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Mary L. Barrett, Ph.D.Mary L. Barrett, Ph.D.
ConsultantConsultant
Shreveport, LAShreveport, LA
mbarrett@centenary.edumbarrett@centenary.edu
2121stst
International Petroleum Environmental ConferenceInternational Petroleum Environmental Conference
Oct. 14Oct. 14--16, 201416, 2014
Houston, TXHouston, TX
Historic Oilfield Arsenic Sources: Implications for Pit Groundwater Models
Mary Barrett, Consultant, Shreveport, LA 71104 (mbarrett@centenary.edu)
A popular model for elevated arsenic in groundwater plumes uses reductive dissolution of
iron oxides. Here, adsorbed natural arsenic is released into solution when oxides are
dissolved under reducing conditions. A groundwater reducing zone is commonly
modeled as due to crude oil, benzene or organic-rich clays. This model is increasingly
used in oilfield and related environmental studies to explain elevated groundwater arsenic
and iron below pits. Anthropogenic reasons may not be considered. Potential historic
oilfield arsenic sources are related to corrosion control, original produced waters, or weed
control. Oilfield pits were main impact areas of these arsenic sources. Arsenic or
organic compounds were used in two ways for corrosion control: a) added to well acid
jobs from the late 1930s into the 1970s, mainly; and b) added to produced fluids of 1950s
oilfields of low-pressure oil wells and high water production. Produced fluids’ corrosive
nature was commonly judged by elevated dissolved iron. Impacted oilfield pits carry
similar arsenic and iron groundwater signatures as put forth in a “natural” model. Means
for recognizing oilfield-related arsenic impacts include spatial distribution of
geochemical signatures, knowledge of original produced water chemistry, and associated
groundwater arsenic and chlorides significantly above local and regional patterns.
1
Consider issues for a pit arsenicConsider issues for a pit arsenic
groundwater model if a productiongroundwater model if a production
corrosion arsenic inhibitor (1950s) wascorrosion arsenic inhibitor (1950s) was
usedused
–– Review history of arsenic corrosion inhibitorsReview history of arsenic corrosion inhibitors
–– Reminder of oilfield chemistry & ironReminder of oilfield chemistry & iron
–– Review As pit groundwater modelReview As pit groundwater model
assumptionsassumptions
–– Look at probably the best example in U.S. toLook at probably the best example in U.S. to
address questionsaddress questions
AuthorAuthor’’s Use of Public Records for Her Opinionss Use of Public Records for Her Opinions
The example from LSJ Field, LA, has large public recordThe example from LSJ Field, LA, has large public record
available due to litigation (court records in one case) andavailable due to litigation (court records in one case) and
especially due to LA Act 312 (2006+) & LA Office ofespecially due to LA Act 312 (2006+) & LA Office of
Conservation (OOC) oversight of oilfield cleanup of allConservation (OOC) oversight of oilfield cleanup of all
oilfield litigationoilfield litigation ““legacylegacy”” sites (reports, raw data; hearingsites (reports, raw data; hearing
recordsrecords……))
I was a defense expert retained in the two cases thatI was a defense expert retained in the two cases that
generated public records above; geologist, oilfieldgenerated public records above; geologist, oilfield
historian (environmental companies responsible forhistorian (environmental companies responsible for
cleanup plans:cleanup plans: PisaniPisani & Assoc., ICON; some& Assoc., ICON; some GeosyntecGeosyntec))
My work on last case ended Feb. 2014; I have pursuedMy work on last case ended Feb. 2014; I have pursued
this research since then, not retained by anyone, nothis research since then, not retained by anyone, no
discussions with other past experts (MY OPINIONS)discussions with other past experts (MY OPINIONS)
2
(Example of Heavy Oil Earthen Tank Farms, SE Texas, 1900s(Example of Heavy Oil Earthen Tank Farms, SE Texas, 1900s--
1920s; 1990s subsurface regulatory records)1920s; 1990s subsurface regulatory records)
(Barrett,
2006)
Groundwater arsenic (As) above 0.01 mg/lGroundwater arsenic (As) above 0.01 mg/l
occurs in Louisiana (natural variability + ?)occurs in Louisiana (natural variability + ?)
Groundwater arsenic above 0.01 mg/lGroundwater arsenic above 0.01 mg/l
occurs in oldoccurs in old ““legacylegacy”” oilfield areasoilfield areas
Groundwater arsenic models &Groundwater arsenic models &
assumptions in the U.S. are affected byassumptions in the U.S. are affected by
larger studies from the northern andlarger studies from the northern and
northeastern U.S. and internationalnortheastern U.S. and international
3
Arsenic models are useful, but extrapolated toArsenic models are useful, but extrapolated to
Gulf Coast oilfield regions of different geology &Gulf Coast oilfield regions of different geology &
hydrogeology, and may not consider impactshydrogeology, and may not consider impacts
fromfrom ““oilfield chemistryoilfield chemistry””
““Oilfield chemistryOilfield chemistry”” & its potential component& its potential component
impacts (esp. iron) have a history, & pits oftenimpacts (esp. iron) have a history, & pits often
record itrecord it
The detailed history of oilfield pitsThe detailed history of oilfield pits----how used, itshow used, its
shallow fluid movement patterns, howshallow fluid movement patterns, how
““disturbeddisturbed”” over timeover time——is importantis important
LA groundwater published
arsenic record limited, but
Miss. R. alluvium waters can
be elevated (USGS 2000)
Modern work, shallow
groundwater As values
from S. LA, 78 wells,
up to 0.200 mg/l
(Yang et al, 2014)
4
AnAn equilibriumequilibrium diagram fordiagram for
system Assystem As--OO22--HH22OO
Iron oxides common in our LAIron oxides common in our LA
sedimentsediment
As bound to iron oxides,As bound to iron oxides,
released into GW withreleased into GW with
““reductive dissolutionreductive dissolution”” whenwhen
some cause for a reducingsome cause for a reducing
environment (organics, oil,environment (organics, oil,
clayclay……))
Iron oxides reIron oxides re--precipitate asprecipitate as
GW move into oxidizing zone,GW move into oxidizing zone,
also locks up Asalso locks up As
Does not address AsDoes not address As
desorption (phosphates)desorption (phosphates)
Model looks for relationsModel looks for relations
between ORP, Fe, Asbetween ORP, Fe, As
Amorphous Iron Precipitates in the OilfieldAmorphous Iron Precipitates in the Oilfield——longlong
history in oilfield chemistryhistory in oilfield chemistry
((Hydrous ferric oxidesHydrous ferric oxides——HFOsHFOs))
1950s Oklahoma Oilfield Water Treatment (Powell & Johnson, 1952)
5
PesticidesPesticides
–– Concordia Parish cotton,Concordia Parish cotton,
1910+1910+
–– Vegetable gardens, treesVegetable gardens, trees
–– Cattle dipping vatsCattle dipping vats
HerbicidesHerbicides
–– Inorganic & organicInorganic & organic
–– Land & aquatic weed killerLand & aquatic weed killer
Oilfield usageOilfield usage
IndustrialIndustrial
–– Corrosion inhibitorCorrosion inhibitor
–– othersothers
Griffin presentation on
oilfield legacy litigation (2006)
U. S. OilfieldsU. S. Oilfields
–– Studies elsewhere fromStudies elsewhere from
late 1950s (White) throughlate 1950s (White) through
20052005
–– As values range from NDAs values range from ND
to 1.6 mg/lto 1.6 mg/l
–– LA data from 1989 andLA data from 1989 and
onward range from ND toonward range from ND to
0.5 mg/l0.5 mg/l
–– 7 studies!7 studies!
No produced waterNo produced water
analysis (As) for myanalysis (As) for my
exampleexample
S. Louisiana & GOMS. Louisiana & GOM
1989 and later publications1989 and later publications
6
OilFieldOilField Arsenic Corrosion InhibitorsArsenic Corrosion Inhibitors
Historic U. S. SummaryHistoric U. S. Summary
Acid Corrosion InhibitorAcid Corrosion Inhibitor
–– 19321932, Michigan oilfield acid, Michigan oilfield acid
job, limestonejob, limestone
–– 19341934, arsenic is important acid, arsenic is important acid
job inhibitor, but organics nowjob inhibitor, but organics now
availableavailable
–– Early 1960sEarly 1960s, decrease As, decrease As
usage, but good for highusage, but good for high--TT
wellswells
–– In 1970sIn 1970s, arsenic inhibitor, arsenic inhibitor
phasephase--out in acid jobsout in acid jobs
Production Corrosion InhibitorProduction Corrosion Inhibitor
–– 19491949, Reported first usage in, Reported first usage in
Texas Wilcox trend (Jones,Texas Wilcox trend (Jones,
1955)1955)
–– 19541954, CA survey, 17 fields;, CA survey, 17 fields;
65 % pumping wells used65 % pumping wells used
inorganic inhibitors (arsenicalinorganic inhibitors (arsenical
compounds and chromates)compounds and chromates)
(Hill & Davie, API, 1955)(Hill & Davie, API, 1955)
–– 19571957, LA Stream Control, LA Stream Control
Commission minutes reportCommission minutes report
phasephase--out of oilfield arsenicout of oilfield arsenic
corrosion pellets, strippercorrosion pellets, stripper
fieldsfields
–– 19601960, general end of U. S., general end of U. S.
oilfield arsenic corrosionoilfield arsenic corrosion
inhibitors (Gardner, 1960);inhibitors (Gardner, 1960);
move to organicsmove to organics
Iron & 1950s Arsenic Inhibitor in ProducedIron & 1950s Arsenic Inhibitor in Produced
Water (Wilcox Trend, Texas)Water (Wilcox Trend, Texas)
Jones (1955)
(Jones, 1955)
7
1945 analysis, 141945 analysis, 14 ppmppm ((ClCl 13,82013,820 ppmppm))
1959 analysis, 901959 analysis, 90 ppmppm ((ClCl 80,90880,908 ppmppm))
1970 analysis, 2151970 analysis, 215 ppmppm ((ClCl 101,135101,135 ppmppm))
1995 analysis, 21 mg/l (1995 analysis, 21 mg/l (ClCl 59,44959,449 ppmppm))
GENERAL OBSERVATION: While an old oilfield may have used
arsenic inhibitors within the 1950s, more likely is that many oil
fields had many possible decades (into 1970s, esp.) of elevated
dissolved iron in produced water, and thus into pits
(OOC, Poppadoc hearing files, 2009;
Norman reliance documents, v. 52-53)
Discovered in 1942, Tensas & ConcordiaDiscovered in 1942, Tensas & Concordia
Parishes, LAParishes, LA
Major producing field for The CaliforniaMajor producing field for The California
Company (Standard Oil of CA)Company (Standard Oil of CA)
Both unit (Cretaceous & some Tertiary age) &Both unit (Cretaceous & some Tertiary age) &
lease productionlease production (Wilcox Fm mainly)(Wilcox Fm mainly)
Outline of remaining presentationOutline of remaining presentation
–– Public records supporting 1950s arsenic inhibitor usePublic records supporting 1950s arsenic inhibitor use
–– Modern shallow groundwater geochemistry around leaseModern shallow groundwater geochemistry around lease
emergency pit usage areasemergency pit usage areas
8
(Modified from Pisani report, 2008; OOC
Poppadoc file # 006-007)
Letters, OctLetters, Oct--Nov 1950, north side of field, testNov 1950, north side of field, test
program for chemical inhibitors, liquid injectorsprogram for chemical inhibitors, liquid injectors
and solid pelletsand solid pellets
–– Oct 23:Oct 23: ““A most promising type of inhibitor is sodiumA most promising type of inhibitor is sodium
arsenitearsenite, which we intend to make use of in the very, which we intend to make use of in the very
near future.near future.””
–– Oct 27Oct 27:: ““have been advised of the promising results ofhave been advised of the promising results of
sodiumsodium arsenitearsenite in corrosion mitigation workin corrosion mitigation work””
–– Nov 13Nov 13:: ““In view of the fact that it is intended to try outIn view of the fact that it is intended to try out
sodiumsodium--arsenitearsenite pellets in the very near future, it is feltpellets in the very near future, it is felt
desirable to postpone any trial of the downdesirable to postpone any trial of the down--hole injectorhole injector
until results from that method of corrosion inhibition canuntil results from that method of corrosion inhibition can
be obtained.be obtained.””
(OOC Poppadoc hearing, 2009; Miller/ICON reliance docs,
v. 25, Exhibit P-1066)
9
(Poppadoc hearing, 2009; Miller/ICON reliance docs, v. 28;
Tensas/Miller 02469-02470)
WW--41, an arsenic corrosion inhibitor, is one41, an arsenic corrosion inhibitor, is one
example of arsenic corrosion inhibitors usedexample of arsenic corrosion inhibitors used
in some 1950s oilfields of the U.S.in some 1950s oilfields of the U.S.
Its history is available in public documents.Its history is available in public documents.
10
The California Oil CoThe California Oil Co
CaliforniaCalifornia ReseachReseach
CorpCorp
California SprayCalifornia Spray--
Chemical CorpChemical Corp
California ResearchCalifornia Research
CorpCorp (As & oilfield corrosion)(As & oilfield corrosion)
–– Dec 1950, 2 patents,Dec 1950, 2 patents,
RohrbackRohrback et al (1954)et al (1954)
–– Mar 1951, 2 patents,Mar 1951, 2 patents,
RohrbackRohrback et al (1953)et al (1953)
–– Dec 1951, patent,Dec 1951, patent,
RohrbackRohrback et al (1953)et al (1953)
–– Oct 1954, patent,Oct 1954, patent,
FrisiusFrisius (1959)(1959)
California SprayCalifornia Spray--
Chemical CorpChemical Corp
–– 1952, Patent application1952, Patent application
granted in 1953 forgranted in 1953 for ““OrthoOrtho
WW--41,41,”” also used isalso used is ““WW--
41,41,”” for arsenic corrosionfor arsenic corrosion
inhibitor (42 % sodiuminhibitor (42 % sodium
arsenitearsenite) (EPA, 1973)) (EPA, 1973)
(My Opinion from the public record: W-41 was used in the LSJ Field
in the 1950s; organic inhibitors were used after that)
11
Mississippi RiverMississippi River
Alluvium & AquiferAlluvium & Aquifer
–– Braided streamBraided stream
gravels at basegravels at base
–– Mostly pointMostly point--bar sandsbar sands
–– FiningFining--up into levee,up into levee,
overbank, floodplainoverbank, floodplain
sections (8sections (8--12 feet12 feet
here)here)
–– This nearThis near--surface unitsurface unit
is aquifer confiningis aquifer confining
layerlayer
(Modified from Pisani report, 2008; OOC
Poppadoc file # 006-007)
12
The data fromThe data from PisaniPisani & Associates, ICON (G.& Associates, ICON (G.
Miller), is large and of highMiller), is large and of high--quality (quality (GeosyntecGeosyntec
data is less but of highdata is less but of high--quality)quality)
Shallow groundwater data are most reflective ofShallow groundwater data are most reflective of
old impacts & possible controlling influences inold impacts & possible controlling influences in
pit areaspit areas
Groundwater wells at deeper depths (60Groundwater wells at deeper depths (60’’--8080’’, +, +
below surface) do not have arsenic valuesbelow surface) do not have arsenic values
above natural variability range; deeper alluviumabove natural variability range; deeper alluvium
waters are a variation within the largerwaters are a variation within the larger
sediment/water geochemical systemsediment/water geochemical system
Regional Shallow Groundwater Movement,Regional Shallow Groundwater Movement,
near the Mississippi Rivernear the Mississippi River
(back & forth, net movement towards river(back & forth, net movement towards river----PisaniPisani))
(Pisani Report, 2008; OOC Poppadoc records, file # 006-007)
RIVER
LSJ LAKE
13
Pan Am Pit Area, ORP & GW ElevationPan Am Pit Area, ORP & GW Elevation
(not being used enough!)(not being used enough!)
Oilfield legacy records of LA Act 312, at OCC inOilfield legacy records of LA Act 312, at OCC in
Baton Rouge, for background work away fromBaton Rouge, for background work away from
pitspits
Records of Parish dump closures and landfillRecords of Parish dump closures and landfill
monitoring through the LA DEQ (EDMS system)monitoring through the LA DEQ (EDMS system)
–– Tensas landfill, ~ 25 mi away, monitored by ICON forTensas landfill, ~ 25 mi away, monitored by ICON for
Parish, 1994 to 2014 (EDMS # AI 43506)Parish, 1994 to 2014 (EDMS # AI 43506)
–– Two shallow wells, 1997Two shallow wells, 1997--2008,2008, downgradientdowngradient fromfrom
groundwater mound, As <0.02 to 0.162 mg/lgroundwater mound, As <0.02 to 0.162 mg/l
14
PisaniPisani & Associates (2012 report; OOC Tillman& Associates (2012 report; OOC Tillman
records)records) interpreteinterprete the natural range from nonthe natural range from non--
detect (ND) up to 0.12 mg/ldetect (ND) up to 0.12 mg/l
A study in shallowA study in shallow allluviumallluvium across the River inacross the River in
Mississippi has an As range of ND to 0.10 mg/lMississippi has an As range of ND to 0.10 mg/l
(Welsh et al, 2010; also phosphorous)(Welsh et al, 2010; also phosphorous)
ICON data from Tensas Parish landfill, ND up toICON data from Tensas Parish landfill, ND up to
0.16 mg/l0.16 mg/l
Given this & LA data to date, find shallowGiven this & LA data to date, find shallow
groundwater measurements above 0.16 mg/l ingroundwater measurements above 0.16 mg/l in
study area to consider possible anthropogenicstudy area to consider possible anthropogenic
impactsimpacts
15
(oil wells in green, SWD wells in blue)(oil wells in green, SWD wells in blue)
Wilcox
pit
PA pit
16
Applegate Pit (closed ~ 1984)Applegate Pit (closed ~ 1984)
–– 7070’’ x 150x 150’’ x 8x 8’’ (include 2(include 2’’ levee)levee)
–– UsageUsage ““only in emergencyonly in emergency””
Wilcox Pit (closed 1990)Wilcox Pit (closed 1990)
–– 100100’’ x 100x 100’’ x 8x 8’’ (include 2(include 2’’ levee)levee)
–– UsageUsage ““well backwashingwell backwashing”” (and emergency)(and emergency)
Pan American Pit (closed ~ 1984)Pan American Pit (closed ~ 1984)
–– 150150’’ x 200x 200’’ x 8x 8’’ (include 2(include 2’’ levee)levee)
–– UsageUsage ““only in emergencyonly in emergency””
Arsenic in Pit Soils, Sediment, & WatersArsenic in Pit Soils, Sediment, & Waters
55 years after alleged As usage, the pit solids of today55 years after alleged As usage, the pit solids of today
have arsenic ranges within Parish soil rangeshave arsenic ranges within Parish soil ranges
–– Pits modified, rebuilt 2Pits modified, rebuilt 2--3 times during usage3 times during usage
–– Pan Am & Applegate pit closure ~1984; both rePan Am & Applegate pit closure ~1984; both re--closedclosed
(Applegate 2007; Pan Am 2010); Wilcox pit closed in 1990(Applegate 2007; Pan Am 2010); Wilcox pit closed in 1990
–– AsAs analysedanalysed inin ““soilssoils”” range from 1 to 10 mg/kgrange from 1 to 10 mg/kg
A 1984 G & E study found elevated arsenic in ApplegateA 1984 G & E study found elevated arsenic in Applegate
(0.04 mg/l) and Pan Am (0.05 mg/l) pit surface waters.(0.04 mg/l) and Pan Am (0.05 mg/l) pit surface waters.
The 2 ft of bottom sludge ranged from 3 to 4.5 mg/kg AsThe 2 ft of bottom sludge ranged from 3 to 4.5 mg/kg As
(OOC(OOC PoppadocPoppadoc hearing, ICON/Miller & Norman exhibits)hearing, ICON/Miller & Norman exhibits)
GENERAL STATEMENT: Pit surface characteristics mayGENERAL STATEMENT: Pit surface characteristics may
not be innot be in ““equilibriumequilibrium”” with older shallow surface leakagewith older shallow surface leakage
characteristicscharacteristics
17
Applegate LeaseApplegate Lease
–– PisaniPisani 2008 report2008 report
–– (OOC file #006(OOC file #006--007)007)
contours 250 mg/lcontours 250 mg/l
chloride (yellow line)chloride (yellow line)
–– I labeled dissolvedI labeled dissolved
arsenic over 0.160 mg/larsenic over 0.160 mg/l
–– Occurs In Wilcox SWDOccurs In Wilcox SWD
& pit area& pit area
(Fe not measured; ORP not flow(Fe not measured; ORP not flow--thru cell)thru cell)
(OOC Poppadoc file #006-007, ICON 2006-07 data)
Wells screened 8’ – 22’
Below surface
Did not plot
two points:
Cl of 6,600 &
9,080 mg/l
w/ As ND
(<0.01 as “0”)
18
(also Fe, ORP w/ flow(also Fe, ORP w/ flow--thru cells)thru cells)
OOC Poppadoc file # 006-007, Geosyntec Report, 2008
Applegate PitApplegate Pit
–– GeosyntecGeosyntec GW data,GW data,
20082008
–– As relationships withAs relationships with
ORP, FeORP, Fe
–– Salinity and ORP?Salinity and ORP?
19
Applegate PitApplegate Pit
–– AddAdd PisaniPisani data,data,
2012 (no ORP)2012 (no ORP)
–– As vs. Fe trendsAs vs. Fe trends
–– ClCl relation in MWrelation in MW--1 ?1 ?
OOC, Tillman file #007-007, Pisani monitor reports
20
Pan Am Pit GWPan Am Pit GW
–– Higher iron w/Higher iron w/
chlorides under pit;chlorides under pit;
probable oilfield waterprobable oilfield water
source impactsource impact
–– Higher arsenic (overHigher arsenic (over
0.160 mg/l) w/0.160 mg/l) w/
chlorides under pit,chlorides under pit,
probable oilfield waterprobable oilfield water
source impactsource impact
Pan Am Pit GWPan Am Pit GW
–– As v. Fe relationshipAs v. Fe relationship
varies in relation to pitvaries in relation to pit
proximityproximity
–– ORP v. FeORP v. Fe
In GW away from pit,In GW away from pit,
see relationship of ORPsee relationship of ORP
& iron& iron
In GW under pit,In GW under pit,
reducing conditionsreducing conditions
alone not correlatingalone not correlating
with iron (or As)with iron (or As)
amountsamounts
21
Observed ion mobility in GW from pit:Observed ion mobility in GW from pit: ClCl > Fe > As> Fe > As
HFOsHFOs added to emergency pits from produced wateradded to emergency pits from produced water
over decades; As limited, but strongly absorbed byover decades; As limited, but strongly absorbed by
HFOsHFOs when presentwhen present
In pit bottom, oily sludge and sometimes stagnantIn pit bottom, oily sludge and sometimes stagnant
saltwater above this, reducing; GW below reducingsaltwater above this, reducing; GW below reducing
Movement of reducing water withMovement of reducing water with ClCl, Fe (, Fe (++ As) where pitAs) where pit
seepage, into sediment with Fe grain coatingsseepage, into sediment with Fe grain coatings
GW away from pit more oxidizing, see Fe frontGW away from pit more oxidizing, see Fe front
Added As stays within or close to pit boundaries; theAdded As stays within or close to pit boundaries; the
movement ofmovement of addedadded iron further away from pit may beiron further away from pit may be
affecting natural arsenic patterns previously only relatedaffecting natural arsenic patterns previously only related
to iron oxide grain coatingsto iron oxide grain coatings
22
The geochemistry of pit impacts and signaturesThe geochemistry of pit impacts and signatures
is greatly enhanced by historic knowledgeis greatly enhanced by historic knowledge
Arsenic GW models for oilfield pits are useful,Arsenic GW models for oilfield pits are useful,
but oilfield chemistry & past pit functions willbut oilfield chemistry & past pit functions will
strongly modify generic modelsstrongly modify generic models
IRON and possibly phosphorous are importantIRON and possibly phosphorous are important
to further research (i.e., data,to further research (i.e., data, monitoring overmonitoring over
time)time) for pit GW modelsfor pit GW models
Past supplied produced watersPast supplied produced waters’’ dissolved iron todissolved iron to
an oilfield pit may be impacting localized naturalan oilfield pit may be impacting localized natural
dissolved arsenic variabilitydissolved arsenic variability
Chlorides important marker for recognizingChlorides important marker for recognizing
oilfield impact boundariesoilfield impact boundaries

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Barrett IPEC 2014 paper

  • 1. 1 Mary L. Barrett, Ph.D.Mary L. Barrett, Ph.D. ConsultantConsultant Shreveport, LAShreveport, LA mbarrett@centenary.edumbarrett@centenary.edu 2121stst International Petroleum Environmental ConferenceInternational Petroleum Environmental Conference Oct. 14Oct. 14--16, 201416, 2014 Houston, TXHouston, TX
  • 2. Historic Oilfield Arsenic Sources: Implications for Pit Groundwater Models Mary Barrett, Consultant, Shreveport, LA 71104 (mbarrett@centenary.edu) A popular model for elevated arsenic in groundwater plumes uses reductive dissolution of iron oxides. Here, adsorbed natural arsenic is released into solution when oxides are dissolved under reducing conditions. A groundwater reducing zone is commonly modeled as due to crude oil, benzene or organic-rich clays. This model is increasingly used in oilfield and related environmental studies to explain elevated groundwater arsenic and iron below pits. Anthropogenic reasons may not be considered. Potential historic oilfield arsenic sources are related to corrosion control, original produced waters, or weed control. Oilfield pits were main impact areas of these arsenic sources. Arsenic or organic compounds were used in two ways for corrosion control: a) added to well acid jobs from the late 1930s into the 1970s, mainly; and b) added to produced fluids of 1950s oilfields of low-pressure oil wells and high water production. Produced fluids’ corrosive nature was commonly judged by elevated dissolved iron. Impacted oilfield pits carry similar arsenic and iron groundwater signatures as put forth in a “natural” model. Means for recognizing oilfield-related arsenic impacts include spatial distribution of geochemical signatures, knowledge of original produced water chemistry, and associated groundwater arsenic and chlorides significantly above local and regional patterns.
  • 3. 1 Consider issues for a pit arsenicConsider issues for a pit arsenic groundwater model if a productiongroundwater model if a production corrosion arsenic inhibitor (1950s) wascorrosion arsenic inhibitor (1950s) was usedused –– Review history of arsenic corrosion inhibitorsReview history of arsenic corrosion inhibitors –– Reminder of oilfield chemistry & ironReminder of oilfield chemistry & iron –– Review As pit groundwater modelReview As pit groundwater model assumptionsassumptions –– Look at probably the best example in U.S. toLook at probably the best example in U.S. to address questionsaddress questions AuthorAuthor’’s Use of Public Records for Her Opinionss Use of Public Records for Her Opinions The example from LSJ Field, LA, has large public recordThe example from LSJ Field, LA, has large public record available due to litigation (court records in one case) andavailable due to litigation (court records in one case) and especially due to LA Act 312 (2006+) & LA Office ofespecially due to LA Act 312 (2006+) & LA Office of Conservation (OOC) oversight of oilfield cleanup of allConservation (OOC) oversight of oilfield cleanup of all oilfield litigationoilfield litigation ““legacylegacy”” sites (reports, raw data; hearingsites (reports, raw data; hearing recordsrecords……)) I was a defense expert retained in the two cases thatI was a defense expert retained in the two cases that generated public records above; geologist, oilfieldgenerated public records above; geologist, oilfield historian (environmental companies responsible forhistorian (environmental companies responsible for cleanup plans:cleanup plans: PisaniPisani & Assoc., ICON; some& Assoc., ICON; some GeosyntecGeosyntec)) My work on last case ended Feb. 2014; I have pursuedMy work on last case ended Feb. 2014; I have pursued this research since then, not retained by anyone, nothis research since then, not retained by anyone, no discussions with other past experts (MY OPINIONS)discussions with other past experts (MY OPINIONS)
  • 4. 2 (Example of Heavy Oil Earthen Tank Farms, SE Texas, 1900s(Example of Heavy Oil Earthen Tank Farms, SE Texas, 1900s-- 1920s; 1990s subsurface regulatory records)1920s; 1990s subsurface regulatory records) (Barrett, 2006) Groundwater arsenic (As) above 0.01 mg/lGroundwater arsenic (As) above 0.01 mg/l occurs in Louisiana (natural variability + ?)occurs in Louisiana (natural variability + ?) Groundwater arsenic above 0.01 mg/lGroundwater arsenic above 0.01 mg/l occurs in oldoccurs in old ““legacylegacy”” oilfield areasoilfield areas Groundwater arsenic models &Groundwater arsenic models & assumptions in the U.S. are affected byassumptions in the U.S. are affected by larger studies from the northern andlarger studies from the northern and northeastern U.S. and internationalnortheastern U.S. and international
  • 5. 3 Arsenic models are useful, but extrapolated toArsenic models are useful, but extrapolated to Gulf Coast oilfield regions of different geology &Gulf Coast oilfield regions of different geology & hydrogeology, and may not consider impactshydrogeology, and may not consider impacts fromfrom ““oilfield chemistryoilfield chemistry”” ““Oilfield chemistryOilfield chemistry”” & its potential component& its potential component impacts (esp. iron) have a history, & pits oftenimpacts (esp. iron) have a history, & pits often record itrecord it The detailed history of oilfield pitsThe detailed history of oilfield pits----how used, itshow used, its shallow fluid movement patterns, howshallow fluid movement patterns, how ““disturbeddisturbed”” over timeover time——is importantis important LA groundwater published arsenic record limited, but Miss. R. alluvium waters can be elevated (USGS 2000) Modern work, shallow groundwater As values from S. LA, 78 wells, up to 0.200 mg/l (Yang et al, 2014)
  • 6. 4 AnAn equilibriumequilibrium diagram fordiagram for system Assystem As--OO22--HH22OO Iron oxides common in our LAIron oxides common in our LA sedimentsediment As bound to iron oxides,As bound to iron oxides, released into GW withreleased into GW with ““reductive dissolutionreductive dissolution”” whenwhen some cause for a reducingsome cause for a reducing environment (organics, oil,environment (organics, oil, clayclay……)) Iron oxides reIron oxides re--precipitate asprecipitate as GW move into oxidizing zone,GW move into oxidizing zone, also locks up Asalso locks up As Does not address AsDoes not address As desorption (phosphates)desorption (phosphates) Model looks for relationsModel looks for relations between ORP, Fe, Asbetween ORP, Fe, As Amorphous Iron Precipitates in the OilfieldAmorphous Iron Precipitates in the Oilfield——longlong history in oilfield chemistryhistory in oilfield chemistry ((Hydrous ferric oxidesHydrous ferric oxides——HFOsHFOs)) 1950s Oklahoma Oilfield Water Treatment (Powell & Johnson, 1952)
  • 7. 5 PesticidesPesticides –– Concordia Parish cotton,Concordia Parish cotton, 1910+1910+ –– Vegetable gardens, treesVegetable gardens, trees –– Cattle dipping vatsCattle dipping vats HerbicidesHerbicides –– Inorganic & organicInorganic & organic –– Land & aquatic weed killerLand & aquatic weed killer Oilfield usageOilfield usage IndustrialIndustrial –– Corrosion inhibitorCorrosion inhibitor –– othersothers Griffin presentation on oilfield legacy litigation (2006) U. S. OilfieldsU. S. Oilfields –– Studies elsewhere fromStudies elsewhere from late 1950s (White) throughlate 1950s (White) through 20052005 –– As values range from NDAs values range from ND to 1.6 mg/lto 1.6 mg/l –– LA data from 1989 andLA data from 1989 and onward range from ND toonward range from ND to 0.5 mg/l0.5 mg/l –– 7 studies!7 studies! No produced waterNo produced water analysis (As) for myanalysis (As) for my exampleexample S. Louisiana & GOMS. Louisiana & GOM 1989 and later publications1989 and later publications
  • 8. 6 OilFieldOilField Arsenic Corrosion InhibitorsArsenic Corrosion Inhibitors Historic U. S. SummaryHistoric U. S. Summary Acid Corrosion InhibitorAcid Corrosion Inhibitor –– 19321932, Michigan oilfield acid, Michigan oilfield acid job, limestonejob, limestone –– 19341934, arsenic is important acid, arsenic is important acid job inhibitor, but organics nowjob inhibitor, but organics now availableavailable –– Early 1960sEarly 1960s, decrease As, decrease As usage, but good for highusage, but good for high--TT wellswells –– In 1970sIn 1970s, arsenic inhibitor, arsenic inhibitor phasephase--out in acid jobsout in acid jobs Production Corrosion InhibitorProduction Corrosion Inhibitor –– 19491949, Reported first usage in, Reported first usage in Texas Wilcox trend (Jones,Texas Wilcox trend (Jones, 1955)1955) –– 19541954, CA survey, 17 fields;, CA survey, 17 fields; 65 % pumping wells used65 % pumping wells used inorganic inhibitors (arsenicalinorganic inhibitors (arsenical compounds and chromates)compounds and chromates) (Hill & Davie, API, 1955)(Hill & Davie, API, 1955) –– 19571957, LA Stream Control, LA Stream Control Commission minutes reportCommission minutes report phasephase--out of oilfield arsenicout of oilfield arsenic corrosion pellets, strippercorrosion pellets, stripper fieldsfields –– 19601960, general end of U. S., general end of U. S. oilfield arsenic corrosionoilfield arsenic corrosion inhibitors (Gardner, 1960);inhibitors (Gardner, 1960); move to organicsmove to organics Iron & 1950s Arsenic Inhibitor in ProducedIron & 1950s Arsenic Inhibitor in Produced Water (Wilcox Trend, Texas)Water (Wilcox Trend, Texas) Jones (1955) (Jones, 1955)
  • 9. 7 1945 analysis, 141945 analysis, 14 ppmppm ((ClCl 13,82013,820 ppmppm)) 1959 analysis, 901959 analysis, 90 ppmppm ((ClCl 80,90880,908 ppmppm)) 1970 analysis, 2151970 analysis, 215 ppmppm ((ClCl 101,135101,135 ppmppm)) 1995 analysis, 21 mg/l (1995 analysis, 21 mg/l (ClCl 59,44959,449 ppmppm)) GENERAL OBSERVATION: While an old oilfield may have used arsenic inhibitors within the 1950s, more likely is that many oil fields had many possible decades (into 1970s, esp.) of elevated dissolved iron in produced water, and thus into pits (OOC, Poppadoc hearing files, 2009; Norman reliance documents, v. 52-53) Discovered in 1942, Tensas & ConcordiaDiscovered in 1942, Tensas & Concordia Parishes, LAParishes, LA Major producing field for The CaliforniaMajor producing field for The California Company (Standard Oil of CA)Company (Standard Oil of CA) Both unit (Cretaceous & some Tertiary age) &Both unit (Cretaceous & some Tertiary age) & lease productionlease production (Wilcox Fm mainly)(Wilcox Fm mainly) Outline of remaining presentationOutline of remaining presentation –– Public records supporting 1950s arsenic inhibitor usePublic records supporting 1950s arsenic inhibitor use –– Modern shallow groundwater geochemistry around leaseModern shallow groundwater geochemistry around lease emergency pit usage areasemergency pit usage areas
  • 10. 8 (Modified from Pisani report, 2008; OOC Poppadoc file # 006-007) Letters, OctLetters, Oct--Nov 1950, north side of field, testNov 1950, north side of field, test program for chemical inhibitors, liquid injectorsprogram for chemical inhibitors, liquid injectors and solid pelletsand solid pellets –– Oct 23:Oct 23: ““A most promising type of inhibitor is sodiumA most promising type of inhibitor is sodium arsenitearsenite, which we intend to make use of in the very, which we intend to make use of in the very near future.near future.”” –– Oct 27Oct 27:: ““have been advised of the promising results ofhave been advised of the promising results of sodiumsodium arsenitearsenite in corrosion mitigation workin corrosion mitigation work”” –– Nov 13Nov 13:: ““In view of the fact that it is intended to try outIn view of the fact that it is intended to try out sodiumsodium--arsenitearsenite pellets in the very near future, it is feltpellets in the very near future, it is felt desirable to postpone any trial of the downdesirable to postpone any trial of the down--hole injectorhole injector until results from that method of corrosion inhibition canuntil results from that method of corrosion inhibition can be obtained.be obtained.”” (OOC Poppadoc hearing, 2009; Miller/ICON reliance docs, v. 25, Exhibit P-1066)
  • 11. 9 (Poppadoc hearing, 2009; Miller/ICON reliance docs, v. 28; Tensas/Miller 02469-02470) WW--41, an arsenic corrosion inhibitor, is one41, an arsenic corrosion inhibitor, is one example of arsenic corrosion inhibitors usedexample of arsenic corrosion inhibitors used in some 1950s oilfields of the U.S.in some 1950s oilfields of the U.S. Its history is available in public documents.Its history is available in public documents.
  • 12. 10 The California Oil CoThe California Oil Co CaliforniaCalifornia ReseachReseach CorpCorp California SprayCalifornia Spray-- Chemical CorpChemical Corp California ResearchCalifornia Research CorpCorp (As & oilfield corrosion)(As & oilfield corrosion) –– Dec 1950, 2 patents,Dec 1950, 2 patents, RohrbackRohrback et al (1954)et al (1954) –– Mar 1951, 2 patents,Mar 1951, 2 patents, RohrbackRohrback et al (1953)et al (1953) –– Dec 1951, patent,Dec 1951, patent, RohrbackRohrback et al (1953)et al (1953) –– Oct 1954, patent,Oct 1954, patent, FrisiusFrisius (1959)(1959) California SprayCalifornia Spray-- Chemical CorpChemical Corp –– 1952, Patent application1952, Patent application granted in 1953 forgranted in 1953 for ““OrthoOrtho WW--41,41,”” also used isalso used is ““WW-- 41,41,”” for arsenic corrosionfor arsenic corrosion inhibitor (42 % sodiuminhibitor (42 % sodium arsenitearsenite) (EPA, 1973)) (EPA, 1973) (My Opinion from the public record: W-41 was used in the LSJ Field in the 1950s; organic inhibitors were used after that)
  • 13. 11 Mississippi RiverMississippi River Alluvium & AquiferAlluvium & Aquifer –– Braided streamBraided stream gravels at basegravels at base –– Mostly pointMostly point--bar sandsbar sands –– FiningFining--up into levee,up into levee, overbank, floodplainoverbank, floodplain sections (8sections (8--12 feet12 feet here)here) –– This nearThis near--surface unitsurface unit is aquifer confiningis aquifer confining layerlayer (Modified from Pisani report, 2008; OOC Poppadoc file # 006-007)
  • 14. 12 The data fromThe data from PisaniPisani & Associates, ICON (G.& Associates, ICON (G. Miller), is large and of highMiller), is large and of high--quality (quality (GeosyntecGeosyntec data is less but of highdata is less but of high--quality)quality) Shallow groundwater data are most reflective ofShallow groundwater data are most reflective of old impacts & possible controlling influences inold impacts & possible controlling influences in pit areaspit areas Groundwater wells at deeper depths (60Groundwater wells at deeper depths (60’’--8080’’, +, + below surface) do not have arsenic valuesbelow surface) do not have arsenic values above natural variability range; deeper alluviumabove natural variability range; deeper alluvium waters are a variation within the largerwaters are a variation within the larger sediment/water geochemical systemsediment/water geochemical system Regional Shallow Groundwater Movement,Regional Shallow Groundwater Movement, near the Mississippi Rivernear the Mississippi River (back & forth, net movement towards river(back & forth, net movement towards river----PisaniPisani)) (Pisani Report, 2008; OOC Poppadoc records, file # 006-007) RIVER LSJ LAKE
  • 15. 13 Pan Am Pit Area, ORP & GW ElevationPan Am Pit Area, ORP & GW Elevation (not being used enough!)(not being used enough!) Oilfield legacy records of LA Act 312, at OCC inOilfield legacy records of LA Act 312, at OCC in Baton Rouge, for background work away fromBaton Rouge, for background work away from pitspits Records of Parish dump closures and landfillRecords of Parish dump closures and landfill monitoring through the LA DEQ (EDMS system)monitoring through the LA DEQ (EDMS system) –– Tensas landfill, ~ 25 mi away, monitored by ICON forTensas landfill, ~ 25 mi away, monitored by ICON for Parish, 1994 to 2014 (EDMS # AI 43506)Parish, 1994 to 2014 (EDMS # AI 43506) –– Two shallow wells, 1997Two shallow wells, 1997--2008,2008, downgradientdowngradient fromfrom groundwater mound, As <0.02 to 0.162 mg/lgroundwater mound, As <0.02 to 0.162 mg/l
  • 16. 14 PisaniPisani & Associates (2012 report; OOC Tillman& Associates (2012 report; OOC Tillman records)records) interpreteinterprete the natural range from nonthe natural range from non-- detect (ND) up to 0.12 mg/ldetect (ND) up to 0.12 mg/l A study in shallowA study in shallow allluviumallluvium across the River inacross the River in Mississippi has an As range of ND to 0.10 mg/lMississippi has an As range of ND to 0.10 mg/l (Welsh et al, 2010; also phosphorous)(Welsh et al, 2010; also phosphorous) ICON data from Tensas Parish landfill, ND up toICON data from Tensas Parish landfill, ND up to 0.16 mg/l0.16 mg/l Given this & LA data to date, find shallowGiven this & LA data to date, find shallow groundwater measurements above 0.16 mg/l ingroundwater measurements above 0.16 mg/l in study area to consider possible anthropogenicstudy area to consider possible anthropogenic impactsimpacts
  • 17. 15 (oil wells in green, SWD wells in blue)(oil wells in green, SWD wells in blue) Wilcox pit PA pit
  • 18. 16 Applegate Pit (closed ~ 1984)Applegate Pit (closed ~ 1984) –– 7070’’ x 150x 150’’ x 8x 8’’ (include 2(include 2’’ levee)levee) –– UsageUsage ““only in emergencyonly in emergency”” Wilcox Pit (closed 1990)Wilcox Pit (closed 1990) –– 100100’’ x 100x 100’’ x 8x 8’’ (include 2(include 2’’ levee)levee) –– UsageUsage ““well backwashingwell backwashing”” (and emergency)(and emergency) Pan American Pit (closed ~ 1984)Pan American Pit (closed ~ 1984) –– 150150’’ x 200x 200’’ x 8x 8’’ (include 2(include 2’’ levee)levee) –– UsageUsage ““only in emergencyonly in emergency”” Arsenic in Pit Soils, Sediment, & WatersArsenic in Pit Soils, Sediment, & Waters 55 years after alleged As usage, the pit solids of today55 years after alleged As usage, the pit solids of today have arsenic ranges within Parish soil rangeshave arsenic ranges within Parish soil ranges –– Pits modified, rebuilt 2Pits modified, rebuilt 2--3 times during usage3 times during usage –– Pan Am & Applegate pit closure ~1984; both rePan Am & Applegate pit closure ~1984; both re--closedclosed (Applegate 2007; Pan Am 2010); Wilcox pit closed in 1990(Applegate 2007; Pan Am 2010); Wilcox pit closed in 1990 –– AsAs analysedanalysed inin ““soilssoils”” range from 1 to 10 mg/kgrange from 1 to 10 mg/kg A 1984 G & E study found elevated arsenic in ApplegateA 1984 G & E study found elevated arsenic in Applegate (0.04 mg/l) and Pan Am (0.05 mg/l) pit surface waters.(0.04 mg/l) and Pan Am (0.05 mg/l) pit surface waters. The 2 ft of bottom sludge ranged from 3 to 4.5 mg/kg AsThe 2 ft of bottom sludge ranged from 3 to 4.5 mg/kg As (OOC(OOC PoppadocPoppadoc hearing, ICON/Miller & Norman exhibits)hearing, ICON/Miller & Norman exhibits) GENERAL STATEMENT: Pit surface characteristics mayGENERAL STATEMENT: Pit surface characteristics may not be innot be in ““equilibriumequilibrium”” with older shallow surface leakagewith older shallow surface leakage characteristicscharacteristics
  • 19. 17 Applegate LeaseApplegate Lease –– PisaniPisani 2008 report2008 report –– (OOC file #006(OOC file #006--007)007) contours 250 mg/lcontours 250 mg/l chloride (yellow line)chloride (yellow line) –– I labeled dissolvedI labeled dissolved arsenic over 0.160 mg/larsenic over 0.160 mg/l –– Occurs In Wilcox SWDOccurs In Wilcox SWD & pit area& pit area (Fe not measured; ORP not flow(Fe not measured; ORP not flow--thru cell)thru cell) (OOC Poppadoc file #006-007, ICON 2006-07 data) Wells screened 8’ – 22’ Below surface Did not plot two points: Cl of 6,600 & 9,080 mg/l w/ As ND (<0.01 as “0”)
  • 20. 18 (also Fe, ORP w/ flow(also Fe, ORP w/ flow--thru cells)thru cells) OOC Poppadoc file # 006-007, Geosyntec Report, 2008 Applegate PitApplegate Pit –– GeosyntecGeosyntec GW data,GW data, 20082008 –– As relationships withAs relationships with ORP, FeORP, Fe –– Salinity and ORP?Salinity and ORP?
  • 21. 19 Applegate PitApplegate Pit –– AddAdd PisaniPisani data,data, 2012 (no ORP)2012 (no ORP) –– As vs. Fe trendsAs vs. Fe trends –– ClCl relation in MWrelation in MW--1 ?1 ? OOC, Tillman file #007-007, Pisani monitor reports
  • 22. 20 Pan Am Pit GWPan Am Pit GW –– Higher iron w/Higher iron w/ chlorides under pit;chlorides under pit; probable oilfield waterprobable oilfield water source impactsource impact –– Higher arsenic (overHigher arsenic (over 0.160 mg/l) w/0.160 mg/l) w/ chlorides under pit,chlorides under pit, probable oilfield waterprobable oilfield water source impactsource impact Pan Am Pit GWPan Am Pit GW –– As v. Fe relationshipAs v. Fe relationship varies in relation to pitvaries in relation to pit proximityproximity –– ORP v. FeORP v. Fe In GW away from pit,In GW away from pit, see relationship of ORPsee relationship of ORP & iron& iron In GW under pit,In GW under pit, reducing conditionsreducing conditions alone not correlatingalone not correlating with iron (or As)with iron (or As) amountsamounts
  • 23. 21 Observed ion mobility in GW from pit:Observed ion mobility in GW from pit: ClCl > Fe > As> Fe > As HFOsHFOs added to emergency pits from produced wateradded to emergency pits from produced water over decades; As limited, but strongly absorbed byover decades; As limited, but strongly absorbed by HFOsHFOs when presentwhen present In pit bottom, oily sludge and sometimes stagnantIn pit bottom, oily sludge and sometimes stagnant saltwater above this, reducing; GW below reducingsaltwater above this, reducing; GW below reducing Movement of reducing water withMovement of reducing water with ClCl, Fe (, Fe (++ As) where pitAs) where pit seepage, into sediment with Fe grain coatingsseepage, into sediment with Fe grain coatings GW away from pit more oxidizing, see Fe frontGW away from pit more oxidizing, see Fe front Added As stays within or close to pit boundaries; theAdded As stays within or close to pit boundaries; the movement ofmovement of addedadded iron further away from pit may beiron further away from pit may be affecting natural arsenic patterns previously only relatedaffecting natural arsenic patterns previously only related to iron oxide grain coatingsto iron oxide grain coatings
  • 24. 22 The geochemistry of pit impacts and signaturesThe geochemistry of pit impacts and signatures is greatly enhanced by historic knowledgeis greatly enhanced by historic knowledge Arsenic GW models for oilfield pits are useful,Arsenic GW models for oilfield pits are useful, but oilfield chemistry & past pit functions willbut oilfield chemistry & past pit functions will strongly modify generic modelsstrongly modify generic models IRON and possibly phosphorous are importantIRON and possibly phosphorous are important to further research (i.e., data,to further research (i.e., data, monitoring overmonitoring over time)time) for pit GW modelsfor pit GW models Past supplied produced watersPast supplied produced waters’’ dissolved iron todissolved iron to an oilfield pit may be impacting localized naturalan oilfield pit may be impacting localized natural dissolved arsenic variabilitydissolved arsenic variability Chlorides important marker for recognizingChlorides important marker for recognizing oilfield impact boundariesoilfield impact boundaries