Gamma Ray and Gamma Ray Absorption Logs

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    Units

    Decayratesan a i e

    Naturalgammaradiationasshaleindicator

    Gammarayabsorption

    Elasticandinelasticneutronscattering

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    GammaRay

    and

    GammaRa Absor tion

    Logs

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    BassiouniCh.7GammaRayLog

    BassiouniCh.8GammaRayAbsorptionLogs

    Liu,C(Richard),UH(API)NuclearLoggingCalibrationFacilityPowerPointpresentation

    J.S.WahllJ.TittmanlC,W.Johnstone,TheDualSpacingFormationDensityLog,,JPT1964

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    .

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    Detectors

    GeigerMuellertube

    Proportionalcounter

    ScintillationcounterThalliumiodidedopant

    em ts or ue g t

    Fastandefficient

    byspring

    raysscattermultiple

    timesscatterbefore

    reachingthedetector

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    AveragingEffectson

    ApparentGammaRayIntensity

    Electronicaveragingindetector

    Loggingspee

    Toollength

    Othernecessarycorrections

    Eccentricity

    as ngan cemen presen

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    AveragingofStatisticalVariations

    andEffectonLoggingSpeed

    decay

    statisticalvariationhasnothingtodowith

    formationevaluation

    Toproduceaninterpretablelog,weaverageoutthestatisticalvariationselectronically

    Theelectronicaveraginghasasideeffectonloggingspeed

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    Open

    Circuit,i.e.,

    Pulses

    veryhigh

    impedance

    single-charge pulses per secondJ

    e ec r c c arge

    inI JQ

    VI

    At steady state soin out

    RI I

    V JQR

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    imposesanupperlimitonloggingspeed

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    ShaleEstimation shmin

    from

    GammaRa Lo s

    logAssumethelog

    ,

    correctionforknown

    effects,islinearly

    proportionaltothe

    amountofshale

    log min

    min

    sh

    sh

    I

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    or

    itcou come romsan stone orot er roc s

    withunusuallyhighamountsofradioactivem nera s euran um.

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    energyaswell

    Approximationschemeforquick

    calculationof

    elementallogs

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    Assumetotal

    response sa

    linear

    superposition

    Th,U,K

    Also

    GRS=Th+K=

    uran um ree

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    Inbothsandstone

    andshale

    Wewouldnaively

    interpretasshale

    wou n we~3Xinshales

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    RuleofThumbCalculation

    ofSpectralComponents

    For Schlumber er devices

    (API units) 4 ( ) 8 ( ) 16 (% )Th U K C ppm C ppm C wt

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    ActivesourceofgammaraysCs137 orCo60

    U timate ywe etectgammaraya sorption

    bythephotoelectriceffectwhichdependsont enum ero ava a ee ectrons

    0e peN xI I e

    number of electrons per unit volume

    cross section for hotoelectric effect

    e

    where

    N

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    path

    effects

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    somewhatfor

    MudcakeThickness

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