a review of traffic light protocol for induced seismicity

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1 A Review of Traffic Light Protocol for Induced Seismicity and Its Effectiveness in Canada Honn Kao Geological Survey of Canada, NRCan Also at School of Earth and Ocean Sciences, University of Victoria 3 Geoscience BC 4 Western University

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Page 1: A Review of Traffic Light Protocol for Induced Seismicity

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AReviewofTrafficLightProtocolforInducedSeismicityandItsEffectivenessinCanada

Honn Kao

GeologicalSurveyofCanada,NRCanAlsoatSchoolofEarthandOceanSciences,UniversityofVictoria

3 GeoscienceBC4 WesternUniversity

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Outline

§ DefinitionofaTrafficLightProtocol(TLP)§ HistoricaldevelopmentoftheTLPforinducedseismicity(IS-TLP).§ IS-TLPinCanada.§ Casestudiesofred-lighteventsinBCandAB.§ Summaryandimplications.

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WhatisaTrafficLightProtocol?§ ATLPisasite-specific,real-time,riskmanagementsystem

withmultiplediscreteresponselevels.§ EachTLPlevelisdeterminedusingobservablecriteriaand

invokesspecificactionsdesignedtomitigatetheassociatedrisk.

§ MostIS-TLPsworkbyprovidingafeedbacksystemthatallowsforanoperationalresponsetothenearbyoccurrenceofseismiceventsexceedingaprescribedsetofcriteria.

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IS-TLPfromRegulator’sPerspective§ Identification,analysis,andtreatmentofseismicrisk

associatedwithinducedseismicity.§ IS-TLPisconsideredareactive riskmanagementtoolinthe

“treatment”catagory.§ Ingeneral,seismicdamagestartswhenpeakground

acceleration(PGA)exceeds5–10%ofEarth’sgravity(g).§ Ultimategoal:Toensureaquickandeffectivereductionin

boththenumberandsizeofinducedearthquakes.

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IS-TLPfromOperatorandServiceProvider’sPerspective§ CAPPPublication2012-0024“CAPPHydraulicFracturing

OperationPractice:Anomalousinducedseismicity:assessment,monitoring,mitigationandresponse”

§ IS-TLPispartofthe“monitoring,mitigationandresponse”category.

§ Fortheindustry,IS-TLPispartofthedecision-makingprocess.Thus,itmustbeeasytounderstand,communicate,develop,andimplement.

§ Ultimately,theeconomicrealityisthebottomline.

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TheFirstIS-TLP§ Proposedfortheoperationsofhydraulicstimulationsof

enhancedgeothermalsystemsineasternElSalvador,CentralAmerica(Bommer etal.2006).

§ Basedonpeakgroundvelocity(PGV).§ Green:Groundmotionbelowthethresholdofgeneral

detectability,ortheoccurrencerateofseismicitylowerthanthealreadyestablishedbackgroundlevel.

§ Amber:Groundmotioncanbefelt,butdamageisunlikely.§ Red:Damagetobuildingsisexpectedtosetin.

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IS-TLPinEurope§ EnhancedGeothermalSystem,Basel,Switzerland(Haringetal.,2008).

§ Green:PGV<0.5mm/s,ML <2.3,nofeltreport(Proceedasplanned)§ Yellow:PGV≤2.0mm/s,ML ≥2.3,fewfeltreport(Informregulators,stop

increasingrate)§ Amber:PGV≤5.0mm/s,ML ≤2.9,manyfeltreports(Reducepumpingrate)§ Red:PGV>5.0mm/s,ML >2.9,generallyfelt(Stoppumping,bleedwells)

§ HydraulicFracturingofShaleGas,UK(https://www.gov.uk)§ Green:ML ≤0.0(Proceedasplanned)§ Amber:ML between0and0.5(Proceedwithcaution,lowerrates,

intensifymonitoring)§ Red:ML >0.5(Suspendinjectionimmediately)

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IS-TLPinUSA§ CO(Wongetal.,2015)

§ Yellow:Feltatthesurface(Modifyoperations)§ Red:ML ≥4.5(Suspendoperations)

§ OK(Stoplight System,http://earthquakes.ok.gov)§ Escalatingreviewofoperator’smitigationproceduresasML ≥2.5,≥3.0.

SuspendoperationswhenML ≥3.5.§ OH(Brudzinski etal.,2017;Dade,2017)

§ ML <1.5(Proceedasplanned)§ ML ≥1.5(Informregulator)§ ML between2.0and2.4(Modifyoperations)§ ML ≥2.5(Temporaryhaltcompletionsonlateral)§ ML ≥3.0(Suspendoperation)

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IS-TLPinAB,Canada§ SubsurfaceOrder#2,issuedonFebruary19,2015.

§ ApplicabletotheDuvernay ZonewithintheFoxCreekarea.§ Green:ML <2.0(Proceedasplanned)§ Yellow:ML between2and4within5kmofaninjectionwell

(ImmediatelyreporttoAER,implementmitigatingplan)§ Red:ML ≥4within5kmofaninjectionwell(ImmediatelyreporttoAER

andceasehydraulicfracturingoperations)

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IS-TLPinBC,Canada§ Section21.1oftheDrillingandProductionRegulation(since

June2015,presentedassite-specificpermitconditionsinceOctober2012).§ Astoplightsystem,noescalatinglevels.§ ApplicabletoallinjectionoperationsinBC.§ Red:ML ≥4within3kmofthedrillingpad,oragroundmotionfeltonthesurfacebyanyindividualwithinthe3kmradius(Suspendoperations).

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MajorDeficienciesofMagnitude-basedIS-TLP§ Possibleconfusionduetomagnitudeuncertainty.

§ Differentscalesand/ormethodology(ML,Mw,Mn,etc.)§ Differentchoice/availabilityofdata(localarrayvs.regionalnetworks)§ Differentsourcecharacteristics(momentscaling,stressdrop,focal

mechanism)§ Differentattenuation/distancecorrections§ Differentsiteeffects

§ Notlinkedtotheimpact/consequencesofreportedevents.§ Completelyignoreotherpotentialusefulindicators(e.g.,changeof

earthquakeoccurrencerate,migrationofhypocenters,correlationwithgeologicalstructures).

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DesignatedGroundMotionMonitoringAreasinBC§ Newpermitconditionforwellsintwodesignatedareas.§ Requirepresenceofadequatemonitoringofgroundmotionduring

hydraulicfracturing.§ Minimumof1groundmotionmonitorwithin3kmofthe

commondrillingpad.§ Instrumentwithadynamicrangeof+/-2gandaminimum

detectabilityof0.02g.§ Submitgroundmotionmonitoringreportwithin30daysof

completion.§ Seismicdataforanygroundmotionsexceeding0.02gmustbe

submitted.

(BCOGCIndustryBulletin2016-19)

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DistributionofRegionalSeismicityinnortheastBCandwestAB

• 4919eventsintotal.• 3030(~62%)occurredinthedesignated

monitoringareas.• Green:~81.5%,Yellow:~18.3%,Red:<0.2%

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Red-Light EventsinBCandAB§ 1.August4,2014,Mw 4.5(ML 4.1)

§ 2.January23,2015,Mw 4.4(ML 4.1)*Mw 3.6(Schultzetal.,2017).

§ 3.June13,2015,Mw 4.6(ML 4.3)*Mw 3.9(Wangetal.,2016),ML 4.4(AGS).

§ 4.August17,2015,Mw 4.6(ML 4.9)

§ 5.January12,2016,Mw 4.4(ML 4.6)*Mw 4.1(Schultzetal.,2017),ML 4.8(AGS).

§ 6.July12,2016,Mw 3.9(ML 4.0)

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15Event1,Mw 4.5(ML 4.1)

August4,2014northernMontney,BC

§ ActiveHFandWDduring7/25– 8/07.§ Oneyellow-light (Mw 3.8)event

occurredon7/30.§ Thered-lighteventoccurredwith

reducedinjectionrateandpressure.§ Prior,during,andpost-injection

earthquakeratesare0,0.14,and0eventperday,respectively.

§ NomoreM4+eventafterwards.

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16Event2,Mw 4.4(ML 4.1)

January23,2015FoxCreek,AB

§ ActiveHFduring12/17– 1/10.§ 1green- and3yellow-lightevents

duringthelast5daysofinjection.§ Seismicitycontinuedafterthe

completionofHFfor2moreweeks.§ Prior,during,andpost-injection

earthquakeratesare<0.01,0.32,and0.21 eventsperday,respectively.

§ AnotherM4+eventaboutayearlater.

§ Aclearcaseof”delayed”triggering.

(Schultzetal.,2017;Wangetal.,2016)

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17Event3,Mw 4.6(ML 4.3)

June13,2015FoxCreek,AB

§ ActiveHFduring5/22– 6/07at6nearbywells.

§ Amongthehighestdailyinjectionvolume.

§ Oneyellow-lighteventoccurredon5/27.

§ Prior,during,andpost-injectionearthquakeratesare0,0.18,and0.01 eventperday,respectively.

§ NomoreM4+eventafterwards.§ Anotherexampleof“delayed”

triggering.

(Schultzetal.,2017)

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18Event4,Event4,Mw 4.6(ML 4.9)

August17,2015northernMontney,BC

§ ActiveHFandWDduring8/11–8/28.

§ Onegreen butNO yellow-lighteventoccurredsincetheinjectionbeganbeforetheMw 4.6event.

§ Seismicitycontinuedfor~oneweek.

§ Prior,during,andpost-injectionearthquakeratesare0.03,0.59,and0.19 eventsperday,respectively.

§ NomoreM4+eventafterwards.

(Babaie Mahani etal.,2017a,2017b)

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19Event5,Mw 4.4(ML 4.6)

January12,2016FoxCreek,AB

§ SamegeneralareaoftheJanuary23,2015,Mw 4.4,red-lightevent.

§ ActiveHFstartedon1/04,stoppedrightafterthered-lightevent,neverresumed.

§ Twoyellow-lighteventsoccurredon1/09and1/10.

§ Prior,during,andpost-injectionearthquakeratesare0.08,1.11,and0.21 eventsperday,respectively.

§ NomoreM4+eventafterwards.ButscatteredM<4seismicitycontinuedtilltheendofourstudyperiod.

(Schultzetal.,2017;Wangetal.,2017)

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20Event6,Mw 3.9(ML 4.0)

July12,2016northernMontney,BC

§ InitiallyreportedML =4.0,laterrevisedtoMw =3.9

§ ActiveHFstartedon7/08.§ Noeventoccurredbeforethis

red-lightevent.§ Prior,during,andpost

earthquakeratesare<0.001,0.6,and0.23 eventsperday,respectively.

§ NomoreM4+eventafterwards.

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KeyObservationsAboutRed-LightEventsinBCandABKeyFeatures Event1

(BC)Event2(AB)

Event3(AB)

Event4(BC)

Event5(AB)

Event6(BC)

Totalnumberofeventsduringinjectionstage 2 12 4 10 10 3

Precursoryseismicityduringinjectionstage YLE YLE+GLE YLE+GLE GLE YLE+GLE None

Rateofseismicitybeforethestartofinjection 0.00 <0.01 0.00 0.03 0.08 <0.01

Rateofseismicityduringtheinjection 0.14 0.32 0.18 0.59 1.11 0.60

Rateofseismicityaftertheinjection 0.00 0.21 0.01 0.19 0.21 0.23

Seismicityrespondingtoinjectionadjustment Yes N/A N/A Yes Yes Yes

Followedbyalargereventcausingdamage No No No No No No

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SummaryandImplications§ AnIS-TLPbasedonescalatingmagnitude(green –>yellow –>red)ismoreapplicabletoAB

thanBC.

§ Backgroundseismicitymaybeausefulreferenceinforecastingtheoverallseismicresponsetoinjections.§ Lowpre-injectionseismicityrate~Lowseismicityrateduringinjection

§ Aclearjumpintheseismicityratefromthepre-injectionperiodtotheinjectionperiod,especiallyafter2015.

§ Thephenomenonof“delayedtriggering”(twored-lighteventsinAB)canbeaproblemfortheeffectivenessoftheIS-TLPandshouldbecarefullyconsidered

§ ExistingIS-TLPforinducedseismicityinbothBCandABappeartobeworkinginthesensethatitpreventsanydamagingearthquakes(M>5.5)fromhappening.

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QuestionsorComments?§ Sendyourquestionsorcommentsto

Dr.Honn KaoProjectLeader,InducedSeismicityResearchGeologicalSurveyofCanada(250)[email protected]