Well log intro

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    Petrophysics,

    Connecting people

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    Well Logging

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    Well Logging

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    Log Header, containing manyinformations of Logging program,

    including :1. Logging interval2. Total depth3. Mud and filtrate resistivity

    measurement4. Elevation etc

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    Log Gamma Ray

    (Pertamina EPTC. 2011)

    (Malcolm rider. 2002)

    (Malcolm rider. 2002)

    Aplikasi log Gamma Ray (Rider. 2000) : Perhitungan Kandungan serpih Pendugaan fasies Identifikasi mineral

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    Log Densitas

    (Oberto Serra. 1984)(Malcolm rider. 2002)(Afdil Evan. 2009)

    Aplikasi log Densitas (Rider. 2000) : perhitungan porositas Perhitungan AI Pendugaan litologi secara umum

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    Log Neutron

    (Pertamina EPTC. 2011) (Malcolm rider. 2002)(Singer. 2008)

    Aplikasi log Neutron (Rider. 2000) : Perhitungan porositas Identifikasi gas

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    Log Resistivitas

    Aplikasi log Resistivitas (Rider. 2000) : Saturasi fluida Karakter perlapisan

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    Log SP

    Aplikasi log SP (Rider. 2000) : Perhitungan resistivitas air formasi Indikasi zona permeabel Perhitungan kandungan serpih

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    Log Sonik

    Aplikasi log Sonic (Rider. 2000) : Perhitungan porositas Perhitungan AI

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    Log Caliper

    Aplikasi log Caliper (Rider. 2000) : Pengukuran kondisi ukuran lubang

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    Clay + silt + other

    Clays

    Plate-like form

    Large surface area

    Contain Al+3 and Si+4

    Substitution by Mg+2

    Negative chargeresults

    Attraction by waterand cations

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    Shale Distribution Types

    Dispersed Clay

    Clay Lamination

    Structural Clay(Rock Fragments,

    Rip-Up Clasts,Clay-Replaced Grains)

    fe

    fe

    fe

    ClayMinerals

    Detrital QuartzGrains

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    Structural replaces matrix

    may not affect porosity-permeability

    relatively uncommon

    e.g., clasts in channels

    Structural Clay

    (Rock Fragments,

    Rip-Up Clasts,

    Clay-Replaced Grains)

    fe

    Clay

    Minerals

    Detrital Quartz

    Grains

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    Laminated

    replaces matrix andporosity

    reduces porosity-permeability

    common e.g., intercalations

    assume similar tonearby shale

    Clay Lamination

    fe Clay

    Minerals

    Detrital QuartzGrains

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    Dispersed

    replaces pore space

    very common

    forms in situ

    may differ greatly from nearby shales

    porosity-permeability reduction depends onform

    Dispersed Clay

    feClay

    Minerals

    Detrital Quartz

    Grains

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    Kaolinite booklets

    moderate perm effects

    may dislodge, blockthroats

    Chlorite coating

    significant perm loss

    traps water

    Illite tangle

    chokes pores and throats

    drastic perm reduction

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