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HomeMy WebLinkAboutGMC Data Report No. 332X-Ray Diffraction analysis and flow testing of Hemlock Sandstone from core of the
XTO Energy Ina (orig. operator was Shell Co.) MGS (Middle Ground Shoal) C31-26 (9,195.5'-
9,196.4'), and
Union Oil Company of California MGS State 17595 No. 31 (9,525.2'-9,526').
Received July 2006 Total of 17 pages in report
Alaska Geologic Materials Center Data Report No. 332
BJ SERVICES COMPANY
RESEARCH AND TECHNOLOGY CENTER
Special Core Analysis Group
TECHNOLOGY CENTER REPORT NO.06-03-0250
XTO ENERGY
FLOW TESTING
HEMLOCK SANDSTONE
FOR USE ON PLATFORM A OIL WELLS
COOK INLET, ALASKA
REPORT PREPARED FOR:
MR. ROD EDWARDS
BJ SERVICES TECHNICAL REPRESENTATIVE
ALASKA
APRIL 17, 2006
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GMC DATA RErt~RT 3 3 Z Page 1/
BJ SERVICES TECHNOLOGY CENTER REPORT #06-03-0250
APRIL 17, 2006
TABLE OF CONTENTS
Page
SUMMARY OF RESULTS .............................................................................. 1
INTRODUCTION ........................................................................................... 2
ROCK CHARACTERIZATION EVALUATION ......................................... 3
FIGURES 1 - 2: SEM IMAGES .................................................. 6 - 7
PERMEABILITY AND FLOW TESTING .................................................... 8
FIGURES 3 - 6: REGAIN PERMEABILITIES ................................ 11 - 14
COMMENTS ................................................................................................... 15
GMC DATA RrP~RT 3 3 2 Page 2/17 ~~
BJ SERVICES TECHNOLOGY CENTER REPORT #06-03-0250 PAGE 1
APRIL 17, 2006
SUMMARY
General
Two core sections from the Hemlock Formation were analyzed to provide regain
permeability data subsequent to mud damage and damage removal treatments.
Flow Testing
Porosity and permeability testing was conducted after aggressive cleaning of plugs.
Helium porosities range from 10.4% to 16.8%, and dry nitrogen permeabilities range
from 1.58 and to 177 and at room temperature and 250 psi confining pressure for
permeability. Results of flow testing indicate that aParavan-25 preflush followed by an
acid treatment is most effective in removing mud damage. The one step treatment with
xyiene and acid was not effective in removing damage. Results of all tests are
summarized below:
Initial k k to Oil k to Oil k to Oil after Change,
FLUID Depth, to Oil, after Mud,
d after One
and
Shot Two Step
Paravan-25 and
(Relative
feet and an , .Acid, and to Mud
Dama e
One Shot 9195.74 28.8 20.1 5.7 - -72
One Shot 9525.37 0.357 0.262 0.068 - -74
Two Ste 9196.13 41 37.8 - 40.2 +6
Two Ste 9525.35 0.290 0.250 - 0.239 -4
On the basis of the flow test data, we recommend that the 2 step system, consisting of
a Paravan-25 preflush followed by the 10% HCI system, be used in the field.
Mineralogy
Quartz was the principal mineral phase detected by bulk X-ray analysis. Feldspars are
abundant with plagioclase being the more abundant feldspar variety. Potassium
feldspar is present in both samples. Iron-bearing dolomite was detected in a minor
quantity in both samples. The total percentage of clay minerals and sheet silicates,
from bulk X-ray analysis, ranges from 4% to 11%, by weight. Kaolinite (migrating) is the
most abundant clay mineral. Illite-smectite, a mixed layer swelling clay with 65%-80%
non-swelling illite layers and 20% - 35% expandable smectite layers, was detected in
both samples. Chlorite (iron-bearing) was detected in both samples. Illite (mica) was
also detected in both samples. By comparison, the 9525 foot sample contains more
feldspar and clay than does the 9196 foot sample.
The above data and interpretations are supplied solely for informational purposes, and BJ Services Company makes no guarantees or warranties,
either expressed or implied, with respect to the accuracy or use of these data and interpretations. All product warranties and guarantees shall be
governed by the standard contract terms at the time of sale. .
r. ~ ~ ~ Page 3/17 ~
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BJ SERVICES TECWNOLOGY CENTER REPORT #06-03-0250
APRIL 17, 2006 PAGE 2
INTRODUCTION
Scope and purpose
The analysis of core plugs, drilled from two submitted hlemlock core section, Cook Inlet,
Alaska, serves as the data base for this study. The study was requested by Mr. Rod
Edwards, BJ Services technical representative, Anchorage, Alaska. Data generated by
the study will be used to clean up possible oil-based mud damage from XTO Energy
horizontal wells in Cook Inlet, Alaska. BJ Services Technology Center sample numbers
and analyses performed in this portion of the study are listed below:
SAMPLE ANALYSIS
Depth, NUMBER
feet 0&03-0250 XRD SEM k FLOW
9525.38 1 - - X X -
9525.37 2 X X X X X
9525.35 3 - - X X X
9525.47 4 - - X X -
9525.48 5 - - X X -
9525.49 6 - - X X -
9196.15 7 - - X X -
9196.13 8 X X X X -
9195.88 9 - - X X X
9195.74 10 - - X X -
9195.80 11 - - X X X
X =Analysis Performed - =Analysis not Performed
XRD = X-ray Diffraction Analysis SEM =Scanning Electron Microscopy
= Porosity k = Permeabili FLOW =Flow Testing
This study was initiated to provide regain permeability data subsequent to acidization
and treatments.
Analyses Pertormed
To supply data required from the study, the following analyses were performed and are
reported in this portion of the study:
X-ray Diffraction Analysis
Scanning Electron Microscopy
Porosity and Permeability Determination
Flow Testing with Acid
Flow Testing with Two Step System
The above data and interpretations are supplied solely for informational purposes, and BJ Services Company makes no guarantees or warranties,
either expressed or implied, with respect to the accuracy or use of these data and interpretations. All product warranties and guarantees shall be
governed by the stantlard contract terms at the time of sale.
I
GMC oa;r~- fC~~ ~~T ~ 3 C Page 4/17 1
BJ SERVICES TECHNOLOGY CENTER REPORT #06-03-0250
APRIL 17, 2006 PAGE 3
MINERALOGY -ROCK CHARACTERIZATION EVALUATION
Sample Analysed and Description of Methods
An evaluation of the rock mineralogy of portions of a plug from each core section was
initiated to determine the mineralogic composition for use as a parameter in the design
of a treatment system. Two samples were analyzed using semiquantitative bulk and
clay fraction X-ray analysis (XRD). Portions of these samples were reserved for ex-
amination with the scanning electron microscope (SEM) to observe the distribution of
clay and other pore filling minerals. Approximate weight percentages of mineral phases
present in a sample, including clay minerals, are specifically determined by X-ray
analysis. Clay mineral distributions and the overall morphology of the pore system
(porosity and the degree of interconnection of open pores) are examined during
scanning electron microscopy. Prior to analysis, residual contamination was removed by
toluene vapor extraction.
X-Ray Diffraction Analysis
Samples were analyzed using both bulk (whole rock) and fine (clay-size) fraction X-ray
diffraction techniques. A portion of each selected sample was gently crushed, and
crushed material was thoroughly mixed. Half of the crushed material was ground to a
fine powder, and the bulk mineralogy of the sample was determined. The clay size
fraction was separated from the second part of the crushed mixture, and the clay
mineralogy of each sample was determined in both air dried and glycolated states.
Note that the term trace (Tr) refers to a quantity of less than 1 %.
Quartz was the principal mineral phase detected by bulk X-ray analysis (69% - 81 %).
Plagioclase is the more abundant feldspar variety (8% - 14%). Potassium feldspar (4%
- 5%) was detected in both samples. Iron-bearing dolomite was detected in a minor
quantity in both samples (1%). The total percentage of clay minerals and sheet
silicates, from bulk X-ray analysis, ranges from 4% to 11 %, by weight. Kaolinite
(migrating) is the most abundant clay mineral (3%). Illite-smectite, a mixed layer
swelling clay with 65-85% non-swelling illite layers and 20% - 35% expandable smectite
layers, was detected in both samples (Tr - 3%). Chlorite (iron-bearing) was detected in
both samples (1 - 3%). Illite (mica) was also detected in both samples (1 % - 2%). By
comparison, the 9525 foot sample contains more feldspar and clay than does the 9196
foot sample. Results of the analysis are given on the following page.
The above data and interpretations are supplied solely for informational purposes, and BJ Services Company makes no guarantees or warranties,
either expressed or implied, with respect to the accuracy or use of these data and interpretations. All product warranties and guarantees shall be
governed by the standard contract lama at the time of sale.
GMC DATA`, RED ART 3 3 2 Page 5/I7 ~
1
BJ SERVICES TECHNOLOGY CENTER REPORT #06-03-0250 PAGE 4
APRIL 17, 2006
SEMIQUANTITATIVE X-RAY DIFFRACTION ANALYSIS
XTO ACID STUDY
AMPLE NO.: 06-03-0250 2 $
SAMPLE DEPTH, ft 9525.37 .9196.13
CLAY MINE RALS
ILLITE-SMECTITE 3 Tr
ILLITE 2 1
1
CHLORITE 3 2
KAOLINITE 3
CARBONATE M INERALS
CALCITE (CaC03} Tr ND
FERROAN DOLOMITE ((Ca(Mg,Fe)(COs)2) 1 1
OTHER MIN ERALS
QUARTZ 69 81
PLAGIOCLASE FELDSPAR 14 8
POTASSIUM FELDSPAR 4 5
TOTAL S
CLAY MINERALS 11 4
CARBONATE MINERALS 1 1
OTHER MINERALS 87 94
*THE ILLITE-SMECTITE IS 20% - 35% EXPANDABLE SMECTITE LAYERS.
Tr = <1 % ND =NOT DETECTED
The above data and interpretations are supplied solely for informational purposes, and BJ Services Company makes no guarantees or warranties,
either expressed or implied, with respect to the accurecy or use of these data and interpretations. All product warranties and guarantees shall be
governed by the standard contract terms at the time of sale.
GMC DATA REPORT 3 3 2 Page 6/17 ~~
BJ SERVICES TECHNOLOGY CENTER REPORT #06-03-0250 pAGE 5
APRIL 17, 2006
Scanning Electron Microscopy
Portions of two samples were examined with the scanning electron microscope. The
principal objective of this examination is to observe the distribution of clay minerals and
other authigenic cements in the pore system. Secondarily, the overall morphology of
the pore system, particularly with regard to pore sizes and the degree of interconnection
of open pores, was examined. Features of samples are illustrated in black and white
photo images which accompany the report (Figures 1 - 2).
Samples examined represent poorly to moderately sorted, fine to lower medium grained
feldspathic quartz sandstones. Quartz is the principal framework grain. Feldspars are
present and have been diagenetically altered to clay minerals. Other framework grains
were not observed. Kaolinite and illite-smectite are obvious authigenic clay minerals
observed in these samples. The kaolinite may have replaced some feldspar grains.
The clay is authigenic and locally fill pores and blocks entrances to pore throats. Illite-
smectite bridges pores and pore throats. Minor quartz overgrowth development was
observed on few quartz grains.
Porosity in these samples is limited by the precipitation of authigenic clay in the pore
system, by the precipitation of quartz overgrowths on quartz grains, by long axis close
packing of framework grains, and by the poor sorting .(allows larger pores to be filled by
finer grains). Pore and pore throat sizes are summarized below:
DEPTH,
ft MAXIMUM
PORE SIZE, m MAXIMUM PORE
THROAT SIZE, m OBSERVED PORE
TYPE
9196.13 100 5 P, M
9525.37 30 1 P ~ M
P =PRIMARY INTERGRANULAR M = M1CR0 ANY PORE <5 m
The above data and interpretations are supplied solely for informational purposes, and BJ Services Company makes no guarantees or warranties,
either expressetl or implied, with respect to the accurecy or use of these data and interpretations. All product warranties and guarantees shall be
governed by the standard contract terms at the time of sale.
GMC D~-TA REPORT 3 3.2 Page ~/1~ ~
BJ SERVICES TECHNOLOGY CENTER REPORT #06-03-0250 PAGE 6
APRIL 17, 2006
FIGURE 1
SEM IMAGES
XTO, PLATFORM A, 9525.37 FEET
The portion of the sample illustrated in these SEM images represents a poorly to moderately sorted,
upper fine to lower medium grained sandstone. Quartz (Q) is the principal framework grain. Most grains
exhibit some overgrowth development. Feldspars (F) are abundant and have locally been altered (AF).
Open pores (arrow and P) are present but are locally filled by silt-sized grains. Kaolinite (K) is a major
authigenic clay mineral. The clay partially fills pores. Illite-smectite (IS) is abundant, forming thin rims on
framework quartz grains and bridging pore throats. Magnification Photo A = 200x; Photo B = 650x.
The above data and interpretations are supplied solely for informational purposes, and BJ Services Company makes no guarantees or warranties,
either expressed or implied, with respect to the accuracy or use of these data and interpretations. All product warranties and guarantees shall be
governed by the standard contract terms at the time of sale. . 1
GMC DATA REPORT 3 3 Z Page s/17 ~
BJ SERVICES TECHNOLOGY CENTER REPORT #06-03-0250
APRIL 17, 2006 PAGE 7
FIGURE 2
SEM IMAGES
XTO, PLATFORM A, 9196.13 FEET
The portion of the sample illustrated in these SEM images represents a moderately sorted, upper fine to
lower medium grained sandstone. Quartz (Q) is the principal framework grain. Most grains exhibit quartz
overgrowth development (QOG). Kaolinite (K) is the principal authigenic clay mineral observed. The clay
partially fills pores and blocks entrances to pore throats. Micropores (arrow) are abundant in areas of the
rock occupied by kaolinite. Chlorite (CH?) rims framework quartz grains. Feldspar grains have locally
been altered to clay (C). The area illustrated in Photo B is an enlargement of the area enclosed by the
box in Photo A. Magnification Photo A = 100x; Photo B = 250x.
The above data and interpretations are supplied solely for informational purposes, and BJ Services Company makes no guarantees or warranties,
either expressed or implied, with respect to the accuracy or use of these data and interpretations. All product warranties and guarantees shall be
governed by the standard contract terms at the time of sale.
GMC DATA REPORT 3 3 2 Page 9/17 j~
BJ SERVICES TECHNOLOGY CENTER REPORT #06-03-0250 PAGE 8
APRIL 17, 2006
PERMEABILITY AND FLOW TESTING
Eleven (11) 1 inch in diameter core plugs were drilled from the two submitted core
sections. Prior to testing, residual hydrocarbon and other contaminants were removed
from plugs, using the toluene vapor extraction technique. In this technique, extraction is
continued until the fluid in contact with cores is colorless. Plugs were further cleaned
with methanol to strip any residual fluids from the pore system. After cleaning, plugs
were dried at 150 °F for 13 hours. Helium porosifles are determined with a dual cell
Boyle's Law porosimeter, and dry nitrogen permeabilities are determined with a
standard permeameter. Bulk densities are determined from plug dimensions and plug
masses. Results of analyses for plugs used in flow testing are given below:
Depth, ft Sample No.
06-03-0250 Pore
Volume,
cm3 Bulk
Density,
g/cm3 Grain
Density,
glcm3 He
Porosity
~, % k to
Nz,
and
9525.38 1 3.46 2.374 2.662 10.8 1.58
9525.37 2 2.93 2.364 2.668 11.4 1.84
9525.35 3 2.60 2.393 2.669 10.4 1.93
9525.47 4 2.59 2.363 2.665 11.3 1.59
9525.48 5 3.66 2.367 2.669 11.3 1.66
9525.49 6 3.37 2.372 2.663 10.9 1.67
9196.15 7 5.19 2.201 2.643 16.7 177
9196.13 8 4.46 2.198 2.642 16.8 132
9195.88 9 4.82 2.241 2.646 15.3 84.1
9195.74 10 4.31 2.245 2.650 15.3 79.2
9195.80 11 5.25 2.225 2.650 16.0 70.3
Special Testing
Testing was initiated to fulfill the following objectives:
• Determine the effectiveness of a single step acid treatment in removing an oil
based mud from the rock
• Determine if the previously developed mud damage removal system is effective
with formation oil and formation rock, with reduced concentrations of Paravan-25
and US-40.
Test fluids, procedures and results are summarized on the following pages.
The above data and interpretations are supplied SolCly for informational purposes, and BJ Services Company makes no guarantees or warranties,
either expressed or impliatl, with respect to the accuracy or use of these data and interpretations. All product warranties and guarantees shall be
governed by the standartl contract terms at the time of sale. .
GNIC DATA REPORT 3 3 Z Page 10/17 ~
BJ SERVICES TECHNOLOGY CENTER REPORT ;6-03-0250 PAGE 9
APRIL 17, 2006
Fluid Systems
Systems utilized in flow testing are given below:
Fluid Formulations
Fluid Additives
MI Versadrill Oil Base Supplied by XTO. 80/20 Oil external/water emulsion. Versacoat
g ppg 5 ppb; Versawet 2.5 ppb; Lime 2 ppb; IMG400 8 ppb; Versa HRP
1 b; CaCl2 25%
One Shot Acid Plus 4 gpt S-400; 1 gpt NE-118; 3 gpt NE-110W; 50 gpt US-40; 5 gpt
10% HCI/25% Xylene CI-27; 30 ppt Ferrotrol-300 + 7 ppt Ferrotrol-200; 15 gpt AS-6
ests 1 - 2
Pretreat -Tests 3 - 4
3% KCI; 25 t Paravan-25; 5% US-40; 10 t NE-110W
Oil 70% Mineral Oil/30% Iso ar L and su lied b XTO
10%HCI -Tests 3 - 4 25 gpt Paravan-25; 5% US-40; 3 gpt NE-110W; 30 ppt Ferrotrol-
300; 7 ppt Ferrotrol-200; 5 gpt CI-25 -Note that AS-6 was not
omitted from this acid because field oil was injected prior to acid
injection.
AQUEOUS FLUIDS ARE BASED IN FILTERED FRESH TOMBALL TAP WATER.
Testing: All testing was performed in accordance with standard BJ Services
test procedures
Test procedures for the flow tests are, generally, as follows:
Prior to analysis, plugs were seated in rubber sleeves at 1000 psi
confining pressure and flowed with filtered formation water (when
available) to core saturation. The system was gradually heated to 165 °F.
A backpressure of 150 psi was used throughout all tests. This step is
common to all flow test procedures.
Tests 1- 2; Mud Damage followed by the One Shot Acid Plus System
2. Flow was established in an arbitrary formation to wellbore (production)
direction with laboratory oil to steady state permeability.
3. After steady state was achieved, formation oil (2 pore volumes) and mud
were injected dynamically (cross-face flow) at 500 psi. The mud was then
statically shut in for 6 hours.
The above data and interpretati°ns are supplied solely for informational purposes, and BJ Services Company makes no guarantees or warranties,
edt+er expressed Or implied, with respect to the accuracy Or use of these data and interpretations. All product warranties and guarantees shall be
governed by the standard eontrae! terms at the time of sale. .
GMC DATA REPORT ~ 3 2 Page 11/17 ~
BJ SERVICES TECHNOLOGY CENTER REPORT #06-03-0250 PAGE 10
APRIL 17, 2006
4. Plugs were flowed in the production direction to determine a damaged
permeability. This step is necessary to make sure that a damaged plug is
being treated. For example, if the plug is not damaged by mud injection
and if the treatment is run immediately after mud injection, an
unsuccessful treatment, relative to mud damage removal, could appear to
be successful if application of the treatment did not result in damage to the
core.
5. The One Shot Acid Plus system (10 pore volumes) was injected in the
wellbore to formation direction.
6. Flow was established in an arbitrary formation to wellbore (production)
direction with laboratory oil to steady state permeability.
7. Results are illustrated on Figures 1 - 2.
Preflush, "New" Acid System Testing
8. Steps 1 through 3 above.
9. Step 4 above, using laboratory oil as the flowing medium.
10. The Paravan-25 system was injected, followed by the injection of 10 pore
volumes of the "new" acid system. Flow was re-established in the forward
(production) direction to steady state permeability.
11. Results are illustrated on Figures 3 and 4.
Tho above dale end interpretations are supplied solely for informational purposes, and 8J Services Company makes no guarantees or warranties,
either expressed or implied, with respect to the accuracy or use of these data and interpretations. AI! product warranties and guararnees shall be
governed by the standard contract terms at the time of sale.
GMC DATA REPORT 3 3. ~ Page 12/7 ~~
BJ SERVICES TECHNOLOGY CENTER REPORT #06-03-0250 PAGE 11
APRIL 17, 2006
FIGURE 1
REGAIN PERMEABILITY TESTING
MUD DAMAGE FOLLOWED BY THE ONE SHOT PLUS SYSTEM
LAB OIL AS FLOWING MEDIUM
9
E
s
E
E
o_
Permeability to Lab Oil:
Permeability to Lab Oil after Mud:
Permeability to Lab Oil after Acid:
0.357 and
0.262 and
0.068 and
The acid did not remove mud damage. The permeability was further
reduced subsequent to acid contact.
The above data and interpretations are supplied solely for informational purposes, and BJ Services Company makes no guarntees or warranties,
either expressed or implied, with respect to the accuracy or use of these data and interpretations. All product warranties and guarantees shall be
governed by the standard contract terms at the time of sale. /
GMC DATA REPORT 3 3 2 Page ~ 3/ 1 ~ ~
Initlal k to oil K to 011 aner mua ~ .........•-• _.._ ___ _ _
Parameter
BJ SERVICES TECHNOLOGY CENTER REPORT #06-03-0250 PAGE 12
APRIL 17, 2006
FIGURE 2
REGAIN PERMEABILITY TESTING
MUD DAMAGE FOLLOWED BY THE ONE SHOT PLUS SYSTEM
LAB OIL AS FLOWING MEDIUM
.~
BJ SERVICES TECHNOLOGY CENTER REPORT #06-03-0250
APRIL 17, 2006 PAGE 13
FIGURE 3
REGAIN PERMEABILITY TESTING
LAB OIL AS FLOWING MEDIUM
MUD DAMAGE FOLLOWED BY THE PARAVAN-25 PREFLUSH
FOLLOWED BY THE "NEW" ACID SYSTEM
E
a
s
r
E
a
Parameter
Initial Permeability to Oil: 0.290 and
Permeability to Oil after Mud: 0.250 and
Permeability to Lab Oil after Acid: 0.239 and
The two step treatment did not remove mud damage. The permeability was
slightly reduced subsequent to acid contact
The above data and interpretations are supplied solely for informational purposes, and BJ Sernces Company makes no guarantees or warrantes,
either expressed or implied, with respect to the accuracy or use of these data and interpretations. All product warranties and guarantees shall be
governed by the standard contract terms at the time of sale.
GMC DATA REPORT 3 3 2 Page ~5/1~ j ~
Initial k to oil k to oil afDer mud k to oil after two step
treatment
BJ SERVICES TECHNOLOGY CENTER REPORT #06-03-0250 PAGE 14
APRIL 17, 2006
FIGURE 4
REGAIN PERMEABILITY TESTING
LAB OIL AS FLOWING MEDIUM
MUD DAMAGE FOLLOWED BY THE PARAVAN-25 PREFLUSH
FOLLOWED BY THE "NEW" ACID SYSTEM
so
ao
E ~
E
a n
11
Parameter
Initial Permeability to Oil: 41.0 and
Permeability to Oil after Mud: 37.8 and
Permeability to Lab Oil after Acid: 40.2 and
The permeability of the rock was nearly restored to its original value by the
use of the two step treatment.
The above data and interpretations are supplied solely for informational purposes, and BJ Services Company makes no guarantees ~~ wa~~a„~~~,
either expressed or implied, with respect to the aceuracy.or use of these data and interpretations. All product warranties and guarantees shall be
governed by the standard contract terms at the time of sale: .
6MC DATA REPORT 3 3 2 Page 16/1 ~
Initial k to oil K to on aner mua ~ .r ~~• ~• V-• •--- --~
freatmsnt
BJ SERVICES TECHNOLOGY CENTER REPORT #06-03-0250
APRIL 17, 2006 PAGE 15
COMMENTS
General -Two core sections from the Hemlock Formation were analyzed to provide
regain permeability data subsequent to mud damage and damage removal treatments.
Flow Testing -Helium porosities range from 10.4% to 16.8%, and dry nitrogen
permeabilities range from 1.58 and to 177 md. Results of flow testing indicate that a
Paravan-25 preflush followed by an acid treatment is most effective in removing mud
damage. The one step treatment with xylene and acid was not effective in removing
damage. Results of all tests are summarized below:
FLUID
Depth,
feet Initial k
to Oil,
and k to Oil
after
Mud,. and k to Oil
after One
Shot, and k to Oil after
Two Step
Paravan-25 and
Acid, and Change,
(Relative to
Mud
Dam e
One Shot 9195.74 28.8 20.1 5.7 - -72
One Shot 9525.37 0.357 0.262 0.068 - -74
Two Ste 9196.13 41 37.8 - 40.2 +6
Two Ste 9525.35 0.290 0.250 - 0.239 -4
On the basis of the flow test data, we recommend that the 2 step system, consisting of
a Paravan-25 preflush followed by the 10% HCI system, be used in the field.
Mineralogy -Quartz was the principal mineral phase detected by bulk X-ray analysis.
Feldspars are abundant with plagioclase being the more abundant feldspar variety.
Iron-bearing dolomite was detected in a minor quantity in both samples. The total
percentage of clay minerals and sheet silicates, from bulk X-ray analysis, ranges from
4% to 11 %, by weight. Kaolinite (migrating) is the most abundant clay mineral. Illite-
smectite, amixed layer swelling clay with 65%-80% non-swelling illite layers and 20% -
35% expandable smectite layers, was detected in both samples. Chlorite (iron-bearing)
was detected in both samples. Illite (mica) was also detected in both samples. By
comparison, the 9525 foot sample contains more feldspar and clay than does the 9196
foot sample.
Laboratory Report No.: 06-03-0250 Reported by:
Carolyn S. De Vine
Requested by: Rod Edwards
Location: Alaska
Analyzed by: K. Spurlock, J. Cutler, L. Vestal, G. Braun, C. De Vine
Data Integration: C. De Vine
Distribution: Rod Edwards, Nabil EI Shaari, SCA File, GS File, TTC File
The above data and interpretations are supplied solely for informational purposes, and BJ Services Company makes no guarantees or warranties,
either expressed or implied, with respect to the accuracy or use of these data and interpretations. All product warranties and guarantees shall be
governed by the standard contract terms at the time of sale.
Page 17/17 ~
GMC DATA REPORT 3 3 2 ~