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Shale Gas Dr HM Schulz

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Shale Gas Dr HM Schulz
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Shale Gas: H.-M. Schulz SS 2013 1 13th - 14th of June 2013 Shale Gas Hans-Martin Schulz The Key Factor for Production: Mineralogy best Barnett Shale production comes from zones with 45% quartz and only 27% clay brittleness controls frac stimulation
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  • Shale Gas: H.-M. Schulz SS 2013

    1

    13th - 14th of June 2013

    Shale Gas

    Hans-Martin Schulz

    TheKeyFactorforProduction:MineralogybestBarnettShaleproductioncomesfrom

    zoneswith45%quartzandonly27%claybrittlenesscontrolsfrac stimulation

  • Shale Gas: H.-M. Schulz SS 2013

    2

    ! Shale gas is self-contained HC system !

    Total Organic Carbon (wt%)- Heterogeneities -

    0 4 8 12 16

    80

    60

    40

    20

    Dep

    th (m

    )

    TOC (%)

    0 2 4 6 8 10 12TOC (Wt%)

    0

    50

    100

    150 compare,Barnett Shale

    Courtesy Brian Horsfield (2011)

    Mesozoic black shale:different coloursIndicate different wells

  • Shale Gas: H.-M. Schulz SS 2013

    3

    Methane in gas shales is stored

    Fractureporositymatrix porosity

    (blue)

    asfreegas

    on the surface of clay minerals

    insorbedstate

    on the surface ofthe organic fraction

    +dissolvedmetha

    ne+

    dissolvedmetha

    ne

    Fracture gasis produced immediatelyAdsorbed gasis released dueto pressure declines

  • Shale Gas: H.-M. Schulz SS 2013

    4

    Processes in a source rock leading to oil, gas, andcarbon-rich residue (pyrobitumen)

    High-maturity shale-gas systems derive high gas contentsfrom the indigenous generation of gas from kerogen, bitumen, and oil cracking.

    Jarvie et al. (2007): Unconventional shale-gas systems: The Mississippian Barnett Shale of north-central Texas as one model for thermogenic shale-gas assessment AAPG Bulletin, v. 91, no. 4 (April 2007), pp. 475499

    Gas Content vs. TOC in Two Shale Gas Plays Implication:Gas Associated with Organic Matter

    Courtesy A. Aplin (2011)

  • Shale Gas: H.-M. Schulz SS 2013

    5

    Sorbed CH4 Increases with Pressure and Amountof Organic Matter

    Increasing TOC

    Methane adsorption isotherms, Antrim shale, Michigan BasinCourtesy A. Aplin (2011)

    ^^

    .but CH4 Sorption Decreases with Temperature

    Data for Dietz Coal

    Bustin and Bustin (2008)

    Courtesy A. Aplin (2011)

  • Shale Gas: H.-M. Schulz SS 2013

    6

  • Shale Gas: H.-M. Schulz SS 2013

    7

    Typical sorption isotherm

    Bob Cluff (2006)

  • Shale Gas: H.-M. Schulz SS 2013

    8

    How Much of the Porosity is Associated with Organic Matter?

    Passey et al. (2010)

    Loucks et al. (2011): Origin and Classification of Pores in Mudstones from Shale-Gas Systems. Search and Discovery Article #40855

  • Shale Gas: H.-M. Schulz SS 2013

    9

    Loucks et al. (2011): Origin and Classification of Pores in Mudstones from Shale-Gas Systems. Search and Discovery Article #40855

    Dark grey:organic matter

    Grey: mineral matrix


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