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TLD 1 Platform Express* TLD Triple Detector Lithology Density

Triple Detector Lithology Density

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Outline Introduction to Density Measurement Hardware Description Physics of Measurement Gamma Ray Interactions, Detector response Nuclear Spectrum, Gain stabilization Measurement Analysis Response model, Inversion algorithm, Examples Operations Parameters, Corrections, Calibration Safety LQC Log Examples, Products Sonde Mechanics - Overview

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Page 1: Triple Detector Lithology Density

TLD 1

Platform Express*

TLDTriple Detector

Lithology Density

Page 2: Triple Detector Lithology Density

TLD 2

Outline

• Introduction to Density Measurement

• Hardware Description

• Physics of Measurement– Gamma Ray Interactions, Detector response

– Nuclear Spectrum, Gain stabilization

• Measurement Analysis– Response model, Inversion algorithm, Examples

• Operations– Parameters, Corrections, Calibration– Safety

• LQC

• Log Examples, Products

• Sonde Mechanics - Overview

Page 3: Triple Detector Lithology Density

TLD 3

Introduction to Density MeasurementDensity Tools measure two main properties:DENSITY ==> bulk density of the formationLITHOLOGY==> indicator of formation type

POROSITY can be derived from Density Measurement

Density Logging Schematic

CaliperThe tool design also allows a simultaneous caliper measurement

Page 4: Triple Detector Lithology Density

TLD 4

Density Tools History • PGT - Powered Gamma Tool• LDT - Litho Density Tool• TLD - Triple Detector Litho-Density

Fundamental Difference in Tool Physics and Detectors have been implemented with each evolution of tool.

Page 5: Triple Detector Lithology Density

TLD 5

TLD Measurement Objectives The main objectives of the Platform Express density measurement are:• Give a high resolution estimate of density when pad

application is good and mudcake thickness small (<.5”)

• Provide a robust formation density measurement in bad borehole conditions (rugosity, standoff)

• Improve the Pe measurement with regard to precision (statistical error) and mudcake effect compensation

• Reproduce the LDT density estimation when this tool performs well

Page 6: Triple Detector Lithology Density

TLD 6

GR24 in.

b, Pe

18 in., 8 in., 2 in.

Rxo, hmc

2 in.

Rt

12 in.

HGNS

HRMS

HALS AIT

N

24 in.

Highly IntegratedGamma RayNeutronSonde

TOOL Hardware: PLATFORM EXPRESS - Density

Electronicscartridge

High-ResolutionMechanicalSonde

High-ResolutionAzimuthalLaterologSonde

ArrayInduction ImagerTool

HRCC

Page 7: Triple Detector Lithology Density

TLD 7

High-Resolution Skid

MCFL MicroCylindrically focussed logTDD Detector DensityLS Long Spacing DetectorSS Short Spacing DetectorBS Back Scatter Detector

Page 8: Triple Detector Lithology Density

TLD 8

High-Resolution Skid - inside

LS

BSSSMCFLLSXtal/PMT

Flex cable to sonde Electronics Xtal/PMT Xtal/PMT

Depleted Uranium

TungstenStainless Steel

MCFL SS BS SOURCE

Safety !!

Page 9: Triple Detector Lithology Density

TLD 10

Density GR Detectors

Long Spacing (LS) DetectorNaI (T) Sodium Iodide,Thallium doped (not colimated)

Short Spacing(SS) DetectorsNaI (T) Sodium Iodide,Thallium doped (not collimated)

Backscatter (BS) Detector GSO - Gadolinium Orthosilicate, Cerium doped, (collimated0

NaI is rated to 350 degf.GSO has lesser temp rating than NaI

GSO is more efficient than NaIGSO is very expensive

TDD Detectors

Scintillation Detectors are used

Page 10: Triple Detector Lithology Density

TLD 12

DENSITY PHYSICS

Page 11: Triple Detector Lithology Density

TLD 13

Gamma Ray Interactions - Review• High Energy GR emitted from chemical source• Reacts with matter in formation• Type of interaction dependent on GR energy level• Source used is Cesium-137, 662 Kev• Hence Compton Scattering and P.E. Absorption occur

Photoelectric Absorption Compton Scattering

Pair ProductionGR < 100 Kev GR > 100 Kev

GR > 1.02 Mev

Page 12: Triple Detector Lithology Density

TLD 15

Density Physics - Compton Scattering

## 2Z / A almost equal to 1 except for Hydrogen

Measuring Rhoe we know Rhob

Ne = Rhob * Z * Na / A

Rhoe = Rhob * ( 2 Z / A)

## ( 2 Z / A) ~ 1

Rhoe Rhob

Electron density index and Bulk Density

(Ne) Number of electrons in one gram(A) Atomic weight - the mass of an atom (grams/gram-atom).(Z) Atomic number (Z) - the number of electrons in a neutral atom (electrons/atom).(Na) Avogadro's number (Na ) - the number of atoms in a gram-atom

(6.02 x 1023 ).(Rhob) Bulk density(Rhoe) Electron density index

Page 13: Triple Detector Lithology Density

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Density Physics - examplesProperties of common elements in formations

Page 14: Triple Detector Lithology Density

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Density Corrections

• Differences exist between bulk (actual bulk density of formation)

electron (electron density of formation)

apparent (what the tool measures)

• Most times the corrections are negligible

• Correction charts are available

• Tool is calibrated for water filled LIMESTONE

• Hence zero correction for Limestone

Page 15: Triple Detector Lithology Density

TLD 18

Density Physics - Photoelectric Absorption• Reaction occurs at Low Energy GR < 100 Kev

• GR interacts with shell electrons Absorption

• Shell electrons related to Z Atomic number

• Higher Z means higher PE absorption

• Count the GR reaching tool after the interactions

measure PEF (PEF = (z/10)3.6)

Knowing ... PEF (Z) LITHOLOGY

Page 16: Triple Detector Lithology Density

TLD 19

Density and PEF - common minerals and liquids

** Also see Log examples later in the presentation.

Page 17: Triple Detector Lithology Density

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Density Physics - SummaryHigh energy GR emitted from chemical sourceSource Energy 662 KevCompton Scattering and Photoelectric AbsorptionAfter interactions, GR reaches the Scintillation detectors

Density tool measures Electron Density

Electron density is related to Bulk Density

2Z/A is almost equal to 1 for common formation

Electron density almost equal Bulk Density

Heavier the matter higher the Z atomic number

Higher Z means higher Photoelectric absorption

Tool also measures the absorption factor

Knowing PEF (Z) gives indication of formation

Page 18: Triple Detector Lithology Density

TLD 21

Density Nuclear Spectrum

Energy

Count Rate

GR Detector Electronics Spectrum

After interaction with the formation, GR reaches crystalIncident GR have different energy levelsBoth .. Energy and Counts of the GR are of interest Detector pulse height proportional to GR energy The pulses are then sorted and counted by electronicsThe count rate vs energy distribution is called SpectrumThe Spectrum will vary with formation - (GR interactions)

Page 19: Triple Detector Lithology Density

TLD 22

Nuclear Spectrum - Regions

Count/Sec

Region of Photoelectric Effect( & Z Information)

Region of Compton Scattering( Information Only)

Source Energy662 keV

Lithology Window

Energy keV

Density Window

Page 20: Triple Detector Lithology Density

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Spectrum Change with Lithology

Count/Sec

Region of Photoelectric Effect( & Z Information)

Region of Compton Scattering( Information Only)(Low Z)(Med Z)

(High Z)Source Energy662 keV

Energy keV

= constant

Page 21: Triple Detector Lithology Density

TLD 24

Spectrum Change with Density

Count/Sec/keVRegion of Photoelectric Effect

(Low )(Med )

(High )

Source Energy662 keV

Region of Compton Scattering

Z = constant

Page 22: Triple Detector Lithology Density

TLD 25

Spectrum Stabilisation

Reference R/A source 1 cu, 662 Kev is usedThis has a small spectrum centered at 662 KevTherefore Photomultiplier High Voltage is adjusted.

CONTINUOUS FEEDBACK LOOP

GR Detector

Energy

Count Rate

Spectrum

Detector level/gain (e.g. temperature) can shift the spectrum

Energy

Count Rate

PM High Voltage

662 KevReference Source

Page 23: Triple Detector Lithology Density

TLD 26

Spectra Comparison - LS

WATER

LIMESTONE

DIABASE

Attenuative - decreasing count rates with density. This also applies to SS.

Two orders of magnitude between counts in water and diabase.

Page 24: Triple Detector Lithology Density

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BS Spectrum - behaves differently

Positive - increasing count rates with density.

Factor of two between counts in water and diabase.

Page 25: Triple Detector Lithology Density

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BS Spectrum

The BackScatter Spectrum differs from LS and SS

Count rates are much higher

Therefore GSO crystal is used

Increasing density results in increasing counts

This is mainly due to detector design

The Backscatter detector is COLLIMATED

Formation

Mudcake

Mud

Density

Hmc

Depleted Uranium

TungstenStainless Steel

BS Integrated

SS Integrated

MCFL

LS Integrated Detector

Electronics

Detector

Detector

Source

Mudcake

Formation

HRGD

Density Formation

Model

Formation

Page 26: Triple Detector Lithology Density

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Processing Outputs

• Standard resolutionResolution of 18”Output sampling rate: 2”LDT like outputRHOZ, PEZ, UZ, ROMZ, PEMZ, DSOZ

• High resolution (main)Resolution of 8”Output sampling rate: 2” RHO8, PE8, U8, ROM8, PEM8, DSO8

• Very high resolutionResolution of 2”Output sampling rate: 0.5” RHOI, PEI, UI, DSOI

Page 27: Triple Detector Lithology Density

TLD 30

Bit Size

Apparent Bit Size

Density Hole Correction

Page 28: Triple Detector Lithology Density

TLD 31

Bit SizeDensity Hole Correction

Page 29: Triple Detector Lithology Density

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Bit Size

Apparent Bit Size

Density Hole Correction

Page 30: Triple Detector Lithology Density

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Bit Size

Caliper Reading

Density Hole Correction

Page 31: Triple Detector Lithology Density

TLD 34

Bit Size

Apparent Bit Size

Density Hole Correction

Page 32: Triple Detector Lithology Density

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SAFETY

Page 33: Triple Detector Lithology Density

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TDD - SafetyHRMS is heavy - back injury hazard - Plan the lifting

HRGD skid is heavy- When caliper is open look out for finger crushing

Depleted Uranium Shield in the HRGD- do not dismantle the HRGD skid

Beryllium Window is highly poisonous - do not scratch /puncture the BS or SS coverBe careful during Q-check

Detector Reference source is CS-1379 Ci for BS and LS, 0.6Ci for LSCs-137 is toxic, Use tweezers while handling

Thallium doped NaI crystal - handle with care. Mildly poisonous

Dessicant in electronics causes irritationUse gloves for handling, Wash hands, Do not ingest, or contact with eyes

High voltages present in the tool250V head voltage3000 V (max) for PM tube.

GSR-J source used for loggingAll R/A precautions and rules to be followed

Page 34: Triple Detector Lithology Density

TLD 37

SAFETY - GSR-J Source

2 mrem/hr

17 metres

The GSR-J source is collimated - Do not Stand in front2 mrem/hr distance is 17 metres17 metres in front of skidSource Handling Tool and Safety Clip must be usedRadiation Badge must be wornOnly the Engineer is allowed to transfer a Radioactive Source

Page 35: Triple Detector Lithology Density

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LOG QUALITY CONTROL

Page 36: Triple Detector Lithology Density

TLD 39

Quality Indicators

Tau loop error /Offsets /Crystal resolution /Low energy noise /Total count rate /P.M high voltage/Form Factor

Density Detector Quality Flag

Density Computation Quality FlagPe computation Quality Flag

Density correction curve (LOW LS

Based on reconstruction errors (W - W )/Wand database limits

Cal CalRec

• Hardware quality flags

• Processing quality indicators

Page 37: Triple Detector Lithology Density

TLD 40

Hardware - LQC

Page 38: Triple Detector Lithology Density

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Processing - LQC

Page 39: Triple Detector Lithology Density

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DENSITY LOG RESPONSE

andEXAMPLES

Page 40: Triple Detector Lithology Density

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Density Log Example - 1... Lithology Identification

Shale

Sand - Hydrocarbon Bearing

Sand - Water bearing

Shale

X800

Page 41: Triple Detector Lithology Density

TLD 45

Density Log Example - 2..

Sandstone

Limestone

Shale

Shale

Page 42: Triple Detector Lithology Density

TLD 46

Density Log Example - 3...

SALT

Shale

Sand- shaly

Page 43: Triple Detector Lithology Density

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Density Log Example - 4...

Dolomite

Limestone

Page 44: Triple Detector Lithology Density

TLD 49

Answer Product - example ... (unreleased example)

LITHOCOLUMN

Carbonate ReservoirAIT Resistivity Image

Resistivity Logs Nuclear Logs

RHOZ

NPHI

PEFZSP

Caliper

GR

PEX ANSWER Product with Lithology Analysis from TDD measurements is shown above.Correct PEF reading is crucialThe TDD provides formation PEF measurement corrected for heavy mudcake (barite) effects , previously not available.

Page 45: Triple Detector Lithology Density

TLD 50

Summary - TDD Measurement

• High resolution density measurement (BS-SS)

• Formation Pe compensated for mudcake effect (non-barite environment)

• Good statistics in hard formations

• Mudcake thickness estimation

• Co-located Rxo measurement

Page 46: Triple Detector Lithology Density

TLD 51

HRMS Overview - Mechanical Design

Page 47: Triple Detector Lithology Density

TLD 52

Flex Joint Advantage - Rugosity

Hinge Joints

Hinge Joints

Good Pad Contact in Rugose Holes

Page 48: Triple Detector Lithology Density

TLD 53

HRMS - Short Radius Logging

• PEX is useful for deviated wells with short radius, due to the high flexibility of HRMS

• Good Field examples• No tools stuck or seriously damaged

– Minimum Dogleg Radius: 20 - 45 metres– Max Build Rate: 39 - 86 deg/30m

• average 72 deg/30m– Bit Size: 6 1/4” - 8 1/2” – Depths: 800 - 2500 m

• Need to convey on Drill Pipe

30 metres measured depth

Build Angle