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UH&CSMFluid /DHI Challenges in 2020 Energy demand: 60% (?) increase CO2 emission increase: 60% (?) Hydrocarbon will be sustainable It is challenge to humanity.

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Presentation on theme: "UH&CSMFluid /DHI Challenges in 2020 Energy demand: 60% (?) increase CO2 emission increase: 60% (?) Hydrocarbon will be sustainable It is challenge to humanity."— Presentation transcript:

1 UH&CSMFluid /DHI Challenges in 2020 Energy demand: 60% (?) increase CO2 emission increase: 60% (?) Hydrocarbon will be sustainable It is challenge to humanity China has to be big part to face the challenge

2 UH&CSMFluid /DHI Technical Challenges Frontier Target Unconventional Resources More Accurate & Efficient

3 UH&CSMFluid /DHI Who will do it National or company wide effort We need team up world wide: –Opening SEG Beijing Office Basic and application research Who will do it – Consortium research? – Project research?

4 UH&CSMFluid /DHI Fluids/DHI Consortium Start 1995- now (13 years) Sponsors (24) Anadarko, BG, BHP, BP, CGGVeritas, Chevron, CNOOC, ConocoPhillips, Devon, Encana, Eni, ExxonMobil, Fugro-Jason, JOGMEC, Nexen, Paradigm, Petrobras, Petrochina, Rock Solid images, RWE, Shell, SLB, StatoilHydro, Total

5 UH&CSMFluid /DHI Seismic Rock Physics - Fluids/DHI Consortium Ceremony of Opining SEG Beijing Office April 3, 2008 Dr. De-hua Han (UH), Dr. M. Batzle (CSM) Manika Prasad (CSM)

6 UH&CSMFluid /DHI King Kong vs. Lisa Anne (O’Brien, 2004) Green Canyon, GOM Plio-Pleistocene Target TVD 11800ft, OB 4100ft Wiggles Rock & Fluid “Local Calibration” GasFizz

7 UH&CSMFluid /DHI Rock Physics Seismic Attributes Reservoir Geology Rock and fluid Properties & models Time, Amp., AVO Spectrum Decom. (T, A, F) Deposition, Structure Compact. & cement. Seismic Rock Physics

8 UH&CSMFluid /DHI S =  K/Ms MdMd Flui d P-wave modulus:

9 UH&CSMFluid /DHI Phase Behavior

10 UH&CSMFluid /DHI 400 600 800 1030507090110 Temperature (c) Velocity (m/s) 15 20 28 35 41 MPa HEAVY GAS COMPRESSIONAL VELOCITY Gas property

11 UH&CSMFluid /DHI Calculated Velocities Using G vseu (API = 48.27) Oil model Gas model Gseu as input Gas model G as input Gas model Gvseu as input Gas model Gvseu as input Data

12 UH&CSMFluid /DHI Calculated Vs vs. Temperature ( API = 9.38)

13 UH&CSMFluid /DHI Sandstone trend

14 UH&CSMFluid /DHI Vuggy model Micro model mm  vug Carbonate Trend

15 UH&CSMFluid /DHI Heavy Oil Sands Figure 16. Heavy oil sands: potential variation of oil and sand structure.

16 UH&CSMFluid /DHI Temperature effect Figure 13. Summarize all (15) the Vp data versus temperature Liquid P.

17 UH&CSMFluid /DHI

18 UH&CSMFluid /DHI Guest Molecules Water Molecules STRUCTURE I STRUCTURE II STRUCTURE H STRUCTURE I Gas Hydrate Crystal Structures

19 UH&CSMFluid /DHI Sand and Shale Compaction

20 UH&CSMFluid /DHI Fluid Property

21 UH&CSMFluid /DHI AVO Response

22 UH&CSMFluid /DHI  Case Study Beijing Sichuan Basin Southwest China Frequency (%) Thickness (m)  100 K: <1mD Target zone: around 2500m Delta-plain dominated with braided channels

23 UH&CSMFluid /DHI Thickness

24 UH&CSMFluid /DHI FLUID TERM VOLUME GAS FIZZ? WATER

25 UH&CSMFluid /DHI Fluid modulus Inverted fluid bulk modulus using Lisa anne well information KingKong GPa

26 UH&CSMFluid /DHI AVO Response Initial P.

27 UH&CSMFluid /DHI De-hua Han: dhan@uh.edu Dr. M. Batzle: mbatzle@mines.edu Thanks


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