Technical Assessment for Authorization to Discharge Waste Report

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TECHNICAL ASSESSMENT FOR AUTHORIZATION TO DISCHARGE WASTE Submitted To: BC MINISTRY OF ENVIRONMENT ENVIRONMENTAL MANAGEMENT BRANCH Prepared For: SOUTH ISLAND AGGREGATES LTD. Prepared By: Reviewed By: Matt Pye, P.Eng. David Kneale, P.Geo. Principal, Hydrogeologist Principal, Hydrogeologist Reviewed By: Reviewed By: Jeff Taylor, P.Eng. David Mitchell, P.Eng., CSAP Principal, Senior Engineer Principal, Senior Engineer Project Number: 320 August 2012

Transcript of Technical Assessment for Authorization to Discharge Waste Report

  • TECHNICALASSESSMENTFOR

    AUTHORIZATIONTODISCHARGEWASTE

    SubmittedTo:

    BCMINISTRYOFENVIRONMENTENVIRONMENTALMANAGEMENTBRANCH

    PreparedFor:

    SOUTHISLANDAGGREGATESLTD.PreparedBy: ReviewedBy: MattPye,P.Eng. DavidKneale,P.Geo.Principal,Hydrogeologist Principal,Hydrogeologist

    ReviewedBy: ReviewedBy: JeffTaylor,P.Eng. DavidMitchell,P.Eng.,CSAPPrincipal,SeniorEngineer Principal,SeniorEngineer

    ProjectNumber:320August2012

  • SouthIslandAggregatesLtd. August2012ApplicationforAuthorizationtoDischargeWasteTechnicalAssessment AEFile#320

    TABLEOFCONTENTS

    1.0 Introduction............................................................................................................1

    1.1 Objectives............................................................................................................11.2 ScopeofWork.....................................................................................................21.3 OverviewofProposedFacility............................................................................31.4 BenefitsofProposedFacility..............................................................................5

    2.0 SiteDescription.......................................................................................................7

    2.1 LocationandTopography...................................................................................72.2 Legal....................................................................................................................72.3 Geology...............................................................................................................82.4 Hydrogeology......................................................................................................92.5 Climate................................................................................................................92.6 SurroundingLandUse.......................................................................................112.7 DistancestoNearestSchools,HospitalsandCareFacilities.............................13

    3.0 ReceivingEnvironment.........................................................................................15

    3.1 SoilConditions..................................................................................................153.2 Hydrogeology....................................................................................................163.3 NearbyDrinkingWater,Irrigation,andLivestockWells...................................213.4 ApplicableCSRSiteSpecificFactors.................................................................243.5 HydrologyofWaterDischargeLocation...........................................................253.6 EnvironmentalMonitoringPlan........................................................................273.7 CumulativeEffectsfromOtherDischargesintheArea....................................29

    4.0 SourceMaterial.....................................................................................................30

    4.1 ContaminantsofConcern.................................................................................304.2 MaximumConcentrations................................................................................314.3 ConfirmationSoilisNotHazardousWaste.......................................................344.4 QA/QCofIncomingSoilQuality........................................................................364.5 HoldingCellforSuspect/RejectSoil..................................................................384.6 SoilAcceptancePlan.........................................................................................38

    5.0 SoilDischarge........................................................................................................40

    5.1 VolumeofSoilPerYearDischarged..................................................................405.2 Concentrations/LevelatDischarge.................................................................415.3 ConcentrationConfirmation.............................................................................42

  • SouthIslandAggregatesLtd. August2012ApplicationforAuthorizationtoDischargeWasteTechnicalAssessment AEFile#3205.4 SoilDischargeLocation.....................................................................................435.5 PermanentSoilContainmentCellDesign.........................................................445.5.1 BaseLinerSystem.........................................................................................445.5.2 ContainmentCells.........................................................................................485.5.3 FinalCap........................................................................................................485.5.4 LeakDetectionandLeachateCollection.......................................................49

    6.0 WaterDischarge...................................................................................................51

    6.1 RunoffandLeachateControlMeasures...........................................................516.2 DischargeLocation............................................................................................536.3 WaterQualityatThePointofDischarge..........................................................556.4 ContaminantsofConcerninEffluent...............................................................576.5 StormEventFlows............................................................................................586.6 TreatmentSystemComponents.......................................................................596.7 MaximumDischargeRateandDischargePeriod..............................................626.8 DischargeMonitoringPlan...............................................................................626.8.1 EffluentTreatmentandDischargeMonitoring.............................................636.8.2 ReceivingWaterMonitoring.........................................................................65

    6.9 BedrockLeachability.........................................................................................676.10 EffluentPermitFees..........................................................................................68

    7.0 OtherDischarges/Nuisances:................................................................................70

    7.1 FugitiveDust.....................................................................................................707.2 Odours...............................................................................................................717.2.1 SoiltoAirPartitioning...................................................................................727.2.2 VapourModelling.........................................................................................767.2.3 VapourMonitoring.......................................................................................767.2.4 EncapsulationAreaVapourMonitoring.......................................................797.2.5 VapourMitigationMeasures........................................................................80

    7.3 Noise.................................................................................................................81

    8.0 Construction/SiteSpecifics.................................................................................82

    8.1 BiocellSizes.......................................................................................................828.2 SoilTreatmentAreaLinerandDrainage...........................................................828.3 LeachateDetection...........................................................................................858.4 StormwaterRunoff...........................................................................................868.4.1 OnsiteCollectionandConveyanceSystem.................................................878.4.2 FloodProtection...........................................................................................888.4.3 StormwaterTreatment.................................................................................888.4.4 EnvironmentalConsiderations......................................................................908.4.5 DesignFlowsandStorage.............................................................................90

  • SouthIslandAggregatesLtd. August2012ApplicationforAuthorizationtoDischargeWasteTechnicalAssessment AEFile#3208.5 Hydrology,LocationsofFloodPlains................................................................928.6 FirstNationsInterests.......................................................................................928.7 Covenants.........................................................................................................93

    9.0 Operations............................................................................................................95

    9.1 SoilTreatment...................................................................................................959.2 WeatherProtection..........................................................................................979.3 SitePlan/FacilityLayout..................................................................................989.4 OnSiteStaff......................................................................................................999.5 ConfirmationofSoilQuantities......................................................................1009.6 SoilTracking....................................................................................................1009.7 SoilTreatmentTrackingSystem.....................................................................1019.8 InterimTreatmentAssessment......................................................................1029.9 SampleMethods.............................................................................................1039.10 AnalyticalMethods.........................................................................................1039.11 SoilPlacementWithinPermanentEncapsulationArea..................................1049.12 FacilityInspections..........................................................................................1049.13 ReportingtoMOE...........................................................................................104

    10.0 SoilAcceptancePlan...........................................................................................105

    10.1 WasteApprovalApplication...........................................................................10510.2 SoilReceivingandVerification........................................................................10610.3 ShipmentandTracking...................................................................................10710.4 QA/QCforIncomingSoils...............................................................................10810.5 ProceduresforRemovalofUnacceptableSoils..............................................110

    11.0 ConsultationPlan................................................................................................111

    12.0 ClosurePlan........................................................................................................112

    12.1 FinalCapDesign..............................................................................................11312.2 ClosureMonitoringPlan.................................................................................11612.3 Discussion........................................................................................................117

    13.0 EmergencyResponsePlan..................................................................................119

    14.0 FinancialSecurity................................................................................................120

    15.0 Limitations...........................................................................................................122

  • SouthIslandAggregatesLtd. August2012ApplicationforAuthorizationtoDischargeWasteTechnicalAssessment AEFile#320ATTACHMENTSFIGURESFigure1 SiteLocationPlan&DrawingIndexFigure2 SurroundingLandUsePlanFigure3 Watershed&TopographyPlanFigure4 Site&SurroundingSurfaceWaterFigure4B GroundwaterFlowDirectionFigure5 RegionalCrossSectionA(NS)Figure6 DetailedCrossSectionB(NS)Figure7 DetailedCrossSectionC(EW)Figure8 SitePlanShowingProposedFacilityFigure8B StormwaterFacilityDetailsFigure8C SurfaceofClayTillBaseofEncapsulationAreaFigure9 SoilManagement/TreatmentAreaTypicalCrossSectionFigure9B WaterTreatmentSystemFigure10 SoilContainmentAreaTypicalCrossSectionFigure10B ContainmentCellTypicalCrossSectionFigure11 FirstLiftQuarryPhasingPlanFigure12 SecondLiftQuarryPhasingPlanFigure13 QuarryPhasingSectionsFigure14 QuarryPhasingSectionsFigure15 ClosurePlanFigureFigure16 CovenantLocationPlanTABLESTable1 AnalyticalResultsinGroundwaterAnions,Nutrients,MicrobiologyTable2 AnalyticalResultsinGroundwaterTotalandDissolvedMetalsTable3 AnalyticalResultsinGroundwaterVolatileOrganicCompoundsTable4 AnalyticalResultsinGroundwaterPolycyclicAromaticHydrocarbonsTable5 AnalyticalResultsinSurfaceWaterAnions,Nutrients,MicrobiologyTable6 AnalyticalResultsinSurfaceWaterTotalandDissolvedMetalsTable7 AnalyticalResultsinSurfaceWaterVolatileOrganicCompoundsTable8 AnalyticalResultsinSurfaceWaterPolycyclicAromaticHydrocarbons

  • SouthIslandAggregatesLtd. August2012ApplicationforAuthorizationtoDischargeWasteTechnicalAssessment AEFile#320APPENDICESAppendixA MinePermitQ8094AppendixB LandTitleAppendixC PhotographsAppendixD WellLogsExistingWaterSupplyWellsandMonitoringWellsAppendixE MonitoringWellResponseTestsAppendixF LaboratoryAnalyticalReportsAppendixG MinistryofEnvironmentGuidanceDocument#1AppendixH FieldProtocolsAppendixI IDFCurveAppendixJ WasteApprovalApplicationFormAppendixK RestrictiveCovenantforShawniganCreekAppendixL CascadiaBiologicalServicesReportAppendixM EmergencyResponsePlanAppendixN ConsultationReport

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    EXECUTIVESUMMARY

    ActiveEarthEngineeringLtd.(ActiveEarth)wasretainedbySouthIslandAggregatesLtd.

    (SIA)toundertakeaTechnicalAssessmentaspartofanapplicationtotheBCMinistryof

    Environment (MOE) for anAuthorization toDischargeWaste. The application ismade

    undertheBCEnvironmentalManagementAct(EMA). The intentoftheapplication isto

    obtain approval for the development of a facility that is capable of accepting

    contaminated soils. There is currently no local facility that services the southern

    VancouverIslandRegion.

    Thesubjectproperty(theSite) is locatedat640StebbingsRoad,theSouthShawnigan

    Lake Area (Electoral Area B)within the Cowichan Valley Regional District. The Site is

    approximately5.0 km southof Shawnigan Lake,3.3 kmwestof FinlaysonArm,1.5 km

    northofDevereauxLakeand5.5kmeastofSookeLake(Figures1and3).Siteislocatedin

    the upper reaches of the south Shawnigan Lake catchment. The area is underlain by

    shallowbedrockasexpressedthroughsteepslopesandsignificantrisesinelevation.The

    Site comprises a local peak elevation of approximately 340mgeod., and the ground

    surfacegenerallyrisestothesouthreachingpeakelevationsof640mgeod.

    TheSiteiscurrentlyoperatedasarockquarryunderthejurisdictionoftheBCMinistryof

    MinespermitnumberQ8094(includedasAppendixA).Anapplicationisbeingmadeto

    modifythereclamationplanintheminingpermitconcurrentlywithanapplicationforan

    AuthorizationtoDischargeWaste. Theproposedchanges/authorizationwouldallowfor

    contaminatedsoiltobetreatedandpermanentlyencapsulatedontheSiteaspartofthe

    minereclamationplan.

    Thereare significantbenefits todevelopinga soil treatmentanddisposal facility in the

    Southern Vancouver Island area, with implications to local economic, social and

    environmental conditions. There is an immediateneed for such a facility toprovide a

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    localandcosteffectivesolutionfortheremediationofmanyexistingcontaminatedsites

    intheregion, includingunderutilizedbrownfieldsites. Theproposed facilityprovidesa

    locallyresponsiblesolutiontoexistingissuesintheregion.

    ThisTechnicalAssessmentReport(TAR)characterizesthegeologicalandhydrogeological

    conditionsoftheSite,andprovidesadetaileddescriptionoftheproposedsoiltreatment

    anddisposal facility. Theproposed facilitywouldonlyaccept contaminated soil that is

    nonleachable and at levels below Hazardous Waste. Soils impacted with organic

    substancessuitableforbioremediationwouldbetreatedatthefacility,andsoilsimpacted

    with inorganic substances would be permanently encapsulated to immobilize the

    contaminants.Nodisposalofliquidsorsludgeswillbepermitted.

    The hydrogeological conditions at the Site have been evaluated through review of

    backgroundsourcesofinformationandobtaininginformationthroughdrillingandtesting

    the rockonSite (Figures3,5,6and7). Thereappears tobeastratificationof fracture

    density/permeabilitybeneaththeSite.Itmaybepossibletogeneralizethebedrockinto2

    distinctlayersasfollows:

    UpperBedrockfrom0to75m(0to250ft):Negligiblegroundwaterflow.

    DeepBedrockbelow75m(250ft):Minorgroundwaterflow.

    Theverylowpermeabilityoftheupperbedrock(K=7.6x1010m/s)providesahighlevel

    ofprotectiontothegroundwaterflowwithinthedeepbedrock(K=1.6x107m/s).

    SurfacewaterbodiesinthevicinityoftheproposedfacilityincludeShawniganCreekand

    itstributaries. ShawniganCreek flowsthroughthe legalparceltotheeastoftheactive

    mineandproposedfacility.Allsurfacewater,shallowseepageandpotentialleachatewill

    bemanagedwithinthefootprintoftheexistingmineanddischargedtogroundalongthe

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    western property line (Figure 8). Background creekwater quality samples have been

    takenforestablishingbaselineconditions.

    The proposed facilitywould include paved areas formanaging and treating soils,with

    surface water and leachate controls including berms, trenches, catchbasins, holding

    ponds,treatmentsystemsandmonitoringlocations.Theconceptualdesignofthefacility

    includesredundancyinwatertreatmentcapabilitiesandwatermonitoringlocationsprior

    todischargetoground(Figures8,9and10). Facilitydesignandoperationwouldaimto

    minimizetheproductionof leachatewithintermediatecoversfromsoilwithintheactive

    managementandtreatmentareasaswellassoilplacedinpermanentencapsulationcells.

    Anyleachategeneratedwouldbecollectedandtreatedpriortodischarge.

    The facility would be operated under the direction of a qualified Environmental

    Engineering Consultant. The Consultants rolewould include general oversight of the

    facility operations, and would ensure soil quality criteria are met through adequate

    characterization prior to soils being transported to the facility. The Consultantwould

    direct the soil treatmentprocedures, reviewwaterqualitymonitoringdataandprovide

    detaileddesignforpermanentencapsulationcells.

    Theproposedfacilitycouldoperateforgreaterthan50years,therefore,thenextlanduse

    followingclosureisdifficulttopredict.However,theclosureplanincludestheplacement

    ofa2mthicksoilcapovertheentirefootprint,withthelower1mofthecapcomprised

    of lowpermeability soil to limit the infiltrationofprecipitation. Thecapwouldalsobe

    crownedtopromotedrainageawayfromthecentreoftheSite,similartothepremining

    conditions. Monitoringofthegroundwater,soilvapourandsurfacewaterqualitywould

    beconductedforaminimumof20yearsfollowingclosureofthefacility(Figure15).

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    In summary, the location and physical conditions at the Site are well suited for the

    proposedfacility.TheSiteislocatedincloseproximitytomanycontaminatedproperties

    andwouldserviceexistingandfuturedemands.Thegroundwaterresourcesarelimitedat

    theSite,andwellprotectedfromtheproposedfacilitywithalargedepthtogroundwater

    andasignificantthicknessofvery lowpermeabilitybedrockatgroundsurfacetoprotect

    the underlying bedrock aquifer. Nearby surface water resources would require

    appropriatefacilitydesign,operationandmonitoringtoensurenoimpactsoccur.Overall,

    the environmental risk posed by the proposed facility, as described in this report, is

    consideredtobelow.

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    1.0 Introduction

    ActiveEarthEngineeringLtd.(ActiveEarth)wasretainedbySouthIslandAggregatesLtd.

    (SIA)toundertakeaTechnicalAssessmentaspartofanapplicationtotheBCMinistryof

    Environment (MOE) for anAuthorization toDischargeWaste. The application ismade

    pursuanttoSection14oftheBCEnvironmentalManagementAct(EMA).

    Thesubjectproperty(theSite)islocatedat640StebbingsRoad,intheSouthShawnigan

    LakeArea(ElectoralAreaB)withintheCowichanValleyRegionalDistrict(Figure1).

    TheSiteiscurrentlyoperatedasarockquarryunderthejurisdictionoftheBCMinistryof

    MinespermitnumberQ8094(includedasAppendixA).Anapplicationisbeingmadeto

    modifytheminereclamationplan intheminingpermitconcurrentlywithanapplication

    for an Authorization to DischargeWaste. The proposed changes/authorizationwould

    allow forcontaminatedsoil tobe treatedandpermanentlyencapsulatedon theSiteas

    partoftheminereclamationplan.

    TheobjectivesofthisTechnicalAssessmentReport(TAR)istocharacterizethegeological

    and hydrogeological conditions of the Site, as this is fundamental to assessing the

    potential for environmental impacts as a result of the requested authorization. In

    additiontodeterminingtheSiteconditions,theTARalsodescribesindetailtheoperations

    anddesignoftheproposedsoiltreatmentanddisposalfacility.

    1.1 Objectives

    TheprimaryobjectivesofthisTechnicalAssessmentaresummarizedasfollows:

    Provide a description of the Site and surrounding areawith respect to surface

    water,groundwater,landuses,climateandlegal/municipalboundaries;

    DeterminethegeologicalandhydrogeologicalconditionsattheSite;

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    ProvideabaselineforgroundwaterandsurfacewaterqualityattheSite;

    Assess the potential for physical environmental impacts including groundwater,

    surfacewater,soil,soilvapourandairqualityasaresultoftheproposedfacility;

    Describe the proposed contaminated soil treatment and disposal facility

    operationsincluding:

    o Soilqualitytobeacceptedandsourcesofcontaminatedsoil;o Soilquantitythatmaybetreatedandpermanentlyencapsulated;o Soilmanagement includingmovement, sampling, temporary storage and

    permanentencapsulation;

    o Surface water management including protection, diversion, collection,sampling,treatmentandmonitoring;

    o Groundwatermonitoring;o Soiltreatmentproceduresandbiocelldesign;o Soildisposalproceduresandpermanentcelldesign;ando Postoperationincludingclosureplanandemergencyresponseplan.

    In addition to the abovestated primary objectives, the TAR includes supporting and

    additionalinformationrelatedtotheoperationandmanagementoftheproposedfacility

    fromdesignthroughclosure.

    1.2 ScopeofWork

    Thefollowingscopeofworkwasperformedtoaddresstheabovestatedobjectives:

    Review of MOE documents pertaining to applications for Authorization to

    DischargeWasteundertheEnvironmentalManagementAct(EMA);

    MeetingwithBCMinistryofMinesandtheMOEpersonneltodiscusstheprocess

    formakinganapplicationforanAuthorizationtoDischargeWasteattheSite;

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    Undertaking a desk study to compile and review all available background

    information for the Site including legal, climate, topography, geology,

    hydrogeology, drainage, surface waters, surrounding land uses, and existing

    miningpermits;

    Drilling,monitoringwellinstallation,piezometricheadmeasurementandhydraulic

    conductivitytestingofthebedrockaquifer;

    Groundwaterand surfacewater sampling toestablishbaseline conditionsat the

    Site;

    Developingfacilitydesigndetails;

    Developingfacilityoperationaldetails;

    Developingafacilitymonitoringplan;

    Developingafacilityclosureplan;

    DevelopingafacilityEmergencyResponsePlan;and

    PreparingthisTechnicalAssessmentReportfortheSite.

    1.3 OverviewofProposedFacility

    TheWaste Discharge Application is beingmade for authorization to develop a facility

    capableof treating andpermanently immobilizing contaminated soilsoriginating in the

    SouthernVancouver Islandarea. Wastematerialsfrom industrialprocessesmayalsobe

    acceptedattheproposedfacilityifshowntobenonleachable.

    The proposed facility would accept contaminated soils that exceed residential,

    commercial and industrial landuse standards asdefinedby theBCContaminated Sites

    Regulation(CSR).However,theproposedfacilitywouldnotacceptsoilsthatareleachable

    orexceedtheBCHazardousWasteRegulation(HWR)standards.

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    Organic/treatable contaminantswouldbe treated/bioremediatedprior toencapsulating

    onSite,orshippedoffSiteforreuseifappropriate.Inorganic/untreatablecontaminants

    wouldbepermanentlyencapsulatedwithinengineeredcontainmentcells.

    The facilitywouldhavea soilmanagementarea comprisedofanasphaltpaved surface

    withwatercontrol/collection/treatment infrastructure. Thisareawouldalsobeusedfor

    soil treatment, likelywith semipermanent covered sections for soilsmore sensitive to

    moisture. The inorganic/untreatable soils and some posttreatment soils would be

    permanentlyencapsulatedwithintheengineeredcontainmentcellswithinthefacility.

    The facility is envisioned to contain soil management, soil treatment and soil

    encapsulation areas at all times during operation. The proposed encapsulation of

    contaminatedsoilswillrequireanamendmenttothereclamationplanasindicatedinthe

    existingminingpermit(Q8094)fortherockquarry.Contaminatedsoilsareproposedto

    be acceptable for backfill of themine pit, and the reclamation activities would be

    undertakenconcurrentwiththeminingactivities. Asaresult,thesoilmanagementand

    treatmentoperationsmayneed tobemovedas theminingprogressesat theSite. The

    mine has an anticipated lifespan of approximately 5060 years, therefore, the facility

    operationswillnotrequireregularmovement.

    Anappropriategroundwaterand surfacewatermonitoringprogramwouldbe followed

    and reporteduponbyaqualifiedprofessional. Surfacewaterandshallowgroundwater

    seepage (if present)would bemanaged through diversion, collection,monitoring and

    treatmentasnecessarypriortodischarge.

    Fugitive dust, noise and odourswill bemonitored and addressed as necessary during

    facilityoperation.

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    1.4 BenefitsofProposedFacility

    ThebenefitsofdevelopingasoiltreatmentanddisposalfacilityintheSouthernVancouver

    Islandareaarefarreaching,withimplicationstolocaleconomic,socialandenvironmental

    conditions. There isan immediateneed for sucha facility toprovidea localand cost

    effectivesolutionfortheremediationofmanyexistingcontaminatedsitesintheregion.

    This application rises, in part, from the need for a local solution to facilitate the

    remediationofcontaminatedsites.Currently,therearemanycontaminatedsitesthatare

    vacant, derelict and/or underutilized because of contamination (ie: Brownfield Sites).

    Thecostassociatedwiththeremediationofmanyofthesesitesisprohibitivebecauseof

    thelackofalocalcontaminatedsoildisposalfacility.Oftenthecosttodisposeofthesoil

    toanapprovedfacility isprohibitivebecauseofsoiltransportationcosts. This isa long

    standing obstacle that has been overcome in many cases by the use of onsite risk

    managementofcontaminatedsoil. While thiscanbeanacceptablesolution,often it is

    preferential(fromanenvironmentalanddevelopmentperspective)todisposeofthesoil

    offsite.

    Theproposedfacilitywouldenabledevelopmentofmanybrownfieldsites,inadditionto

    otherenvironmental,economicandsocialbenefitssuchas:

    Enabling cleanupofmore local contaminated sites via full contaminant removal

    versusleavingcontaminationinplacewithriskmanagement;

    Enablingalocalsolutiontolocalproblems;

    Reducedgreenhousegasgenerationby significantly reduced truck travel (50km

    roundtripvs.500kmroundtripfromVictoriatocurrentmidIsland locationsfor

    example);

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    Reducedwearand tearon thehighway systemdue to lower truck travel,along

    withbettersocialoutcome(e.g.fewertrafficfatalitieswithtrucks);

    Significantsavings toFederal,ProvincialandMunicipal taxpayersduetoreduced

    remediationcostson legacysites.Forexample,DNDhasasignificantamountof

    remediationplannedinthefuture,muchofwhichwillrequiresoildisposal;

    Provides an economically viable solution for the cleanup of local sites

    contaminatedbyformerindustrialactivitiessuchastheincinerationofwaste;and

    Reductionofhydrocarboncontaminantmass.

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    2.0 SiteDescription

    Thissectionofthereportprovidespertinentbackground informationrelatedtotheSite

    availablefrompublicsourcesofinformation.

    2.1 LocationandTopography

    TheSite is locatedat640StebbingsRoad in theSouthShawniganLakeAreawithin the

    CowichanValleyRegionalDistrict(CVRD)onVancouverIsland,BritishColumbia.TheSite

    is approximately 5.0 km south of Shawnigan Lake and 3.3 kmwest of Finlayson Arm.

    DevereauxLakeisapproximately1.5kmsouthoftheSiteandSookeLakeisapproximately

    5.5kmtothewest(Figure1).

    TheexistingmineislocatedintheupperreachesofthesouthShawniganLakecatchment.

    The area is underlain by shallow bedrock as expressed through steep slopes and

    significantrisesinelevation.ThepeakelevationattheSiteisapproximately340mgeod.

    andthegroundsurfacegenerallyrisestothesouth,reachingpeakelevationsof640m

    geod.withintheWarwickRange.

    2.2 Legal

    TheSiteconsistsofasinglelegalparceldescribedasfollows:

    PID: 026226502

    Legal: Lot23,PlanVIP78459,Blocks156,201and323,MalahatLandDistrict

    The current land title is provided in Appendix B. The legal lot boundaries are

    superimposedonFigures2,3,4and8.

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    2.3 Geology

    A review of the Geological SurveyMap 1553A indicates that the Site lies within the

    WarwickRangebetweenSaanichinlettotheeast,andShawniganandSookeLakestothe

    northandwest.TheunderlyingbedrockisknownasWarkGneiss,amafficunitofanearly

    Paleozoicmetamorphic complex. The formation is composed ofmassive and gneissic

    metadiorite alongwithmetagabbro and amphibolites. The unit is generally vertically

    foliateddipping25degreestothenorthwest.

    The ground surface at the Site is an expression of an igneous intrusion of very hard

    granitic bedrock that has resisted erosion and resulted in a local, knobshaped,

    topographic high. This hard granite rock, aswell as theWarkGneiss, are the source

    materialsforthequarry.

    ColquitzGneissisfoundtotheeastandwestoftheWarkGneissunit.Thissilicicunitofa

    similarPaleozoicperiod is also vertically foliated striking to thenorthwest. Theunit is

    composedmainlyofquartzandfeldsparwithlensesofmarbleuptoseveralmetersthick.

    Both units are largely cataclastic and exhibit retrograde metamorphism with severe

    alteration of themain constituents. Contacts between theWark Gneiss and Colquitz

    Gneiss are poorly defined and external contacts are generally faulted and obscure.

    Togethertheunitsunderliea10kmwidebeltwhichextendsfromVictoriaandthecoast

    to Shawinigan Lake to the north, the units terminate against the San Juan and Survey

    MountainFaults.

    TherearenofaultsmappedbeneaththeSite.Thenearestfaultislocatedapproximately

    3km southwest of the Site, and the next closet fault (the Shawnigan Fault) is located

    approximately6kmnorthwestoftheSite.

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    2.4 Hydrogeology

    ThegroundwaterflowregimeinthevicinityoftheSiteispredominantlyviafracturedflow

    withinadeepbedrockaquifer.Limitedoverburdensoilsarepresentintheregion,andare

    generally not sufficient for development of overburden aquifers. The BCMinistry of

    Environmenthasmapped twobedrockaquifers in the region,asshownofFigure3and

    describedbelow:

    TheSpectacleLake/MalahatBedrockAquiferislocatedapproximately1kmeastof

    theSite,andisratedasmoderateproductivityandlowdemand.

    The Shawnigan Lake/CobbleHill BedrockAquifer is located approximately 2 km

    northoftheSite,andisratedaslowproductivityandmoderatedemand.

    ThereisnobedrockaquifermappedbeneaththeSite.However,thereisthepotentialto

    intersectdeepwaterbearing fractureswith sufficientcapacity to servicea residenceas

    indicatedbyWell#86152which is locatedontheSiteandservicesthequarryoffice. All

    existing water wells from theMOE database, within approximately 5 km of the Site

    boundary,areshownofFigure3.

    AdetaileddescriptionoftheSitehydrogeologyisprovidedinSection3.2ofthisreport.

    2.5 Climate

    TheclosestClimateStation(CanadianClimateNormals,19712000)totheSite is located

    at Shawnigan Lake. The total annual precipitation recorded at the Shawnigan Lake

    Climate Station is approximately1,248mm/yr (1,172 falling as rain and75.5 as snow).

    Theaveragemonthlyprecipitationvaries from215mm inNovember to25mm in July.

    Themajorityoftheannualprecipitation(approximately80%)fallsbetweenOctoberand

    March,andthesummersarerelativelydry.TheShawniganLakeClimateStationislocated

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    approximately10kmnorthof theSite,andatanelevationof138mASL. The climate

    normalsareprovidedinTableA.

    TableA:ShawniganLakeClimateData(19712000)

    ClimateData Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Total

    Rainfall(mm) 172 139 115 65 49 40 25 29 38 104 207 190 1,172

    Snowfall(cm) 26.2 16.2 5.6 0.3 0 0 0 0 0 0.6 7.5 19.2 75.5

    Precipitation(mm) 198 155 120 65 49 40 25 29 38 105 215 209 1,248

    DailyAverage(C) 2.7 3.9 5.7 8.4 12 15 17 18 15 9.9 5.4 3 9.6

    Aplotoftheclimatedataisprovidedbelow.

    0

    50

    100

    150

    200

    250

    0

    2

    4

    6

    8

    10

    12

    14

    16

    18

    20

    Mon

    thly

    Pre

    cipi

    tatio

    n (m

    m)

    Mon

    thly

    Tem

    pera

    ture

    (deg

    rees

    C)

    Month

    Climate Normals - Shawnigan LakeAverage TemperatureAverage Precipitation

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    2.6 SurroundingLandUse

    SurroundinglandusesareillustratedonFigure2.

    TheSitelieswithinanareaprincipallyzonedPrimaryForestryandSecondaryForestry,F1

    and F2 respectively. These zones aremainlyused formanagement andharvestingof

    primary forestryproducts,silviculture/horticulture,aswellastheextractionofmineral

    resources. Thezonesalsoallowforuptotworesidentialdwellingsdependingonparcel

    size,andhomebasedbusinesses,includingtheoperationofabedandbreakfast,arealso

    acceptable. Secondary forestryallows forallPrimaryForestryuseswith theadditionof

    thefollowing:sawmilling,manufacturing,andalldrylogsortingoperations.

    The Stebbings Road area is regarded for its production of high grade construction

    aggregates,atleastfivequarriescurrentlyexistwithina1.0kmradiusoftheSite.

    F1/F2

    PrimaryForestry(F1)zonedlandsownedbytheCowichanValleyRegionalDistrict(CVRD)

    are located to the immediate north (Unnamed) andwest (Stebbing Road Community

    Forest).TheunnamedparceloflandwhichstraddlesShawniganCreekonthewestside

    of Stebbings Road includes a linear dedicationwhich runs east across Stebbings Road

    paralleltoGoldstreamHeightsDrivewhereitmeetsaprovincialwoodlot. Theunnamed

    parcel ispartofa largerplan toconnect theShawnigan lake trailsystem to theCapital

    RegionalDistrict(CRD)andTransCanadatrailnetwork.

    Aspartofa rezoning theCVRDacquiredaparcelof landnow known as the Stebbings

    RoadCommunityForest,whichflankstheSiteonthewestand includesanarrowaccess

    corridortoStebbingsRoadalongtheSitessouthpropertyboundary.Priortoitsturnover

    totheCVRDtheparcelhadbeenextensivelylogged,andithassincebeenreplantedwith

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    theintentofprovidingapotentialsourceoffuturerevenuesimilartotheNorthCowichan

    andMapleRidgeCommunityForestinitiatives.

    On Stebbings Road, approximately 320m southeast of the Sites quarry operation, a

    3.7hectares F1 zoned parcelwith one residential dwelling also sits astride Shawnigan

    Creek.Approximately1.2kmsoutheastoftheSite,onGoldstreamHeightsDrive,12lots

    rangingfrom2to7hainsizearecurrentlysellingwithinStonecrestEstates,anF2zoned

    stratasubdivision.

    TothenortheastoftheSite,acrossStebbingsRoadextendingnorthtotheintersectionof

    StebbingsandGoldstreamHeightsDrive,are five1haSecondaryForestry (F2)parcels.

    These parcels have roughedin roads for access to Goldstream Heights Drive, and a

    dwellingunithasbeen recently constructedon thenorthernmostparcelapproximately

    350mfromtheSite.

    CLS1

    Approximately200mtothesouthoftheSite isacomprehensivezonewhichextendsa

    further 2.5 km to the south encompassing Devereux Lake and the Shawnigan Creek

    headwaters. The zone titled community land stewardship (CLS1) includes fivedistinct

    sub zones ranging from Ecological Conservation to Agroforestry. Limited commercial,

    communityfacility,andeducationaldevelopmentispermittedwithintheCLS,aswellasa

    firehall,guest lodgeand somedegreeof infrastructure to support small scale treetop

    accommodationsforecotourism.Thesouthernportionofthesitehasbeenharvestedto

    alargeextent.

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    I1a,I1C&I5

    Agroupingofvarious light industrialproperties is locatedapproximately900mfromthe

    Siteat the intersectionofShawnigan LakeRoad,StebbingsRoadand theE&NRailway.

    This Industrial Park consists of uses including but not limited to aggregate and

    constructionmaterialsuppliers inadditiontowarehousesandsmallfoodserviceoutlets.

    Thezoningallowsforawidevarietyof industrialusesrangingfrom industrialprocessing

    torecyclingfacilities.

    2.7 DistancestoNearestSchools,HospitalsandCareFacilities

    The following Table B summarizes the distance and direction to the nearest schools,

    hospitals,andcarefacilities.ItisevidentbasedontheinformationbelowthattheSiteis

    relativelyremote. Specifically,thenearestschoolandthenearesthospital/carefacility

    are11kmand15kmfromtheSiterespectively.

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    TableB:DistancestoNearestSchools,HospitalsandCareFacilities

    PublicFacility Direction Distance

    Schools CobbleHillElementary3642LearningWay

    S 15km

    DiscoveryElementary2204McKeanRd. NNW 11km

    WillwayElementary2939Mt.WellsDrive SSE 11.5km

    EcoleMillBay3175CobbleHillRoad SSW 13km

    SpencerMiddleSchool1026GoldstreamAve. SSE 13.5km

    GeorgeBonnerMiddleSchool3060CobbleHillRoad NNE 12.5km

    BelmontSecondarySchool3067JacklinRoad SSE 14.5km

    FrancesKelseySecondarySchool953Shawnigan/MillBayRd. NNE 11.5km

    GeorgeBonnerMiddleSchool3060CobbleHillRoad NNE 12.5km

    HospitalsCowichanDistrictHospital3045Gibbins. NNW 27km

    PrioryHospital567Goldstream SSE 15km

    VictoriaGeneralHospital1HospitalWay. SE 16km

    CareFacilitiesPriory(Hiscock&HeritageWoods)567GoldstreamAvenue SSE 15km

    AcaciaTyMawr2655ShawniganLakeRoad, SE 16km

    JeskenAerie817GoldstreamAvenue SSE 14km

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    3.0 ReceivingEnvironment

    A primary objective of this Technical Assessment Report is to document the Site

    conditionsanddeterminethepotentialforimpactstothereceivingenvironmentbasedon

    the Site conditions and theproposed activities. This sectionof the reportdescribes in

    detailthesoilandgroundwaterconditionsattheSite, identifiespotentialreceptorssuch

    as water wells and surface water bodies, and outlines the proposed environmental

    monitoringplan. The informationpresented isobtainedfromSitespecific investigations

    conductedtodate,inadditiontopubliclyavailablesourcesofinformation.

    3.1 SoilConditions

    TheSiteisunderlainbyshallowbedrock,withathinblanketoftillsoilsatsurfaceinareas

    beyond the footprintof the rockquarry. The rockmined from thequarry isextremely

    hard,whichhas resulted in the landform comprising a knoblike,dome shaped surface

    and local topographichighareabecauseof the resistance toerosionversus softer rock

    typessurroundingtheSite.

    Thebedrock at the Site is comprisedof igneous granodiorite andmetamorphic gneiss.

    Thegranodiorite isdescribedasmediumgrained, lightgrey togreen incolor,withdark

    maficmineralgrainswhichgive ita speckledappearance. Thegneiss isadarkgrey to

    blackcolouredrockwithafinelybandedappearance,andiscomposedofmineralssuchas

    hornblendeandplagioclasefeldspar. Themonitoringwells logs(AppendixD)distinguish

    thesetworocktypesasrecordedduringdrilling.

    Asa resultofminingoperations todate,all surficial soilshavebeen stripped from the

    quarryareaexposingtheunderlyingbedrock.

    Thesoilconditionsarepresented inthecrosssectionsthroughtheSiteandsurrounding

    areas,providedasFigures5,6and7.

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    3.2 Hydrogeology

    Theregionaland localhydrogeologicconditionsarepresented incrosssectionsprovided

    onFigures5,6and7.WelllogsobtainedfromtheMOEdatabase,andlogsformonitoring

    wellsinstalledontheSite,areincludedinAppendixD.

    Regionally,theSite is locatedwithintheupperreachesofthesouthernShawniganLake

    catchment,andapproximately5kmfromShawniganLake.Thegroundwaterflowregime

    that links the upper reaches of the catchment to Shawnigan Lake includes deep flow

    through fractures in the bedrock. Recharge to this flow regime is from infiltration of

    precipitation through exposed and connected fracture zones at higher elevations and

    throughperchedsurfacewaterbodies intheuppercatchmentsuchaswetlands,ponds,

    lakes and streams that sit directly over the bedrock. There is a significant elevation

    difference from the upper reaches of the catchment and the regional groundwater

    discharge elevation at Shawnigan Lake. The upper bedrock appears to be less

    permeable/fracturedthanthedeeperbedrockactingasaconfininglayer.Asaresult,the

    piezometricelevationsaregenerallynearorabovegroundsurfacealongthedeepregional

    bedrockgroundwaterflowpath.

    Within theShawnigan Lake catchment thereare localizedareaswithgroundwater flow

    through overburden soils. These overburden aquifers are recharged predominantly by

    infiltrationofprecipitation,whichisenhancedbyincreasedrunofffromsurroundingareas

    withsteepslopesandshallowbedrock.Theseoverburdenaquifersarefoundinthelower

    elevationareasoftheShawnigancatchmentwheresoilshaveaccumulated inthevalley

    bottom. Existingwell#83568, located inthevalleybottomapproximately700mtothe

    northoftheSite,demonstratesthepotentialforlocalizedoverburdenaquifers(Figures3,

    4and5).

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    Atotalof fivemonitoringwellswere installedtodeterminethegroundwaterconditions

    beneaththeSite.Thesewellsareidentifiedas:

    MW111S;

    MW111D;

    MW112;

    MW113S;and,

    MW113D.

    Themonitoringwell logsare included inAppendixD. Themonitoringwells installedon

    theSitedidnotencounteranywaterbearing fractureswithin theupper17m (55 ft)of

    thebedrock.Fracturezoneswithminimalwaterwereencounteredatdepthsbetween18

    and 19m (58 and 61 ft) atMW113 and between 37 and 43m (121 and 141 ft) at

    MW112. Theonly significant fracture zoneencountered in the threemonitoringwells

    wasat82m(269ft)depthatMW111.Itisalsonotedthatthewatersupplywellonthe

    Site(MOE#86152)didnotencounteranysignificantwaterbearingfracturesuntiladepth

    of79m(258ft).

    Thereappearstobeastratificationoffracturedensity/permeabilitybeneaththeSite. It

    maybepossibletogeneralizethebedrockinto2distinctlayersasfollows:

    UpperBedrockfrom0to75m(0to250ft):Negligiblegroundwaterflow.

    DeepBedrockbelow75m(250ft):Minorgroundwaterflow.

    Themonitoringwellswere installedwithin theactivepitatelevations rangingbetween

    approximately 320 mgeod. and 330 mgeod. The ultimate pit bottom elevation is

    313.5mgeod.,therefore,therewillbegreaterthan65moftheupper lowpermeability

    bedrockthatwillremainbeneaththeultimatepitbottomattheSite.

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    Hydraulic response testing was performed on all five monitoring wells in order to

    determinethehydraulicconductivityofthebedrockaquifer.Theresultsoftherisinghead

    tests are summarized in the following Table C. The field test data and details of the

    analysesareincludedinAppendixE.

    Thestaticwater levelswere initiallymeasuredonSeptember11,2011,and itwasnoted

    thatboth shallow anddeeppiezometers atMW113were artesian at that time. As a

    result,thePVCcasingswereextendedandresurveyedtoallowformeasurementofthe

    piezometricelevationsatthis location. Theelevationsweremonitoreduntilstatic levels

    wereachievedaspresentedinTableCformeasurementsobtainedonJune27,2012.

    TableC:SummaryofHydraulicResponseTestingonMonitoringWells

    MonitoringWell

    TopofPVC FractureZone ScreenInterval StaticLevel HydraulicConductivityElev Depth Elev Depth Elev Depth Elev

    (mgeod.) (m) (mgeod.) (m) (mgeod.) (m) (mgeod.) (m/s)

    MW111S 329.99 none n/a 4450 279285 7.84 322.15 1.6x1010

    MW111D 329.96 82 247 7884 245251 7.88 322.09 1.6x107

    MW112 324.13 3743 279285 3743 279285 2.68 321.46 7.4x1010

    MW113S 323.142 1819 301302 1521 299305 1.39 321.76 7.6x1010

    MW113D 322.929 none n/a 4046 274280 1.83 321.10 5.7x1010

    ThegroundwaterflowvelocitythroughthedeepbedrockaquiferunderlyingtheSitemay

    beestimatedbyaformoftheDarcyEquationasfollows:

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    V=(Kxi)/n,where

    V=groundwaterflowvelocity

    K=hydraulicconductivityofaquifer

    i=hydraulicgradient

    n=effectiveporosityofaquifer

    This equation applies directly to the movement of a fluid through a porous media.

    Therefore, the assumption is made that the bedrock fractures are significantly

    interconnectedtoemulateaporousmedia. This isacommonlyusedassumptionand is

    considered to be reasonable for the bedrock conditions at the Site. The individual

    parametersarediscussedinthefollowing:

    Thehydraulic conductivityhasbeendeterminedby thehydraulic response tests

    andisapproximatedtobe:

    o 7.6x1010m/swithintheupperbedrockfrom0to75mdepth;ando 1.6x107m/swithinthedeepbedrockbelow75mdepth.

    The hydraulic gradient within the upper bedrock was measured to be 0.7%

    towardsthenorthwestonJune27,2012.

    Thehydraulicgradientofthedeep,regionalbedrockisestimatedtobe5%,based

    onthefollowing:

    o TheelevationdifferencebetweenmonitoringwellMW111Dpiezometriclevel on the Site (322 mgeod.) and the elevation of Devereaux Lake

    (400mgeod.), located approximately 1,500 m upgradient of the Site.

    LeakagefromthebaseofDevereauxLakeisinferredtorechargethedeep

    bedrock aquifer, and the conservative assumption of a direct hydraulic

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    connectionbetweenDevereauxLakeandthedeepbedrockaquiferresults

    inahydraulicgradientestimateof5.2%.

    o The elevation difference between the upper regional bedrock aquiferrecharge area (500 mgeod.) and the elevation of Shawnigan Lake

    (120mgeod.), divided by the separation distance (8,000m) provides a

    regionalgradientestimateof4.8%.

    The effective porosity of the bedrock aquifer is estimated to be 15% for the

    purposeofcalculatingtherateofgroundwaterflowbeneaththeSite.

    Therefore, based on the above, the groundwater flow velocity through the bedrock

    aquifersbeneaththeSiteareestimatedtobe:

    UpperBedrock=0.001m/year;and

    DeepBedrock=1.7m/year.

    Atthesevelocities, itrequiresthefollowingnumberofyearsforgroundwaterrecharged

    fromtheSitetoreachShawniganLakeapproximately5kmaway:

    UpperBedrock=3,000,000years;and

    DeepBedrock=103,000yearsincludingverticalandhorizontalflowpaths.

    Therearesomesignificantconclusionsthatmaybedrawnwithrespecttotheproposed

    facilityandthehydrogeologicconditionsattheSite,asfollows:

    Groundwater flow through theupperbedrockat theSite isnegligible, therefore

    theriskofimpactinggroundwaterislimitedtothedeepgroundwaterflowthrough

    bedrock.

    Deepgroundwaterflowthroughbedrockoccursbeneathaconfininglayeroflower

    permeabilitybedrockapproximately65m(210ft)inthicknessatthecompletionof

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    mining. This layer protects the deep bedrock aquifer from impacts originating

    fromabovesuchastheproposedfacility.

    Theverticaltraveltimefromgroundsurfacetothedeepbedrockaquiferwouldbe

    greaterthan100,000yearsusingtheverticalgradientmeasuredbetweenMW11

    1SandMW111D(0.4%).

    Deepgroundwaterflowoccursatavelocityofapproximately1.7m/year,whichis

    veryslowandthereforefurthermitigatestheriskofenvironmentalimpacts.

    The horizontal groundwater travel time to Shawnigan Lake within the deep

    bedrockaquifer isapproximately3,000years. This isasignificant lengthoftime

    whichfurthermitigatestheriskofenvironmentalimpacts.

    The horizontal groundwater travel timewithin the deep bedrock aquifer to the

    nearestexistingwatersupplywell(MOEWellTag#86152),located150mfromthe

    Site, isestimatedtobeapproximately88years (plusanadditional100,000years

    forverticaltraveltime).

    Anyleachategeneratedbytheproposedfacilityhassignificantverticalseparation

    fromthedeepbedrockaquifer;

    Overall,thepotentialforleachatederivedfromtheproposedfacilitytoimpactthe

    environmentviagroundwaterflowthroughthebedrockisextremelyremote.

    3.3 NearbyDrinkingWater,Irrigation,andLivestockWells

    TheBCMinistryofEnvironmentonlineWELLSdatabaseandWaterResourcesAtlaswere

    used to identifywells in thestudyarea. The locationsof identifiedwellsareshownon

    Figure3,andrecordsforpertinentwells located incloseproximitytotheSiteandalong

    the regional crosssection are included in AppendixD. No irrigation or livestockwells

    were identified. All pertinentwell records indicate that thewells are used to supply

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    drinkingwater.Asummaryofallwellswithin1kmoftheSiteisprovidedinthefollowing

    TableD.

    TableD:SummaryofWaterWellswithin1kmoftheSiteMOEID DepthtoBedrock WellDepth WellYield

    WellTagNo. (m) (ft) (m) (ft) (USGPM)

    83527 6.1 20 94 307 3

    83531 16.8 55 63 207 20

    85099 0.6 2 215 707 2.5

    86036 12.8 42 135 442 1.25

    86037 0.9 3 110 362 35

    86152 0.0 0 99 325 20

    89253 2.7 9 69 227 10

    93401 0.0 0 38 125 30

    95480 4.3 14 81 265 6

    95485 2.4 8 123 405 4

    96080 1.5 5 62 205 3

    Average 4 14 99 325 12

    As shown in theabove table,groundwater supplywells in theareaaverageadepthof

    approximately 100m,which concurswith the conclusions drawn in Section 3.2 of this

    reportregardingthestratificationofwaterbearingfracturesinthebedrockinthisregion.

    In general, water wells are drilled to the minimum depth required to produce the

    necessaryyield.Therefore,theapproximately75mthicknessoflowpermeabilityrockat

    groundsurfaceidentifiedontheSiteappearstobeapplicabletothesurroundingbedrock

    intheareaasinferredfromthewellswithin1kmoftheSite.

    Well93401islabeledonFigures3and4,anditslogisincludedinAppendixB.Thiswellis

    locatedapproximately600msouthwest(upgradient)oftheSite. Thewell log indicates

    thatitwascompletedto38mdepth.Thegroundelevationatthiswellisapproximately

    385mindicatingacompletionelevationofapproximately347m.Therefore,thebottom

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    of thewell is above the original ground surface elevation on the Site. As a result, no

    groundwater flow canoccur from theSite to thiswellevenunderpumping conditions.

    Extrapolating Section BB (Figure 6), it is anticipated that thiswill is completed in the

    lower bedrock unit despite its shallow depth. It is noted that the thickness of the

    confiningupperbedrockdecreasesupgradientof theSiteandat thehigherelevations

    whererechargetotheloweraquiferoccurs.ThisisillustratedonFigure6.

    The BC Ministry of Environment provides an online Water Resources Atlas

    (http://www.env.gov.bc.ca/wsd/data_searches/wrbc/)thatmapsallmajoraquifersinthe

    provinceandprovidesratings(low,moderateorhigh)foraquifercharacteristic including

    productivity,demandandvulnerability. TheAtlasdoesnotmapanaquiferbeneaththe

    subjectSite,andthetwonearestaquiferstotheSiteareshownonFigure3anddescribed

    below:

    ShawniganLake/CobbleHillAquifer: Locatedapproximately2kmnorthofthe

    Site,thisbedrockaquifer isdescribedas lowproductivity,moderatedemandand

    highvulnerability.

    SpectacleLake/MalahatAquifer: Locatedapproximately1kmeastoftheSite,

    thisbedrockaquifer isdescribedasmoderateproductivity, lowdemandandhigh

    vulnerability.

    TheShawniganLake/CobbleHillAquiferislocatedapproximately2kmdowngradientof

    theSite,andthetraveltimeforgroundwaterflowwithinthedeepbedrockbeneaththe

    Site to reach the mapped aquifer is estimated to be approximately 1,000 years

    (horizontallyonlyandnotincludingverticalflowfromgroundsurfacetothedeepaquifer

    whichwould requireanadditional100,000yearsor so). TheSpectacle Lake /Malahat

    Aquifer is locatedwithinadifferentcatchmentareathantheSite,andthereforethere is

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    nohydraulicconnectionbetweengroundwaterinthedeepbedrockbeneaththeSiteand

    thisaquifer.

    3.4 ApplicableCSRSiteSpecificFactors

    Theexisting landuseasa rockquarry is considered tobe Industrial (IL)under theCSR

    classification. Theproposeduse as a contaminated soil treatment anddisposal facility

    wouldalsobeconsideredCSRIL.

    TheproximityofShawniganCreekanditstributariesresultintheCSRfreshwaterAquatic

    Life (AW) standards being applicable to the Site. In addition the BC ApprovedWater

    QualityGuidelines(BCAWQG)areapplicabletonearbysurfacewaterbodies.

    The presence of approximately 75m of very low permeability (1010m/s) bedrock at

    ground surfaceand sincenoexistingwellsarepresentwithin150m, removes theCSR

    DrinkingWater (DW) standards from being applicable to the Site. The CSR Technical

    Guidance Document 6 (Water Use Determination) indicates that Drinking Water

    Standards(DW)applywherecurrentdrinkingwatersources(groundorsurface)arewithin

    500mof theouterextentofagroundwatercontaminationsource. If thegroundwater

    flowdirectionhasbeenreliablydetermined,thisdistanceislimitedto100mupgradient

    (remainingat500mdowngradient)oftheouterextentofacontaminationsource.

    Futuredrinkingwaterusemustalsobeconsidered in theevaluationofwhetherornot

    DWstandardsapplyatasite.Thisincludesevaluationoftheunderlyingaquifertoassess

    hydraulicparametersincludingyieldandhydraulicconductivity.Iftheaquiferunderlying

    a sitehasahydraulic conductivitygreater than1X106m/s,anda yieldgreater thanor

    equalto1.3L/min,thenDWstandardsareconsideredtoapply.

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    Exceptions to the application ofDW include situationswhere the natural groundwater

    qualityisconsideredunsuitablefordrinkingwaterusebasedonelevatedTotalDissolved

    Solids (TDS 4,000mg/L); orwhere groundwater is containedwithin organic soils or

    muskeg.Also,insituationswherethereexistsaconfininggeologicalunitthatadequately

    protectstheaquifer,DWdoesnotapply. Aconfininggeologicalunit isdefinedasbeing

    uniformandfreeoffractures,continuousacrossthesite,andgreaterthan5mthickwitha

    bulkhydraulicconductivitylessthanorequalto1X107m/s.

    InordertoaddressthepotentialapplicabilityofDWbasedoncurrentuses,ActiveEarth

    searchedtheBCWaterResourceAtlas. Thissearchrevealedthenearestdrinkingwater

    welltobeapproximately150meastoftheSiteboundary, inanupgradientorientation

    relative to the Site (well tag 95485). No wells were indicated in a downgradient

    orientation within the 1 km search radius. The onSite well (86152) is not used for

    potabilitypurposes.

    In order to assess future drinking water use, we determined there to be a suitable

    confining geological unit in the form of the upper bedrock. This confining unit was

    determinedtomeetthecriteriaspecifiedinGuidanceDocument6.

    Followingclosureoftheproposedfacility,therewillbea2mcleansoilcapplacedoverthe

    Sitethatweremoveterrestrialexposurepathwaystothecontaminatedsoil,inadditionto

    theLLDPEcap liner. Theclosedfacilitywillposenounacceptableriskstohumanhealth

    and/ortheenvironment.

    3.5 HydrologyofWaterDischargeLocation

    SurfacewaterfeaturesonandsurroundingtheSiteareshownonFigure4.Thesefeatures

    include:

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    ShawniganCreektotheeastoftheproposedfacilityontheSite;

    Anephemeral tributary toShawniganCreek to thenorthwestof theSite,witha

    tributary to this thatoriginateson the Site and flows from the Siteat thewest

    propertyline;

    AnephemeralwetareaontheSite,tothesoutheastoftheproposedfacility,that

    drainsintoShawniganCreekalongaditch;

    AnexistingSettlingpondontheSite,tothesoutheastoftheproposedfacility,that

    drainsintotheabovedescribedephemeralwetarea;and

    ExistingSettlingpondswithintheexistingquarryfootprint,onthewestsideofthe

    Site,thatwillbeaugmentedfortheproposedfacility.

    ThepredevelopedSiteconsistedofacentralcrestwith runoff travellingdownhill inall

    directions;reportingtoanephemeraltributaryofShawniganCreektothenorthwestand

    directly to ShawniganCreek to the east. The final capof the proposed landfill facility

    would generally reinstate the predeveloped Site conditions. During operation of the

    proposedfacility,theephemeraltributaryoriginatingontheSiteandexitingatthewest

    propertylinewouldbethereceptorofallwaterdischarges.Itisproposedtodischargeall

    waterdirectlytothissurfacewaterbodyontheSitefollowingmonitoringandtreatment.

    ThetributarylocatedonthewestsideoftheSitethatwillbetheinitialreceptorofwater

    discharges from theproposed facilitydoesnotappear to sustainabaseflow in thedry

    summer months, as evidenced by Site reconnaissance of the area in August 2011.

    However,thegroundsurfacealongthissurfacewaterflowpathwaywasobservedtobeat

    ornearsaturationduringthereconnaissance.

    ShawniganCreekflowsthroughtheSite,withinaprotectedcovenantareatotheeastof

    theexistingquarry andproposed facilityoperations. During the late summer, flows in

    ShawniganCreekareestimatedto fallbelow5USgpm (seephotos inAppendixC). This

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    baseflow is sustained from discharges from small lakes upstream of the Site including

    DevereauxLakeandLoganLake.

    TheSitecomprisesapproximately0.3%ofthesouthernShawniganLakecatchmentarea,

    andthereforedoesnothavethepotentialtosignificantly impacthydrologicalconditions

    withinthecatchment.

    A contingency area for collection of stormwater drainage and potential discharge is

    located in the southeastareaof the Site,and consistsof anexisting Settlingpondand

    ephemeral wet area that drains to Shawnigan Creek. Augmentation of the existing

    Settlingpondandditchwould likelybe requiredprior to incorporating thiscontingency

    areaintotheproposedfacilitystormwatermanagementsystem.Additionalsurfacewater

    monitoringofthisareawouldalsobeundertakenifthisareaistobeutilized.

    During operation, the proposed facility will not have a significant impact on the

    surrounding surfacewater bodies as discharge volumeswill not be increased over the

    existingquarryoperation.ThemajorityoftheSiteiscurrentlyexposedbedrockwithinthe

    footprint of the quarry and proposed facility, therefore, runoff rates will not be

    appreciablyincreasedbydevelopmentoftheproposedfacility.Uponclosure,theSitewill

    berestoredtonearpredevelopmentconditionswithrespecttosurfacewaterflows.

    3.6 EnvironmentalMonitoringPlan

    Theenvironmentalmonitoringplan includes groundwater and surfacewaterbodies at,

    and immediately adjacent to, the Site. Analyses included physical parameters, anions,

    nutrients, bacteriological, total metals, dissolved metals, volatile organic compounds,

    polycyclic aromatic hydrocarbons and extractable petroleum hydrocarbons. The

    laboratoryanalyticalreportsareincludedinAppendixF.

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    Thegroundwatermonitoringplanhasbeeninitiatedbytheinstallationoffivemonitoring

    wellsatthreelocationsontheSite.Samplesfromthesewellshavebeenanalyzedandthe

    resultsarepresentedonTables1through4.ThegroundwaterqualitymeetstheCSRAW

    (Aquatic Life) standards for all parameters tested with the exceptions of Cadmium,

    ManganeseandSodium. Noexceedences forCSRDW (DrinkingWater)standardswere

    measuredinthemonitoringwells.

    Baseline surface water samples were collected from three locations along Shawnigan

    CreekandthreelocationsalongtheephemeraltributarytothewestoftheSite,asshown

    onFigures4,8and15.Thesurfacewatermonitoringlocationsarelocatedupstreamand

    downstreamoftheproposedfacility,andtheanalyticalresultsarepresentedonTable5

    through8.ThesurfacewaterqualitymeetstheBCAWWQGstandardsforallparameters

    testedwiththeexceptionsofNitrate,Barium,Chromium,IronandToluene.

    Considerationwasgivenfortheneedtoconductbenthicorganismandsedimentsampling

    withintheephemeraltributarytoShawniganCreek.However,basedonthehighquality

    ofthedischargedwater(meetsBCAWWQGandTSS

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    3.7 CumulativeEffectsfromOtherDischargesintheArea

    Thesurrounding landuseswerereviewedto identifyotherdischargesoractivities inthe

    area thatcouldhaveacumulativeeffecton the impactsanticipated from theproposed

    facility.Thereviewidentifiedtwoexistingoperations:

    TheminingactivitiesonthesubjectSite;and

    ThedepositofcleansoilontheadjacentfillSitetothenorthonStebbingsRoad.

    The cumulative effect of the proposed facility with consideration of the two existing

    activitieswouldbenegligibleorresultinanimprovement.

    Thegroundwaterflowsystemwithinthebedrockaquiferisnotexpectedtobeimpacted

    byeither theexistingorproposedactivitiesasa resultof thehydrogeologic conditions

    presentattheSite(seeSection3.2).

    Theproposed surfacewatermanagement systemwillensureall runoff isappropriately

    diverted,collected,treatedanddischarged. Thiswillresult inanegligible impacttothe

    receivingenvironment.Furthermore,theproposedsurfacewatermanagementsystemis

    more robust than theexisting systemon the Site currentlyutilized for the rockmining

    operation. Since the quarry and the proposed facility will operate within the same

    footprint,theneteffectoftheproposedsurfacewatermanagementsystem isexpected

    tobeanimprovement.Agreaterlevelofcontrolandmonitoringwillbeinplacetoensure

    potentialenvironmentalimpactsareminimized.

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    4.0 SourceMaterial

    Ingeneral,thetargetsourcematerialfortheproposedfacilityincludescontaminatedsoils

    andsomeindustrialwastespresentonsitesintheSouthernVancouverIslandregion.

    The sourcematerialwould contain concentrationsof regulated substances thatexceed

    applicable landuse standards asdefinedby theBCCSR and/orCCMEGuidelines. The

    contaminationwouldhave resulted froma rangeofcommercialand industrialactivities

    suchasthoselistedinSchedule2oftheCSR.

    Nodisposalofliquidswillbepermitted.

    It isanticipated that themajorityof thesourcematerialwould requiremovement from

    thegivensourcesitestofacilitateremediation.

    4.1 ContaminantsofConcern

    Soilsacceptedattheproposedfacilitymaycontainoneormoreofthecontaminantslisted

    undertheContaminatedSitesRegulation,Schedules4,5,7and10.Thebroadcategories

    ofcontaminantsandspecificcontaminantsineachcategoryincludethefollowing:

    InorganicSubstancesMetals

    PetroleumHydrocarbonsBenzene,Ethylbenzene,Toluene,Xylenes(BTEX),Styrene,Methyl Tributyl Ether (MTBE), Volatile Petroleum Hydrocarbons (VPH), LightExtractable Petroleum Hydrocarbons (LEPH), Heavy Extractable PetroleumHydrocarbons(HEPH)

    Polycyclic Aromatic Hydrocarbons Benzo[a]pyrene, benz[a]anthracene,benzo[b]fluoranthene, benzo[k]fluoranthene, dibenz[a,h]anthracene, indeno[1,2,3cd]pyrene,naphthalene,phenanthrene,pyrene,

    Chlorinated Hydrocarbons Chlorinated aliphatics (chloroform, dichloroethane,dichloroethene, dichloromethane, 1,2dichloropropane, 1,3dichloropropene, carbon

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    tetrachloride, trichloroethane), chlorobenzenes (trichlorobenzene,tetrachlorobenzene, pentachlorobenzene), dichlorobenzenes (1,2dichlorobenzene,1,3dichlorobenzene, 1,4dichlorobenzene), hexachlorobenzene, lindane,monochlorobenzene, tetrachloroethylene, trichloroethylene, vinyl chloride,polychlorinatedbiphenyls.

    Phenolic Substances Chlorinated phenols (chlorophenol isomers, dichlorophenols,trichlorophenols, tetrachlorophenols), pentachlorophenol, nonchlorinated phenols(2,4dimethylphenol, 2,4dinitropheno, 2methyl 4,6dinitrophenol, nitrophenol,phenol,cresol)

    GlycolsEthyleneGlycol,PropyleneGlycol

    Wastematerialsfromindustrialprocessesincludeincineratorash(nonHazardousWaste)

    withcontaminantsofpotentialconcernincludingmetalsandhydrocarbons,perabove.No

    liquidwasteswillbeaccepted.

    4.2 MaximumConcentrations

    Soilsacceptedattheproposedfacilitywillnotexceedthestandardssetoutforhazardous

    wasteintheHWR(i.eHazardousWastewouldnotbeaccepted).Allsoilswillalsobenon

    leachable. Soilwith contaminant concentrations exceeding CSR residential, commercial

    andindustrialstandardswouldbeaccepted.

    Potentially problematic parameters including moisture content, pH and incompatible

    wastetypesarediscussedinthefollowing.

    SoilMoistureContent

    Moisturecontentcanbecomeproblematicwhensoilsaresupersaturatedandfreewater

    is able to drain from the soil. This freewater can provide a transportmechanism for

    contaminantstomobilizeandpotentiallycreateleachate;atleastuntilthesoildrainstoa

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    stable moisture content. However, the potential to generate leachate from

    supersaturatedsoils isconsideredtopresentavery lowriskasthesoilsacceptedtothe

    facilitywillnotbe leachableand thevolumeofwaterderived fromsupersaturatedsoils

    willbesmall. Nonetheless,thepossibilityofspecifyingmaximummoisturecontents for

    soiltobepermanentlyencapsulatedwasevaluatedasdescribedinthefollowing.

    The maximum moisture content that can be held within the soil before it becomes

    supersaturated is related to the soil type. There isawide rangeof saturatedmoisture

    contentsthatcanoccurfordifferentsoiltypesasshowninthefollowingtable.

    TableE:SoilTypevsMoistureContent

    SoilType SaturatedMoistureContent

    Gravel

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    moisture content. Soilsmusthaveamoisture contentbelow saturation inorder tobe

    placedwithinthepermanentencapsulationarea.

    Based on the continuum for potential moisture content, visual inspection of soils is

    consideredtobetheonlypracticalwayofassessingthepresenceofsupersaturatedsoils.

    ToreiteratethatthepossibilityexistsforsupersaturatedsoilstobeacceptedtotheSoil

    ManagementArea,however,thesesoilswillbetreatedtoreducethemoisturecontentto

    belowsaturationpriortopermanentencapsulation.

    SoilpH

    The potential for pH to be problematic either by impacting liner stability and/or

    mobilizationofcontaminantssuchasmetalsfromsoilrequireseitherdirectlinercontact

    ora transportmechanism suchas themigrationofwater. Without theability to react

    withthe liner,pHdoesnotposeariskto linerstability. Withoutatransportmechanism

    such as water, it is not possible to mobilize contaminants and therefore pH is not

    consideredasignificantrisk.

    Thesoilplacedinthepermanentencapsulationcellsisseparatedfromdirectcontactwith

    the linersviathecleansanddrainageblanketandgeofabrics,removingthepotentialfor

    directlinercontact.

    The facilitydesignandoperationaimstoremovethetransportmechanismandmitigate

    the potential for leachate generation. Temporary and permanent coversmitigate the

    impacts of incident precipitation both within the soil management area and the

    permanentencapsulationarea. Sitedrainageworksensure that thecellsareprotected

    against runoff, and screening for supersaturated soils mitigates the potential for soil

    moisturetoproduceleachate.

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    Any leachategeneratedwillbecollected,monitoredandtreatedpriortodischarge. The

    treatment systemwill have the ability to handle a full range of potential pH levels if

    encountered.

    IncompatibleWasteTypes

    Similar to the rationaledescribedabove forpH, thepotential forcomplications toarise

    fromincompatiblewastetypesisconsideredtobelowbecauseofthelackofatransport

    mechanism for the waste types to interact. That said, precautions will be taken to

    segregate potentially incompatiblewastes by encapsulating thesewastematerials into

    separatecells. Cellsizesarevery flexibleand it ispossible tocreateverysmallcells to

    mitigatethisconcernasneeded

    4.3 ConfirmationSoilisNotHazardousWaste

    Ingeneral,soilswillbecharacterizedatthesourcesiteandthedatawillbereviewedby

    qualifiedpersonnelprior to acceptance to the facility. Therewillbe a requirement to

    provide key laboratory analytical data to support the determination of soil as non

    Hazardous Waste. For example, all materials will require leachability testing results

    performedbyanaccreditedlaboratory.Thisstepwillprovidetheprimaryconfirmationof

    soilquality.

    Hazardous Wastes as defined under the Hazardous Waste Regulation are not to be

    imported to the landfill facility. Thiswould includeall categoriesofHazardousWastes

    listedintheRegulations.TheWasteApprovalApplicationFormrequiresthatGenerators

    state thatHazardousWastes arenotpresent. In addition, analyticaldataprovided for

    each shipment of soilwill be reviewed against theHWR standards,which include the

    following:

    BiomedicalWastesasdefinedintheHWR.

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    Free Liquidmeansanyquantityofa liquidwhich is separated froma solidwhensubjectedtotheFreeLiquidTestProceduredescribedinPart3ofSchedule4.

    HouseholdHazardousWastesasdefinedbytheHWR.

    Leachable ToxicWaste Meanswastewhen subject to the extraction proceduredescribed in the US EPA Method 1311 produces an extract with a contaminantconcentrationgreaterthanthoseprescribedinTable1ofSchedule4.

    PCBWastesmeansPCBliquid,PCBsolidandPCBequipmentthathavebeentakenoutof service for thepurposeof treatment, recycling, reuseordisposalor for thepurposeofstoragepriortotreatment,recycling,reuseordisposal.

    RadioactiveWastemeanswaste containingaprescribed substanceasdefined inthe Atomic Energy Control Act in sufficient quantity of concentration to require alicenceforpossessionoruseunderthatActandregulationsmadeunderthatAct.

    WasteAsbestosmeansawastecontainingfriableasbestosfibresorasbestosdustinaconcentrationgreaterthan1%byweighteitheratthetimeofmanufacture,orasdeterminedusingamethodspecifiedinSection40(1).

    WasteContainingDioxinmeansawastecontainingdioxinTEQ (asdefined in theHWR)inaconcentrationgreaterthan100partsperbillionbyweight.

    Waste containing Polycyclic Aromatic Hydrocarbons means waste containingpolycyclicaromatichydrocarbons inatotalconcentrationgreaterthan100partspermillionmeasuredaspolycyclicaromatichydrocarbonTEQ(asdefinedbytheHWR)byweight.

    Waste Containing Tetrachloroethylene means a waste containingtetrachloroethyleneinaconcentrationgreaterthan100partsperbillionbyweight.

    WasteOilmeansautomotive lubricatingoil,cuttingoil,fueloil,gearoil,hydraulicoiloranyotherrefinedpetroleumbasedoilorsyntheticoilwheretheoilsareinthewaste ina totalconcentrationgreater than3%byweightand theoils throughuse,storage or handling have become unsuitable for their original purpose due to thepresenceofimpuritiesorlossoforiginalproperties.

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    WastePestControlProductsincludescontainersandwastecontainingpestcontrolproducts, including wastes produced in the production of treated wood productsusingpestcontrolproducts.

    The Transportation of Dangerous Goods (TDG) regulation also specifies Hazardous

    Wastes,however,thiswillnotbeusedforscreeningcontaminantsatthefacility.Rather,

    thisRegulationwouldbeusedtomanagethemovementandtransportationofWastes

    It isrecognizedthatsomeparametersmayexceedHWRLQSwhenCSR ILstandardsare

    met. Forthisreason,allsubstanceswillbescreenedagainsttheHWRLQSbyassuming

    the entire concentration is leachable (i.e. multiplying the LQS by 20 L/kg). When

    substancesarefoundinexcessoftheselevels,thentheGeneratorSitewillberequiredto

    providetheTCLPanalysistoconfirmalackoftheHWRLQSexceedances.

    4.4 QA/QCofIncomingSoilQuality

    To confirm the quality of incoming soil meets the requirements of the facility, the

    followingprotocolswillbefollowed:

    Contaminatedsoilwillbecharacterizedatthesourcesite inaccordancewiththe

    CSRrequirements,priortorelocationtothefacility.Thisdatawillbereviewedby

    qualifiedprofessionalfacilityrepresentativespriortoanysoilbeingrelocated.

    All soilswillbe initially stored in theSoilManagementArea forassessmentand

    confirmationofsoilquality.

    AllsoilswillbescreenedagainsttheHWRLQSusingtheruleof20,todetermine

    ifconfirmatorycharacterizationisrequired.

    Incaseswheresoilcharacterizationatthesourcesiteisconsideredtobemarginal,

    additionalcharacterizationatthefacilitywillbeundertakeninaccordancewiththe

    MOETechnicalGuidanceDocument1(GD1).

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    All incomingsoilwillbesubjecttorandomandsystematicconfirmationfromsoil

    samplescollectedbyfacilitypersonnel.

    Oncesoilqualityhasbeenconfirmedbyqualifiedpersonnel,thesoilmaythenbe

    relocatedon Site to the soil treatment areaor to thepermanentencapsulation

    areadependinguponthenatureofthecontaminants.

    EmphasisisplacedonsoilbeingappropriatelycharacterizedatthesourceSite;theWaste

    Approval Application includes reference to soil characterization in accordancewith

    GuidanceDocument1.

    Thischaracterizationshould includeappropriateanalyticalQA/QCchecks,andstatistical

    analyses in accordance with MOE Technical Guidance Document 12 (Statistics for

    Contaminated Sites) and Technical Guidance Documents 10 and 11 (Checklist for

    ReviewingPSIandDSIrespectively).

    AQualifiedProfessionalwillaccountforthesoilbeingappropriatelycharacterizedpriorto

    thesoilbeingacceptedtotheFacility.

    Fortheconversionfromtruck loadstovolume,a load isconsideredtobeatandemaxle

    dump truck typically carrying about 1214 tonnes. At a density of 2 tonnes/m3, this

    representsapproximately67m3ofsoil.

    In addition to soil chemical quality, incoming soilswill also be screened formoisture

    content. Asdescribedabove,moisturecontentcanbecomeproblematicwhensoilsare

    supersaturatedandfreewaterisabletodrainfromthesoil.

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    4.5 HoldingCellforSuspect/RejectSoil

    AllsoilacceptedtothefacilitywouldbeinitiallyplacedintheSoilManagementArea.This

    area will be asphaltpaved with appropriate water management systems in place to

    controlandcollectrunoff,monitorwaterquality,treatifnecessaryandthendischargeas

    appropriate.

    WithintheSoilManagementArea,apermanentlycoveredarea,oranareadesignedfor

    coveringsoil(tarpsandlockblocks),willbepresentforthetemporarystorageofsuspect

    HazardousWastesoils.Allsuspectsoilswouldbeplacedinthisareaandrecharacterized

    toconfirmsoilquality.

    Soil identified tomeetorexceed theHWRstandardswouldbeshipped toanapproved

    facilityoffSite.

    4.6 SoilAcceptancePlan

    The soil acceptance plan has twomajor components; acceptance to the facility, and

    acceptancetothePermanentEncapsulationArea.

    Soilacceptancetothefacilityincludesthefollowingcomponents:

    Completion of a standardWaste Approval Application form to filled out by a

    qualified,professionalrepresentativeofthesourcesite;

    Review of data, reports and available documents by a qualified professional

    representative of the facility to assess if soil quality has been adequately

    characterized;

    Acceptedsoil isreceivedtotheSoilManagementArea foradditionalassessment

    and characterization as determined to be necessary by the facilitys qualified

    professional;

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    Soil received to the SoilManagementAreawillbe stockpiled indesignated and

    signedareasinwindrowsorincoveredcellsasdeterminedbysoilquality;

    Soilwillbestockpiled intheSoilManagementAreaunderthedirectionoffacility

    personnelandallstockpileswillbemarked inthefieldandonthedailystockpile

    monitoringsheets(standardizedform);

    Oncesoilqualityhasbeenconfirmedbyqualifiedpersonnel,thesoilmaythenbe

    relocatedonSite to theSoilTreatmentAreaor to thePermanentEncapsulation

    Areadependinguponthenatureofthecontaminants.

    SoilacceptedtothePermanentEncapsulationAreacouldbesourcedfromeithertheSoil

    Management Area or the Soil Treatment Area depending upon the nature of the

    contaminantsandinaccordancewiththefollowing:

    SoilsmustbeadequatelycharacterizedasnonHazardousWaste;

    Soils with metals contamination may be relocated directly to the Permanent

    EncapsulationAreafromtheSoilManagementArea;

    Soilswith organic contaminants that are not responding to treatmentmay be

    relocatedfromtheSoilTreatmentAreatothePermanentEncapsulationArea;

    Soilswillbeplaced inengineered cellswith appropriate liners, covers,drainage

    systems,andleachatedetection/collectionsystems;and

    Landfill cells will be designed and constructed in conjunction with the quarry

    operations to facilitate land reclamation coincidentally with the

    progress/completionofminingactivitiesadiscussedindetaillaterinthisreport.

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    5.0 SoilDischarge

    5.1 VolumeofSoilPerYearDischarged

    TheSitehasthecapacity/requirementtoacceptatotalof15,000,000m3ofmaterialfor

    minereclamationpurposes.Itisestimatedthatapproximately70%ofthisvolumecould

    beutilizedforthepermanentcontainmentofcontaminatedsoils,andtheremaining30%

    ofthevolumewouldcomprisethedrainageblankets,covermaterials,finalcapmaterial,

    celllayoutinefficienciesandfacilityinfrastructure.

    Therockquarryhasanestimatedoperatinglifeof60yearsandiscurrentlyinPhase5of

    themineplan(thereareatotalof20Phases).Todate,atotalof580,000m3ofmaterial

    hasbeenremovedfromthemineand,assuch,miningisapproximately4%complete.

    Theproposedfacilitywouldoperateconcurrentlywiththeminingoperation.Soilswould

    be landfilled in cellswithin completed phases of themine. It is difficult to accurately

    predictthevolumeofcontaminatedsoilthatwouldbeacceptedannuallyattheproposed

    facility, as there are several factors that would impact the demand for a local soil

    treatment and disposal facility such as regulatory requirements, real estate market

    conditionsand localgovernmentpolicies. It isanticipated thatdemandmaybehigher

    initiallyduetoabuildupresultingfromthe lackofa localdisposalalternative,andthen

    demandmaydropoff toamorestable levelasdictated largelybyeconomicconditions

    andtherealestate/landdevelopmentmarketsinparticular.

    Therateofsoildischargedoverthelongtermofthefacilityoperationwouldbelimitedby

    therateofaggregateextraction.Therateofaggregateextractionattheminetodate,has

    averagedapproximately100,000m3/yearoverthepast6years.Therateofextractionis

    anticipated to increaseover themine life inaccordancewithdemand. It isanticipated

    that somemodification to theminingoperation sequenceofphaseswillbe required to

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    allowfortheconcurrentactivitiesoftheproposedfacility/reclaimationandthemining

    operations.

    Insummary,soildischargerateswillbelimitedbyrockminingratesprovidedthedemand

    ispresent.Therateofrockminingiscurrentlyabout100,000m3/yearandanticipatedto

    increaseovertheremainingminelifespanofapproximately60years.Thelongtermrate

    forsoilacceptancetothepermanentlandfillwillbelimitedbyeitherthisrateofminingor

    thelongtermdemandforasoildisposalfacilityintheregion.Assuch,theapplicationis

    madeforannualdischargeofwasteatarateof100,000tonnes.

    5.2 Concentrations/LevelatDischarge

    TheSiteiscurrentlyclassifiedashavinganindustriallanduse(CSRIL)accordingtotheBC

    CSR. The landuseof theSite inpartdetermines theacceptable levelsofcontaminants

    thatmaybepresentinshallowsoils.Ifthelanduseofasitechanges(uponclosureofthe

    mineandproposedfacility),therewouldbeatrigger(suchasadevelopmentpermit)fora

    reevaluation of site conditions, including the assessment of soil quality related to

    potentialimpactsonhumanhealthandtheenvironment.

    The proposed facility has been developed conceptuallywith the understanding that a

    moresensitivefuturelandusewillultimatelyoccupytheSite;suchasresidential(CSRRL)

    and/orpark(CSRPL) landuses. Specifically,onlynon leachablesoilswillbeacceptedat

    the facility. To provide additional factors of safety, the engineered landfill cells will

    permanentlycontainthecontaminatedsoilsandpreventtheexposuretomoistureinthe

    event that any leachablematerialwas inadvertently received. An additionalbarrier to

    leachate impacts includes a seepage collection system that is routinelymonitored and

    treated ifnecessarypriortodischarge. Finally,theentire landfillwillbecoveredwitha

    cleansoilcapwithaminimumthicknessof2.0m. Thissoilcapwillmitigateallpotential

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    exposurepathwaysforhumansandtheterrestrialecosystem,asitisdoublethethickness

    generallyrequiredatriskmanagedcontaminatedsitesinBC.

    Soil discharged may exceed the generic numeric soil standards set out in the

    EnvironmentalManagementAct(EMA)ContaminatedSitesRegulation(CSR)pertainingto

    industrial land use (IL). However,no soil that is classified asHazardousWastewill be

    placedatthefacility.

    Soilscontaminatedwithorganicsubstancesthatareamenabletobioremediationwillbe

    treatedatthefacilitypriortodischarge. Thesesoilswouldbetreatedtoconcentrations

    below the CSR IL standards if possiblewith a reasonable level of effort. Successfully

    treatedsoilsmaybeusedforcellcovermaterialsifappropriate.

    Soils contaminatedwith inorganic substances that are not amenable to treatment via

    bioremediationwillbeencapsulatedfollowingstandardfacilityscreeningandtesting.

    5.3 ConcentrationConfirmation

    Soilreceivingprotocolswillprovideconfirmationofsoilconcentrationsandaredescribed

    inSection10ofthisreport.

    Soilstreatedatthefacilitywillbereclassified inaccordancewithGD1thatspecifiesthe

    recommended density andmethodologies for sampling stockpiles. A copy of GD1 is

    includedasAppendixGforeaseofreference.Ingeneral,onesamplewillbecollectedfor

    every10m3ofsoilundergoingtreatment.

    Typically,soilsundergoingtreatmentwillberandomlysampledtomonitortheprogressof

    bioremendation. Complete recharacterization in accordance with GD1 would be

    undertakenpriortosoildischarge.Soilstockpilescanbemanagedinaccordance