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List of Tables2.1 Interval velocities for SW Hub Conceptual model 2 . . . . . . . . . . . . . . . . . . 222.2 Interval velocities for Gippsland Conceptual model . . . . . . . . . . . . . . . . . . . 284.1 Survey parameters used for finite difference modelling of seismic responses for <strong>the</strong>SW Hub model . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 554.2 Dimensions of CO 2 plumes modelled for SW Hub Conceptual model 2 . . . . . . . . 614.3 Dimensions of CO 2 plumes modelled at Gippsland . . . . . . . . . . . . . . . . . . . 674.4 Advantages and disadvantages of frequency and domains in electromagnetic prospecting. 814.5 Parameter variation for separated borehole modelling study . . . . . . . . . . . . . . 904.6 Target size variation in mCSEM study . . . . . . . . . . . . . . . . . . . . . . . . . 1034.7 LOTEM Gate parameters . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1134.8 Typical densities of aquifer rocks . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1184.9 Micro seismicity location techniques . . . . . . . . . . . . . . . . . . . . . . . . . . 1225.1 Two general M&V programs . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1295.2 Suitability of geophysical methods for CO 2 monitoring and verification . . . . . . . . 131A.1 Rock physics parameters used for <strong>the</strong> Lesueur group . . . . . . . . . . . . . . . . . . A 1D.1 Geophysical codes used in this project . . . . . . . . . . . . . . . . . . . . . . . . . D 1E.1 Report responsibility by section . . . . . . . . . . . . . . . . . . . . . . . . . . . . . E 1| xi
Page 1 and 2: www.csiro.auA deployment strategy f
Page 3: Response to referee’s commentsThi
Page 6 and 7: This project identified the followi
Page 8: 4.2.3 Marine electromagnetics . . .
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Page 18 and 19: and Hoversten, 2006, 2005; Wells et
Page 20: Fundamentally, CO 2 detectability i
Page 24 and 25: which rises. Eke et al. (2011) reco
Page 26 and 27: • Rock physics uncertainties are
Page 28 and 29: 2.1 South West Hub CCS ProjectThe S
Page 30 and 31: 2.1.2 Data reviewPublically-availab
Page 32 and 33: GSWA Record 2004/8Gravity and magne
Page 34 and 35: −32˚30'115˚30'116˚00'−32˚30
Page 36 and 37: 0cdp100 200 300 400 500 600 700 800
Page 38 and 39: W
Page 40 and 41: Figure 2.12: The Seaspray depressio
Page 42 and 43: 2.2.2 Data reviewAs might be expect
Page 45 and 46: 0South-WestNorth-East2depth (km)46F
Page 47 and 48: 3 Rock physics relationshipsNo exta
Page 49 and 50: For the reservoir member a porosity
Page 51 and 52: 3.1.2 Clean sandstone modelThe foll
Page 53 and 54: 3.2 Electrical propertiesThe model
Page 55 and 56: 300Lesueur project GEMTIP Rock phys
Page 57 and 58: 4 Geophysical remote sensing techni
Page 59 and 60: 0500100021.81.61.4 T (ms) 150
Page 61 and 62: 108A S/A N64202000 2100 2200 2300 2
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Figure 4.5: The seismic lines super
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4.1.2 Data processingThe end goal o
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4.1.3 1D Reflection seismicsSeismic
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the detectability of CO 2 when only
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4.1.4 2D Reflection seismicsModelli
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(a) Baseline velocity model(b) Velo
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(a) Baseline and 2.5% CO 2 saturati
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• ρ = 2.497g/cm 3 .This gives th
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!me$(ms)$Figure 4.17: Noise-free ba
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CDP0400 time (ms)800120016002
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5004504000.64kt1.59kt3.18kt6.37kt12
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010020040060080014000.116001800N ra
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Figure 4.27: Zoomed in synthetic ba
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Figure 4.30: Zoomed view of the inj
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4.1.6 Permanent receiver installati
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Figure 4.33: Well 6, Zero-offset (1
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4.1.6.2 Ocean bottom cablesFor mari
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4.2 Electromagnetic surveying & int
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• Clearly, the induction monitori
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Key points to consider for applicat
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4.2.2.1 Single-borehole electromagn
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4.2.2.2 Separated-borehole electrom
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The second and third examples of cr
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0 A 100 m 50010001500 2000 250010
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0Wonnerup, 1000 m target; Tx 1200m
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Downloaded 23 Sep 2010 to 130.116.1
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ceiver offset from the transmitter
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Figure 4.50: Dependence of mCSEM re
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The second variation of Figure 4.48
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0 A EE Component0B E Z Component0 C
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The third variation of Figure 4.48
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0 A EE Component0B E Z Component0 C
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4.2.4 Ground electromagneticsThe mC
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Table 4.7: LOTEM Gate parameters. T
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Response Background1.0101.0051.000
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Response Background1.101.051.000.9
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Primary Industries, 2011). However,
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Effect of drill hole offset0DDH10DD
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Microseismic monitoring ideally beg
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ferromagnetic magnet which has a te
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5 Monitoring & verification strateg
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5.1 General recommendations & strat
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Table 5.2: Suitability of geophysic
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confused with seepage. In this case
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6 ConclusionsThis report has discus
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7 Recommendations for future resear
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ReferencesAl-Ali, Z. A., M. H. Al-B
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Du, J., D. L. Tilbrook, J. C. Macfa
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JafarGandomi, A., and A. Curtis, 20
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Schilling, F., G. Borm, H. Würdema
Page 163 and 164:
Yan, W., S. Huang, and E. H. Stenby
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ACO 2 PropertiesThis Appendix gives
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BSeismic preprocessing workflowThe
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CSeismic data processing for quanti
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Preprocessing prior to any stack wi
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Recent developments, such as target
Page 175 and 176:
and should not be used for quantita
Page 177 and 178:
DGeophysical software used in the p
Page 179:
EProject detailsThis section lists
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