. π π Water Deghost data at a depth (at E.S.) above cable πΈ ππ (output) E.S. Use current Greenβs theorem deghosting πΈ , πΈ π (input) M.S.(Cable) ( Weglein 2002, J. Zhang & Weglein 2007 ) O.B. Earth π π E.S. evaluation surface, shallower than cable 54
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data The new method π π Air Step 2: F.S. π π Water Predict deghosted data right on the cable πΈ ππ (input) E.S. Use Greenβs theorem one-way wave prediction πΈ ππ (output) M.S.(Cable) ( Weglein et al., 2011a,b, 2016 ) O.B. Earth π π 55
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data Numerical test: Model 0m F.S. 10m 40m M.S. Water 300m O.B. Earth Layer Velocity (m/s) Density (kg/m 3 ) Water 1500 1000 Earth 2500 1000 56
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data Numerical test: Model 0m F.S. 10m E.S. 25m 40m M.S. Water 300m O.B. Earth Layer Velocity (m/s) Density (kg/m 3 ) Water 1500 1000 Earth 2500 1000 57
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data E.S. Input total π at cable cable Offset/m -1000 -500 0 500 1000 0 0.2 1.0 0.5 Time/s 0.4 0 -0.5 -1.0 0.6 x105 0.8 58
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data E.S. Input total π at cable cable Offset/m -1000 -500 0 500 1000 0 0.2 1.0 0.5 Primary Time/s 0.4 0 -0.5 -1.0 0.6 x105 0.8 59
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data E.S. Input total π at cable cable Offset/m -1000 -500 0 500 1000 0 Direct 0.2 1.0 0.5 Primary Time/s 0.4 0 -0.5 -1.0 0.6 Receiver-ghost x105 0.8 60
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data E.S. Deghosted π at E.S. (Step 1) cable Offset/m -1000 -500 0 500 1000 0 0.2 1.0 0.5 Primary Time/s 0.4 0 -0.5 -1.0 0.6 x105 0.8 61
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data E.S. Input total π at cable cable Offset/m -1000 -500 0 500 1000 0 Direct 0.2 1.0 0.5 Time/s 0.4 0 -0.5 -1.0 0.6 Receiver-ghost x105 0.8 62
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data E.S. Deghosted π at E.S. (Step 1) cable Offset/m -1000 -500 0 500 1000 0 Direct 0.2 1.0 0.5 Time/s 0.4 0 -0.5 -1.0 0.6 Receiver-ghost x105 0.8 63
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data E.S. Input total π at cable cable Offset/m -1000 -500 0 500 1000 0 0.2 1.0 0.5 Primary Time/s 0.4 0 -0.5 -1.0 0.6 x105 0.8 64
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data E.S. Deghosted π at E.S. (Step 1) cable Offset/m -1000 -500 0 500 1000 0 0.2 1.0 0.5 Primary Time/s 0.4 0 -0.5 -1.0 0.6 x105 0.8 65
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data E.S. Deghosted π at cable (Step 2) cable Offset/m -1000 -500 0 500 1000 0 0.2 1.0 0.5 Primary Time/s 0.4 0 -0.5 -1.0 0.6 x105 0.8 66
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data E.S. Input total π on cable cable Offset/m -1000 -500 0 500 1000 0 Direct 0.2 1.0 0.5 Primary Time/s 0.4 0 -0.5 -1.0 0.6 Receiver-ghost x105 0.8 67
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data E.S. Deghosted π at cable (Step 2) cable Offset/m -1000 -500 0 500 1000 0 0.2 1.0 0.5 Primary Time/s 0.4 0 -0.5 -1.0 0.6 x105 0.8 68
ΓΌ Deghosting on a depth variable cable Removal of ground roll & ghost onshore Deghosting ocean bottom data Summary Step 1 Step 2 One-way wave prediction Current deghosting method output deghosted data on cable output deghosted data above cable v Provide a two-step new method to deghost actual data on the cable, and without limitation of cableβs shape. 69
Progress v Deghosting data on a depth variable cable v Wave separation onshore for the removal of ground roll and ghosts v Deghosting data at the ocean bottom 70
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Ground roll (Rayleigh wave) ( Boustani et al., Journal of Geophysics and Engineering, 2013 ) 71
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Deliverable ( J. Wu & A. Weglein, SEG 2016 ) v A new and simplified Greenβs theorem wave separation algorithm ΓΌ for onshore ground roll and ghost removal ΓΌ with a reduced data requirement ΓΌ retains effectiveness of original algorithm ( J. Wu & A. Weglein, SEG 2015 ) 72
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Marine -- Wave separation ' β π» & ' π K π ππβ² π & = @ ππ K π» & A.C. ( Weglein & Secrest 1990 ) Air Water π & : Reference wave Earth 73
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Marine -- Data requirement ' β π» & ' π K π ππβ² π & = @ ππ K π» & A.C. ( Weglein & Secrest 1990 ) Air Water π & : Reference wave Earth 74
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Marine -- Data requirement ' β π» & ' π K π ππβ² π & = @ ππ K π» & A.C. ( Weglein & Secrest 1990 ) β’ π K π was rarely measured in 1990s 75
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Marine -- Reduce data requirement ' β π» & ' π K π ππβ² π & = @ ππ K π» & A.C. ( Weglein & Secrest 1990 ) β’ π K π was rarely measured in 1990s ' = 0 along the cable β’ Reduce requirement of π K π with π» & ( Osen et al. 1998, Tan 1999 ) 76
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Onshore -- Wave separation π£ >? = @ β 6 π― & ππβ² π£ 6 π 8 6 π― & β π’ A.C. ( Weglein & Secrest 1990, J. Wu & Weglein, SEG, 2015 ) π£ >? Reflection without ground roll & receiver ghost π― & Greenβs tensor in homogenous whole-space elastic reference π― & Stress tensor of Greenβs function π£ Displacement β π’ Traction 77
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Onshore -- Wave separation ' β π» & ' πΌβ²π 6 π @ ππΌβ²π» & 8ππβ² A.C. π£ >? = @ β 6 π― & ππβ² π£ 6 π 8 6 π― & β π’ A.C. ( Weglein & Secrest 1990, J. Wu & Weglein, SEG, 2015 ) π£ >? Reflection without ground roll & receiver ghost π― & Greenβs tensor in homogenous whole-space elastic reference π― & Stress tensor of Greenβs function π£ Displacement β π’ Traction 78
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Onshore -- Wave separation π£ >? = @ β 6 π― & ππβ² π£ 6 π 8 6 π― & β π’ A.C. ( Weglein & Secrest 1990, J. Wu & Weglein, SEG, 2015 ) Not a filtering method of ground roll removal, but a wave theory based wave prediction and no damage on π£ >? 79
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Onshore -- Wave separation π£ >? = @ β 6 π― & ππβ² π£ 6 π 8 6 π― & β π’ A.C. ( Weglein & Secrest 1990, J. Wu & Weglein, SEG, 2015 ) π£ >? Reflection without ground roll & receiver ghost π― & Greenβs tensor in homogenous whole-space elastic reference π― & Stress tensor of Greenβs function π£ Displacement β π’ Traction 80
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Onshore -- Data requirement π£ >? = @ β 6 π― & ππβ² π£ 6 π 8 6 π― & β π’ A.C. ( Weglein & Secrest 1990, J. Wu & Weglein, SEG, 2015 ) π£ >? Reflection without ground roll & receiver ghost π― & Greenβs tensor in homogenous whole-space elastic reference π― & Stress tensor of Greenβs function π£ Displacement β π’ Traction 81
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Onshore -- Data requirement π£ >? = @ β 6 π― & ππβ² π£ 6 π 8 6 π― & β π’ A.C. ( Weglein & Secrest 1990, J. Wu & Weglein, SEG, 2015 ) ππ + 2ππ U π£ U π(π U π£ W + π W π£ U ) π(π U π£ E + π E π£ U ) π U π£ >? Reflection without ground roll & receiver ghost π W β = π(π U π£ W + π W π£ U ) ππ + 2ππ W π£ W π(π W π£ E + π E π£ W ) π’ π E π― & Greenβs tensor in homogenous whole-space elastic reference π(π U π£ E + π E π£ U ) π(π W π£ E + π E π£ W ) ππ + 2ππ E π£ E π― & Stress tensor of Greenβs function π=π U π£ U + π W π£ W + π E π£ E π£ Displacement β π’ Traction 82
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data The data requirement is satisfied ( J. Wu and A. Weglein, SEG 2015 ) β β’ Measure both π and π 83
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data β ) from air/earth Model -- Generate data ( π & π Air A/E boundary M.S. 100m (π£ U , π£ E ) , (π’ U , π’ E ) Earth 400m Layer P Velocity (m/s) S Velocity (m/s) Density (kg/m 3 ) 1(Air) 340 0 3 2(Top earth) 1800 1200 1500 3(Bottom earth) 4000 2500 1800 84
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Total π£ U input to the separation algorithm Offset/m -3000 -2000 -1000 0 1000 2000 3000 0 0.5 5 4 3 2 1.0 1 Time/s 0 -1 -2 -3 1.5 -4 -5 x10-12 2.0 85
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Total π£ U input to the separation algorithm Offset/m -3000 -2000 -1000 0 1000 2000 3000 Direct Direct 0 0.5 5 4 3 2 1.0 1 Time/s 0 -1 -2 -3 1.5 -4 -5 x10-12 2.0 86
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Total π£ U input to the separation algorithm Offset/m -3000 -2000 -1000 0 1000 2000 3000 0 Rayleigh Rayleigh 0.5 5 4 3 2 1.0 1 Time/s 0 -1 -2 -3 1.5 -4 -5 x10-12 2.0 87
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Total π£ U input to the separation algorithm Offset/m -3000 -2000 -1000 0 1000 2000 3000 0 Primary Primary 0.5 5 4 3 2 1.0 1 Time/s 0 -1 -2 -3 1.5 -4 -5 x10-12 2.0 88
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Total π£ U input to the separation algorithm Offset/m -3000 -2000 -1000 0 1000 2000 3000 0 Ghost Ghost 0.5 5 4 3 2 1.0 1 Time/s 0 -1 -2 -3 1.5 -4 -5 x10-12 2.0 89
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Total π£ U input to the separation algorithm Offset/m -3000 -2000 -1000 0 1000 Direct 2000 3000 0 Rayleigh Primary Ghost 0.5 5 4 3 2 1.0 1 Time/s 0 -1 -2 -3 1.5 -4 -5 x10-12 2.0 90
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Deghosted π£ U from the separation algorithm Offset/m -3000 -2000 -1000 0 1000 2000 3000 0 Primary 0.5 5 4 3 2 1.0 1 Time/s 0 -1 -2 -3 1.5 -4 -5 x10-12 2.0 91
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data The data requirement is satisfied ( J. Wu and A. Weglein, SEG 2015 ) β β’ Measure both π and π β’ Effectively separate ground roll and ghosts out, without damaging reflection data 92
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data The data requirement is satisfied ( J. Wu and A. Weglein, SEG 2015 ) β β’ Measure both π and π β’ Effectively separate ground roll and ghosts out, without damaging reflection data The data requirement is not satisfied ( J. Wu and A. Weglein, SEG 2016 ) β β’ Measure only π , but not π 93
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data 2D onshore experiment Air (πΊ U , πΊ E ) A/E boundary (π£ U , π£ E ) Earth 94
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data 2D onshore experiment -- approximation ΓΌ Vacuum/earth boundary Vacuum (πΊ U , πΊ E ) V/E boundary (π£ U , π£ E ) Earth 95
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data 2D onshore experiment -- approximation ΓΌ Vacuum/earth boundary β(π’)π(π¦ β π¦ C ) , πΊ β π’ : source wavelet ΓΌ A localized force on surface πΊ Vacuum (πΊ U , πΊ E ) V/E boundary (π£ U , π£ E ) Earth 96
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Boundary condition β(π) : source wavelet β π π π¦ β π¦ C β π¦, π¨ = 0, π = βπΊ πΊ π’ Vacuum (πΊ U , πΊ E ) V/E boundary (π£ U , π£ E ) Earth 97
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Formula simplification β(π) : source wavelet β π π π¦ β π¦ C β π¦, π¨ = 0, π = βπΊ πΊ π’ Original π£ >? (π β(π β, π C , π) = @ π£ 6 π 8 6 π― & β π’ ββ², π C , π) 6 π― & (π ββ², π β, π) ππβ² A.C. 98
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Formula simplification β(π) : source wavelet β π π π¦ β π¦ C β π¦, π¨ = 0, π = βπΊ πΊ π’ Original π£ >? (π β(π β, π C , π) = @ π£ 6 π 8 6 π― & β π’ ββ², π C , π) 6 π― & (π ββ², π β, π) ππβ² A.C. Simplified β(π) 6 π― π (π π£ >? (π 8 6 π― & ππ ^ β, π C , π) = @ π£ 6 π + πΊ C , π β, π) A.C. 99
Deghosting on a depth variable cable ΓΌ Removal of ground roll & ghost onshore Deghosting ocean bottom data Formula simplification β(π) : source wavelet β π π π¦ β π¦ C β π¦, π¨ = 0, π = βπΊ πΊ π’ Original π£ >? (π β(π β, π C , π) = @ π£ 6 π 8 6 π― & β π’ ββ², π C , π) 6 π― & (π ββ², π β, π) ππβ² A.C. Require traction everywhere along acquisition surface Simplified β(π) 6 π― π (π π£ >? (π 8 6 π― & ππ ^ β, π C , π) = @ π£ 6 π + πΊ C , π β, π) A.C. Require source wavelet 100
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