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8/10/2019 SPE-30086-MS
1/12
Society of Petroleum
Engineers
SPE 3 86
Formation Damage due t Losses ea based Brine and How Was Revealed
Through Post Evaluation Scale Dissolver and Scale Inhibitor Squeeze
Treatments
K.
Lejon, Statoil
as,
J. Tuxen Thingvoll, Statoil
as,
E.A. Vollen, Statoil
as, P.
Hammonds, Baker Performance Chemicals
Copyright
1995,
Society
at
Petroleum Engineers, Inc,
This paper was prepared for presentation
at
the European Formation Damage Conference held In The Hague, The Netherlands, 15-16
May
1995,
This paperwasselected forpresentation by an SPE Program Committee following review of informationcontained inan abstract submitted by the author s). Contents ofthe paper, as presented,
have
not
been
reviewed
by
the Society of Petroleum Engineers and
are
subjected to correction
by
the author s ,
The material, as
presented, does
not
necessarily
reflect anyposition of
the
Society
of
Petroleum Engineers
Its officers
or members Papers presented
at SPE
meetings are SUbject
to publication review
y
Editorial
Committees
of
the
Society
of
Petroleum
Engineers
Permission to copy
is
restricted to a n abstract
of
not
more than 300
words. illustrations
may not be
copied,
The
abstract should contain conspicuous acknowledgment
of where
and by
whom
the paper
is
presented, Write Librarian, SPE, P,O.
Box
833836. Richardson. TX 75063-3836, U,S.A. Facsimile 214-952-9435).
ABSTRACT
Calcium based brine has regularly been used during workover
operations
on
naturally completed wells without any sign of
for-
mation damage.
In
gravel packed wells which have seen severe
losses
of
Ca based brine production decline was observed.
Fur some
of
the gravel packed wells the production decline oc-
curred when bringing the well on production after completion,
whilst
in
others, the
loss in
productivity occurred after sea water
breakthrough.
I
In
order
to
increase productivity
and
confirm the relationship
be-
tween productivity decline and formation of CaS0
4
scale due to
losses of completion brine, scale dissolver treatments were car
ried out.
The use of dissolver chemicals resulted
in
mobilization
and re-
moval
of
several hundred kilograms
of
solids from the near well
bore area.
A post-evaluation strategy to provide information about the na-
ture, origin
and
location
of
scale was successfully implemented.
More importantly, the dissolver treatments resulted
in
increased
oil production.
The findings and lessons learned have had several important
im-
plications
for
gravel pack completions
an d w ell
treatments
in
Statoi .
INTRODUCTION
Solutions
of
high density brines
of
calcium chloride and calcium
bromide are extensively used
in
workover and drilling opera
tions. Normally, this practice does not produce any deleterious
effects. However, the potential for formation damage due
to re-
action between calcium-based brine and water present
in
t he r es -
ervoir exists and is documented through laboratory studies and
field experience
2
3
References
and
figures
at e nd of
paper
75
Unfavorable mixing ratios of Ca-based brine
and
sea
water, used
as
solvent for chemicals or
as
displacing fluid, c an a ls o pl Oduce
favorable conditions for precipitation of solids
and
subsequent
formation damage.
In
addition, oilfield waters will deposit sparingly soluble salts
eg.
CaC0
3
) due to either changes
in
physical conditions e.g
temperature, pressure) or change
in
chemical composition loss
of gas, mixing
of
waters).
Scale deposits
are
commonly calcium carbonate; barium,
stl on-
tium and calcium sulphates; and various naturally occurring
ra-
dioactive materials NORM). The latter
are
commonly
precipitated with the other sulphate scales.
Carbonate scales
are
easily removed
by
acid treatment
and
cal
cium sulphate with moderate difficulty
by
using converters,
In oilfield operations Sulphate scales a re mor e commonly treated
with non-acid dissolvers. These formulations
are
blends of
chelating agents, accelerators, dispersants and other synergists.
4
The chelants are capable of forming soluble complexes with
metal ions. The stability
of
these complexes
is
known to depend
on the chelating agent and metal, solution pH, temperature,
etc.
For dissolution
to
occur, the solubility of the complex
m us t e x-
ceed that of the scale
as
indicated
by the
equations:
CaS0
4
s)
H
Ca2+
+
SO
l
Ca
2
+
+
EDTN- H
Ca EDTAl
aq)
Also, the scale must furnish metal ions
in
solution for chelation
to
occur. The strengths
of
chelant metal complexes
may be com-
pared from values
of
their stability constants
as
shown
in
Table I
8/10/2019 SPE-30086-MS
2/12
2
Formation
Damage due to Losses of Ca-based Brine and
How
Was Revealed
Through
Post Evaluation of Scale Dissolver and Scale
Inhibitor
Squeeze
Treatments
SPE 30086
Table
1:
S tabi li ty C lns tant s (loglllK) If Meta l Chelant
ClIInplexes'
elapsed from the time
of
completion to the apperance
of
the pro
duction problems,
Definition
of
productivity index:
PI
Q 10 P
s
- P Ibhp) where:
A list
of
events and observations leading to the verification of a
causal link between observed productivity problems and losses
of completion brine is given below,
Metal Chelant
NTA
HEDTA
EDTA
DTPA
A1
3
+ 11.40 14.40 10.30 18,70
Ca'+
6.40 8.30
10,70
10,80
Fe'+
8,30 12,20
14.30 16.40
Fe
3
+
15.90
19,80 25,10
28,00
Ba'+
4.80
6,30
10,70 10,80
Sr'+
5.00
6,90
8,70
9.80
QIo
P
I'CS
P
lbhp=
Total fluid rate Sm
3
/d)
Reservoir pressure
bar)
Flowing bot tom hole pressure bar)
Chelants are of relatively high molecular weight in compal'ison
to metal ions and therefore are required in high concentrations
for substantial scale dissolution, The aminocarboxylate chelants
are active over a broad pH range,
The activity toward a part icular metal ion varies with pH. A
chelant can then be formulated to be somewhat ion specific in
dissolution, These chelants are also stable to hydrolysis at high
temperatures: an essential property for surviving downhole con
ditions without degradation, The aminocarboxylates have low
toxicity to marine organisms but are not readily biodegradeable,
Formulated products are not aggresive to elastomeric material
and show low corrosion rates, relative to acid, on metals used in
well completion. 4
Use of brines containing alkaline earth metal ions as solvents,
pre-tlush or overt lush should be avoided where possible, as
these ions reduce the efficiency
of
the dissolver treatment.
For optimum performance, the design
of
a scale dissolver
job
should be conducted on a well by well basis,
An effective scale dissolver treatment requires correct applica
tion as well as an efficient product, Improper application
of
an
efficient product has been shown to produce poor results.
6 7
The treatment may be a simple bullheading of tluids downhole,
or require diverting agents
01'
coiled tubing. for accurate place
ment. A typical sequence is outlined below,
WELL HISTORIES
During a period of less than six months several gravel packed
wells experienced a sudden and sharp decline in productivity,
The problems appeared shortly after seawater breakthrough or in
connection with scale inhibitor squeeze treatments.
It was soon realized that the problems could be related to heavy
losses
of
calcium brine during completion operation,
During most complet ion operations, the bulk part ot the brine
volumes used are backproduced during the clean-up period.
Brine still remaining
in
the formation, so-called lost brine , is
expected to return over the next few days together with oil and
produced water.
For the problematic wells, heavy losses
of
high density calcium
brine (150-1000 m
3
)
were recorded, The volumes lost are sum
marized
in
t ab le 2. For these wells, several months to a year
76
Q
Ilit
and Pres are measured values,
P
lbhP
is calculated using a well hydraulic prediction programme,
Production data input comprises tlowing wellhead pressure, total
tluid rate and water cut.
Well A showed symptoms typical
of
formation dam,lge due to
calcium sulphate scale:
In July 93,10 months after completion, the PI dropped
from 750
to
520 m
d bar
and further
to
95 Sm
3
/d/bar
in October 93.
The first produced water sample obtained had a Ca'+
content (2100 mg l five times higher than expected
compared
to
the level found in more tban 20
neighbouring wells (350-450 mg/l),
Production logging in October
93
verified reduced
productivity together with high Gamma Ray (GR)
readings
In well B, formation damage occured after scale inhibitor
squeeze treatment following sea water breakthrough:
A sharp increase
in
the Ca'+ level was recorded during
a 48 hours backtlow period after inhibitor squeeze (500
mg l before, 4200 mg l after (see figure 1)
Only
6
return
of
inhibitor was found. This is
significantly lower compared to previous squeeze
treatments (25 30%)
Production logging performed before and after the
treatment verified reduced productivity
During a short period, three more gravel packed wells experi
enced productivity decline that have been linked to residuals
of
calcium brine in the neal' wellbore area,
In Well C, breakthrough
of
produced water with high sea water
content (98 %)
11
month after completion had a dramatic effect
on productivity:
During a few months produced water rate decreased
significantly and eventually ceased completely
The productivity (PI) alsoclecreased and this trend
continued after the water production ended,
Wel l 0 produced only I
water after, compared to 18 before,
gravel pack operation. Analyses
of
pr lduced water showed a
threefold increase in Ca'+ after gravel pack operation (from 1612
8/10/2019 SPE-30086-MS
3/12
SPE 30086 K. Lejon, J. Tuxen Thingvoll, E.A. Vollen, Statoil,
P.
Hammonds, Baker Performance Chemicals
3
to
4462 mg/I).
In
this
well
tangible evidence
of
calcium sulphate
precipitation
was
found:
Scale particles found
in
the sand trap and
in
downhole
bailer were identified as CaS0
4
21-lp gypsum).
Well E was eventually added
to
the list
of
problematic wells.
This well produced dry oil prior
to
the gravel pack operation. A
short time after, both the production rate and wellhead pressure
started
to
decline table 3)
For well
E,
the drop
in
production rate
was
related
to
possible
precipitation of CaS0
4
due
to
use of seawater during gravel pack
operation
Table 3. Well E - Production data after completion operation
Date
Choke P
WII
UiI
Water
mm
bar
SmJ/d
cut
14.11.93 17
138 958 0
17.11.93 24.8 109
1.564 0
02:12.93 24.2
81
449 0
17.12.93 24.2
80 348 0
01.01.94 53.9 80 210
0
For all wells, except well B, the potential for sulphate scale
formation
was
evident due
to
high concentrations
of
sulphate
(eg. high sea water content) and high calcium.
High GR-readings readings are normally scen
when
sulphate
scales
of
barium
and
strontium are formed.
In
well A,
the pres
ence of sulphate scale incorporating NORM was detected. Thus
the observed formation damage could
be
due to both natural
formed barium sulfate scale and calcium sulphate
from
lost
brine.
In
well B,
no
increase
in
radiation was detected after production
decline indicating precipitation
of
calcium and inhibitor.
SCALE DISSOLVERTREATMENTS
In
order
to
remove the formation damage
and
restore
the
produc
tivity, scale dissolver treatments were carried out
in well A, C,
D
and E.
Well
A,
C and D
The dissolver treatments were carefully designed and carried out
according
to
the following procedure:
A scale dissolver formulation incorporating EDTA was
chosen from laboratory studies.
Solutions were bullheaded except
in
one operation well
D,
1st treatment) where coiled tubing
was
employed.
A spear
of
sea water (*) containing demulsifier and
scale inhibitor was pumped ahead of the scale dissolver.
Sea water containing scale inhibitorwas used
as
the
displacement fluid.
The shut in period was set to
48
hours
t
achieve
optimum reaction temperature and enough time for
chemicals
to
react.
To obtain the highest possible dissolution rate, sea
water was pumped every 4 hours during the shut
in
77
period to make sure that fresh dissolver contacted the
CaS0
4
scale
in
the near wellbore area.
Based
on
ideal conditions, the dissolver front
was
calculated to be displaced 2 m out from the wellborc.
(*)
Seawater was replaced by 2 KCI
in
the sccond
treatment ofwell D
WellE
In
order to reveal the nature
and
composition ofthc problem, a
diagnostic treatment with a very limited amount of dissolver
chemicals
was
planned. The results from this treatment provided
the basis for the decision
on
whether
to
initiate another
and
larger dissolver treatment.
15
m
3
of chemicals were initially pumped
down to the
perfora
tion interval
and 1/3
of the tubing
was
filled with chemicals.
Agitation
and
addition of
fresh
chemicals
to the
gravel
pack
was
then
achieved
by
pumping small volumes every 4 hours during
the 48 hour shut-in period, giving a 0.6 m radial displacement of
the fluids into the formation.
POST EVALUATION
OF
BACK- PRODUCED AQUEOUS
PHASE
Well A
The backflow profile was established
by
offshore monitoring of
pH
and level
of
scale dissolver. See Figure 2.
Based
on
these analyses, the sampling period
was
established.
Onshore analyses
for
ion compositions
were
carried out
on
the
same samples using Inductively Coupled Plasma Spectrometry
lCP) and volumetric titrations Mettler Auto Titrator).
The amount of dissolved scale
was
estimated t1 om material bal
ance calculations based
on
the percentage
of
formation water
and seawater/dissolver solution
in
back produced water
In
principle,
all
ions or species that do not take part
in
any physi
calor
chemical reaction during the dissolver process
can be used
as
indicators for the formation water content.
As no
such species
exist, a comprimise
was
chosen.
The concentration of magnesium ions (Mg
2
was selected as the
best indicator because sea water dissolver solvent) is
high
and
formation water low
in
magnesium. More importantly, there are
few
slightly soluble magnesium compounds,
and the one which
may be
present downhole MgC0
3
) is
relatively unaffected
by
EDTA
at
pH
8/10/2019 SPE-30086-MS
4/12
4 Forma tion Da ma ge due to Losses of C a- ba se d B r in e a nd H o w
Wa s
Revealed
Through
Post Evaluation of Scale Dissolver
an d
Scale Inhibitor Squeeze
Treatments
SPE 30086
Th e concentration of excess calcium ions throughout the back
flow period
is
not balanced by chloride or sulphate ions. The
surplus of Ca'+ ions is reported as calcium carbonatelcalcium
chloride CaCO/CaCI,).
(Bicarbonate was not included
In
the ion analyses.)
Th e
rationale for doing this is as follows:
Th e dissolver has probably dissolved some
CaC0
3
, bu t to as
cribe the whole surplus of Ca'+
to
dissolved
CaC0
3
is not realis
t ic based on solubility considerations.
Large concentrations of bicarbonate and carbonate wil l form
downhole due to the injection of the alkaline dissolver solution:
Th e
calculations are based on excess ions in backproduced water
phase and rate/volume of produced water.
In retrospect, it was realized that fewer samples than optimum
were taken during the.backflow and variations in the ion pattern
may not have been properly detected. An underestimate
of
the
amount of material mobilised and removed is therefore likely.
WellC
Fol lowing the disso lver t reatment a total number
of
34 water
samples were taken during a per iod of 200 hours. Analyses of
pH and scale dissolver
)
were carried out offshore. Ion analy
ses were determined onshore.
is not known
if
CaCI, exists in solution (aq) or as solid salt (s)
CaCI, (s,aq) + 2Na\aq) = 2NaCI (s) +
Ca \aq)
High concentrations of CO/ subsequently suppress the rate
of
dissolution
ofCaC0
3.
CaS0
4
is re turned at a constant level from 14 to 40 hours. The
presence of CaCO/CaCI, is again observed when the concentra
tion of chloride starts to climb (35-60 hours). This creates a fa
vorable condition for NaCI precipitation as suggested for well
A
Therefore the amount of CaC03 should be less than reported
830 kg).
Using the same arguments as for well A, the quantit ies of solids
mobilised and removed during the backflow period were deter
mined. Th e results are plotted in figure 5
The backflow profile in well C is different from well
A
The ma
jo r
part of the mobilised material is returned between 30 and 80
hours suggesting that the brine was lost further out in the forma
tion. Also, a larger amount
of
brine was removed in well C com
pared to well A
CO
2
(aq)
HC 0
3
'
C O / + 2 H P
CO, (oil)
CO, (aq) + OH'
HC 0
3
+ O H
is conceiveable that precipitation of sodium chloride will oc
cur when concentra ted ca lc ium br ine is mixed with alka line
EDTA solution containing sodium ions. This happens because
sodium chloride is much less soluble than calcium chloride
The reaction explains why dissolved quantit ies are reported as
CaCO/CaCI
2
Th e total quantit ies removed during the dissolver operation are
summarized in table 6
Dissolved material during the backflow period is shown in fig. 4
Th e
plo t shows a major peak equivalen t to 7000 mg/I (7 kg/m
3
)
of CaCI
2
which
is
observed be tween 1.5 and 2.5 hour s a fte r
opening the well. Later on, the level stays constant. Th e conen
tration of CaS0
4
in the return fluid is relativelyconstant over the
14
hour backf low period. This may indicate that the sulphate
scale i s evenly distributed from the gravel pack into the near
wellbore area.
WellD
Th e quantities of solids mobilised during the 10 hours backflow
per iod was de te rmined as decribed above for A and C, and the
results are plotted in figure 6.
Th e
plot shows elevated amounts
of
CaCI one peak appearing
a t 1-2 hour s and another broader peak at 4 -10 hours. A minor
amount o f C aS 0
4
is observed after 1 hour, but the bulk is pro
duced back after 4-10 hours.
A small amount o f B a S 0
4
is
mobilised after 2-3 hours. This sug
gests that the dissolved BaS0
4
was located in the gravelpack. At
that time both pH and dissolver return are at their highest level.
A large amount (peak) of CaCO/CaCI, is observed between 2.5
and 5.5 hours. This happens when the concentration
of
scale dis
solver in the return (and
Na
ions) is at maximum (38 ). Also,
this period starts with maximum concentration of Ca'+ and CI'
ions. The concentration
of
calcium continues
at
a high level
while chloride drops sharply, suggesting that the solubility of so
dium chloride is exceeded and NaCI salt is precipitated.
The disso lver t reatment also mobi li sed a constan t amount
of
BaS0
4
throughout the initial backflow period indicating that the
conditions were favourable high pH, sufficient concentration of
EDTA) for dissolving this hard and difficult scale. This also sug
gests that a significant amount of
CaC0
3
is dissolved
Prior to the disso lver t reatment , the produced water of well D
contained enhanced levels of Ca'+ (6226 mg/l compared to 1612
mg/I in the formation water).
If
cor recti on is made for the en
hanced Ca'+ levels, both the broad peaks of mobilised CaCl, dis
appear while the amount of CaC0
3
diminishes
figure
7). The
amount ofCaS0
4
and BaS0
4
remains the same.
The estimated total amounts of material removed during the
14
hour backflow period were:
1700 kg CaCI,
300 kg CaS0
4
6 kg
BaS0
4
45 0 kg CaC0
3
/CaCI,)
This indicates that the lost brinc CaCI/CaBr,) is located further
out in the formation than the CaSO/BaS0
4
scale, and that the
dissolver solution has not penetrated the area of lost brine. This
observation may also suggest that when CaS0
4
is
formed, sul
phate ions from the passing sea water /injection water picks up
78
8/10/2019 SPE-30086-MS
5/12
SPE 30086
K.
Lejon, J. Tuxen Thingvoll, E.A. Yolien, Statoil, P. Hammonds, Baker Performance Chemicals
5
Ca
2
ions from the br ine and move into, or to the vicini ty
of
the
gravel pack where deposition occurs.
The
second dissolver treatment in well D with limited volume of
solvent (EDTA) also removed some CaS0
4
and CaC0
3
in
addtion to iron. The backproduced aqueous phase was deficient
in
chloride ions, indicating that precipitation
of
NaCI may have
occured.
The analyses and post evaluation of the second dissolver treat
ment was somewhat difficult due to lack
of
analytical results
from the backflow period. Low water cut and formation
of
stable
oil/water emulsions made
it
difficult to obtain enough water for
ion analysis.
WellE
The
quantities
of
solids mobilised during the 22 hours backflow
period are presented in
figure 8.
The plot shows that the return
of CaS0
4
is minor during the first
4 hours, but later the content increases and reaches a constan t
level from 5 to 22 hours after which sampling was terminated.
As observed for well A precipitation ofNaCI has occured con
current with an increase
in CaCO CaCI
2
The bulk part of the
material mobil ised is bel ieved to be CaCI
2
based on solubility
considerations.
PRODUCTION IMPROYEMENTS
Well
A
As described in the previous chapter a relatively large amount
of
CaS0
4
scale was removed from the gravel pack or near wellbore
area.
In table 4, well tests before and after the dissolver treatment are
listed. An immediate increase
in productivity was observed, the
oil rate increasing from 2871 Sm
3
/d to 3465 Sm
3
/d. However ,
this inc rease on ly lasted a few days. 10 days la te r t he well tes t
showed an oil rate
of
2743 Sm
3
/d. In the foll owing weeks the
productivity showed a further decrease. Due to the short term ef
fect on productivity no data acquisition programme was carried
out
in
this well.
Despite the short effect
of
the dissolver treatment, the net profit
from increased oil p roduct ion more than balanced the opera
tional cost, including chemicals.
Table
4: Well A -
Production
data
before and a ft er
dissolver
treatment
Date W P
Qoi
Water PI
bar Sm
3
/d
u
Sm
3
/d/bar
14.12.93be
77
2.871
26.5
92
fore
06.0
I
94aft
77 3.465
31.2
177
er
12.01.94aft
75
2.743
34 88
er
79
WellC
The well was put on product ion at a rate
of
approximately 1000
Sm
3
/d. This rate was chosen to min imize any process prob lems
due to high concentration of spent dissolver fluid and high pH.
The
production rate was increased
in
s tcps over a period of 24
hours.
Before the scale dissolver treatment, the well produced with an
oil rate of 2900 Sm
3
/d at a wel lhead pressure
of
76 bar. After
the t reatment the well was producing 5700 Sm
3
/d at maximum
choke setting and a wellhead pressure
of95
bar.
During the sampling period wellhead pressure decreased from
94 to 84 bar and water cut increased from 2 to 15 .
A well tes t performed a week after the treatment , showed a loss
in productivity (PI) from
210
to 80 Sm
3
/d/bar. The production
data are given in table
5.
Further well tes ts 2 and 3 weeks later also showed a decrease
in
productivity, but the well was sti ll producing at a considerably
higher PI and rate than before the treatment.
Table
5:
Well
C -
Production data before and after
dissolver
treatment
Date
W P
Qoi
Water
cu t
PI
bar
Sm
3
/d
Snl d bar
02.11.93 76 2.900 0 31
before
24.12.93
95 5.700 1 210
after
30.12.94 84
3.960
80
after
To gather more information on how the t reament affectcd the
productivity it was decided to perform a PLT/BU. The most in
teresting findings are given below:
A PLT prior to the dissolver treatment gave a
contribution
of30
of
total flow from the lower
1/3 of
the gravel packed interval. The PLT after the treatment
gave an increase
in
contribution to 46 , indicating a
stimulation effect across the lower part of the interval.
All water production was coming from the lower
1/3 of
the gravel packed interval
PI , at a total rate
of 3000 Sm
3
/d, increased from 33
Sm
3
/d/bar to 128 Sm
3
/d/bar
Pressure drop across the gravel pack decreased form
93.9 bar to 22.4 bar.
As can be seen from
figure
9, the well p roduced at a higher oil
rate dur ing January - April 94 compared with the well test pet
formed prior to the treatment.
The benefical effect
of
the dissolver trcatmcnt is also reflected
in
the economic results.
The
operational cost for the treatment was
estimated to 100.000. As a comparison, the extra oil produced
during this period was worth about 40 million.
8/10/2019 SPE-30086-MS
6/12
6
Formation Damage due to Losses of Ca based Brine and How Was Revealed
Through
Post Evaluation of Scale Dissolver and Scale
Inhibitor
Squeeze
Treatments
SPE 30086
WellD
The first dissolver treatment
in
Well D gave an increase in well
head pressure that enabled the production rate initially to be kept
at the target rate
of
1100 Sm
3
/d, but shortly after the operation
the wellhead pressure started declining
Three months after the treatment the wellhead pressure was back
at the same level as before. The positive scale dissolver result
experienced in well E next section), triggered another treatment
in
well D using the same procedure and dissolver volumes as in
well E After the 2nd treatment the wellhead pressure was stable
at a high level for several months, maintaining the production
rate at the target of 1100 Sm
3
/d.
The results are summarized
in
table
7
Our study indioates that diagnostio treatments with
small dissolver volumes is as effective and durable as
large volumes.
Monitoring programmes and post evaluation strategies
for soale dissolver treatments are essential.
For
gravelpaoked wells, the brine system has been
ohanged to sodium bromide NaBr)
if
high brine losses
are expected.
AKNOWLEDGEMENT
The authors wish to thank the management of Statoil for pennis
sion to publish this paper.
REFERENCES
WellE
Production data in table 3 clearly show that well E experienoed
a dramatic decrease in productivity prior to the dissolver treat
ment. There was a conoern that the well oould be oompletely
blooked, thus preventing the pumping of soale dissolver
solution.
The treatment enabled the well to be produced at an oil rate that
was above the initial rate following the gravelpack operation, in
dicating that the gravel paok operation had oaused formation
damage that now was removed.
The wellhead pressure deolined slightly during the next 2
months, but thenstabilized. For the next 8 months no further de
crease in produotion rate or wellhead pressure was observed.
Remarkably, the limited scale dissolver operation resulted in a
full restoration
of
well produotivity. Aooordingly, it was decided
to design the seoond operation in well D the same way.
The results are summarized
in
table7.
CONCLUSIONS
The major reason for the deoline in produotivity in gravel paoked
wells has been confirmed to be due to heavy losses
of
calcium
based brine during completion operation. Breakthrough of sea
water has led to precipitation
of
CaS0
4
Use
of
sea water as sol
vent for scale dissolvers and scale inhibitors has also added to
the deleterious effects.
The observations and findings have lead to fol lowing conclu
sions and recommendations:
Formation damage is related to the volume of brine lost
during completion operation.
Lost Ca-brine during gravel paoking has been found to
be present in the formation after many months
of
produotion.
Loss
of
oompletion fluids during gravel paoking should
be minimised and monitored properly.
Laboratory compatibility studies
of
treating chemicals
should be initiated if heavy losses
of
completion brine
has occurred.
Use of soale dissolver has been identified as an effective
and economical method for repairing formation damage
related to sulphate scale.
80
1
2.
3
4.
5
6
7
Schmidt, T., and S0reide, F., Mineral Soale in
Gravelpaoked Wells , Paper no. 56, Corrosion 94,
NACE
Martinko, B., Investigation of Chemical
Compatibility
of
Fonnation Waters with CaCl
2
and
CaBr
2
Brines , NAFTA 44,
p
265-269 1993)
Ali, S A., Javora, P. H Guenard, J H and Kitziger,
F. W., Test High-Density Brines For Formation
Water Interaotion , Petroleum Engineer International
July 1994)
Paul, J.M., and B.D. Fieler, A new solvent for
Oilfield Scales , 67th Annual Conference, SPE no.
24847.
Chelant Stability Constants, Akzo Chemioals Ltd.
Produot literature.
Fieler, E.D., Applioation and evaluation
of
soale
dissolver treatment , paper 58, Corrosion
94 NACE.
Hunton, A.G., Improvements in Scale Dissolver
Formulation , Oilfield Chemical Symposium, Geilo
1994)
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ATTACHMENT
1
Table 2:
Calcium
Based Brine
Injected
and
Lost
During Completion Operation
Type
*)
Specific Lost Perforation length
Gravity
m
3
)
Well
A CaCl
2
1.38 1000 57 m
WellB CaCl
2
1.36
500 7 m
WellC CaCl
1.33 400-450
35 m
WellD
CaBr
2
1.68 450 27 m
WellE
CaBr
2
1.63 150 26m+15 m
*)
The brines contain both CaCl
2
and CaBr
2
.
Low density brine is low
in
CaBr
2
.
Hig h d en sity b rine is rich in CaBr
2
Table 6: Compounds Removed Precipitated **)
During
Dissolver Treatments
CaCI
2
CaS0
4
CaCO/CaCI
2
BaS0
4
SrS0
4
NaCI
Well A 1700 kg 300 kg 450 kg
5 kg 0 0
WellB
- - -
- - -
WellC
6 20 0 k g
280 kg 830 kg
okg 0 0
Well
D, no 1 *) 5.5 kg/m
3
1.2 kg/m
3
4 k g/m
3
I kg/m
3
0 0
Well D no 2 *)
1.2 kg/m
3
1.5 kg/m
3
8 k g/m
3
0 0 -15 kg/m
3
)
Well E *) -
5 k g/m
3
17 kg/m
3
0 0 - 3 kg/m
3
)
*) Total amount dissolved not determined because volume produced water was not recorded
**)
Precipitation
of
sodium chloride
Table 7: O il Production Improvements and Duration of Dissolver Treatments kg)
Q Q
Maximum Duration
Other
immediate effects
before)
after)
improvement
4)
Comments)
Sm
3
/d)
Sm
3
/d)
Sm
3
/d)
Well A
2871
3465
594 10 days PI increase: 92
to
77 Sm
3
/d/bal
WellB
- -
- -
No dissolver treatment)
Welle
2900 5700 2800 70-120 days PI increase:
3
t0210 Sm
3
/d/bal
Well D I
518
986 468
8
months
P
WH
inc re as e: 82 to 132 bar
Well E 3)
210 1542
1332 >8 months
PwHincrease: 80-136 bar
P
WH
Wellhead pressure
1)
First dissolver treatment, large dissolver volume injected, coiled tubing
2) Second dissolver job, small dissolver volume injected, pump job, bullheading
3)
Small dissolver volume injected, pump job, bullheading
4) Period of increased oil production
*)
O il r ate ke pt a t a bo ut 1 100 S m
3
/d due to production limitation
8
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ATTACHMENT
Figure
WELL
B: CalciumConcentration in Produced
Water
500
1500 - - - - - - t - - - - - - - - l l ~
3000 +--------------- ----{
4500
..
= = = ; = = = ; ~ = = ; j ~ = = = ; ; = = = = ; ~ ~ ~ ~ = T I
Iseve,ol
month,l 8
hours pe lool
~ ~ I
4000 l ~ ~ ~ = ~ I H ~ = = = = = : J -
3500 -1--------------.---1 \------_---\l.ill )..1JJlllJ - =L.- tl
Q
5 +----== - - =T-=----H
+
ij 2000
+-- - - - - - - - - - - -7J
N N ~ ~ ~ ~ ~ ~
g
Semple number
Figure
Well A Return Curves for
Scale
Dissolver and
pH
2nd y-axis
7
10,5
10
9,5
8,5
7
9 10 11 12 13 14 15 16 17 18
Hours
OL,....-- '--'- '--..l-_L---'-_..l-_L---'-_..l-_L----'-_..l-_-'---==----- --l Ill -.......
. .-----
o
40
35
30
15
25
20
15
.
10
8
8/10/2019 SPE-30086-MS
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140.00
120.00
1100.00
80 00
i
60.00
40 00
] 20.00
0.00
20.00
Figure 3
WELL A : EXCESS ION CONCENTRATIONS
me/l
/1
0
1\
-...
@;]
\
-.
.
-
r ....
........
/
.-
=:::::
~
~
~
7
I I a
Ba
8 4
C[
11 111 5
1
2 4 6
Figure 4
WELLA: Compounds Removed During Dissolver Treatment
12000
10000
i
E
6000
B
l:j
4000
0
2000
1.5 2 75 3.25 3 75
Hours
83
4.75 5 75
7 75 11.17
14 75
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igureS
WELL
Compouuds
dissolved duriug dissolver treatmeut
4 y
12000 ~ _ A ~ j
10000
ll
8000 ~ ~ ~ ~ _ _ i
I
6000
+ - - - - - ~ - - - = = ~ = = ~ - y
4000 ~ V
2000
Hours
Figure
Well D: Compouuds Removed
Duriug Dissolver Treatmeut
12 00
10 00
8 00
l
6
e
6 00
rJ
-l:
g
4 00
2 00
0 00
0 5 1 5 2 5 4 5
Hours
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Figul c 7
Wcll
D:
Compounds Removcd Dul ing Dissolvcl
re tmcnt
Correction Made
for Enhanced Levels
ofCa
in Produced
Waler Prior to Treatment
12 00
10 00
;;,
i
g
8 00
]
J
6 00 -
+l
4 00
=
2 0 0
0 00
0 5
1 5
2 5 4 5
Hours
Fignl e 8
Wcll E: Componnds Removcd Dnl ing Dissolvcl re tment
10
90 00
.
80 00
1
__l _
_ _ ~ - - - - 1 - - - d . - - - - ~ - L - - - l - - - - - - - - - - - - - - . L - - - - L - _ _ - I
70 00 t - - - - - I - - - - - j , - - - - t - - -+ - - - \ -7
I
60 00
50 00
IcaC03fCaC1
2
1
]
40 00
J
30 00
i l
20 00
+l
10 00
l
0 0 0
C
-10 00
-20 00
1 1
- 30 00 - -- -
___- - - - . J _ _ ___ _ __ __ _ ___
_ _
_ _
_ _ _ ___ _ _ _
..J
0 5
1 5
4 5
Hours
85
10
13
16 19
22
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Figure 9
Well
Production
rates
5
50
I
I
4
7 J ~ 1 2 d l l Y S
/
355
Dissol ver treatment
25
55
5
r
: 45
4
35
S
3
25
.0
2
8
5
o
5
ys