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Probabilistic Seismic Hazard Analysis (PSHA).pptx

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    Probabilistic Seismic

    Hazard Analysis(PSHA)

    Site/Building Specifc Spectral Analyses,

    Liqueaction Susceptibility and Deaggregation oRisk or Grenada

    By: Kevin M. Blache - 8!""""

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     Aim:

    #he $ltimate %oal o& this 'roect as to cona Probabilistic Seismic Hazard Analysis (PS

    &or *renada.

     As a res$lt o& this a series o& obectives %eared toards achievi'rescribed %oal ere created.

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    +bectives:#he obectives re,$ired ere as &ollos:

    • #o cond$ct a revie o& Seismicity and the res$ltanSeismic Hazard both on a *lobal scale and mores'ecically &or the /aribbean 0e%ion.

    • #o research and dene the methods o& assessin%Seismic Hazard and hence com'are methods.

    • #o ded$ce the method &or cond$ctin% a ProbabilisSeismic Hazard Analysis and 1ea%%re%ation o& Se0is2.

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    +bectives:#he obectives re,$ired ere as &ollos:

    • #o 'er&orm a Probabilistic Seismic Hazard Analysis and 1ea%%re%ation Analysis &or *re

    • #o com'are the res$lts o& the analyses cond$

    to similar analyses thro$%ho$t the re%ion.

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    Seismicity 3 Seismic Hazar

    •  An 4arth,$a2e is a s$dden violent sha2in% o& the %ro$&rom movements o& the 4arth5s cr$st. (6e 1ictionary/ivil 4n%ineerin%)

    • Seismicity re&ers to the occ$rrence or &re,$ency o&

    earth,$a2es in a re%ion.• #he %enesis o& seismic activity is the res$ltin% moveme

    the s$r&ace o& the 4arth ca$sed by convection c$rrentlocated beneath 4arth5s cr$st in the mantle.

    •  A seismic hazard in a /ivil 4n%ineerin% conte7t arisethe seismicity o& a re%ion 'oses a threat to citizens5 sa

    ell as '$blic and 'rivate 'ro'erty.

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    Seismicity 3 Seismic Hazar

    #y'es o& 4arth,$a2es

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    Seismicity in the /aribbean

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    Past St$dies on Seismicity in

    /aribbean• Pereira and *ay ("8) 9 Seismic Hazard Analysis (amaica 3 #

    • #aylor et al. ("8) 9 Seismic Hazard Analysis

    •  Ambeh (;) 9 4arth,$a2e Hazard in the /aribbean

    • #anner 3 She'herd (") 9 Seismic Hazard in

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    Seismic Hazard Analysis Metho1eterministic vs. Probabilistic

    1eterministic Analysis:=ses 'ast events to determine seismic ris2 in an e?ort to ens$re thatan event is realistic. @t ass$mes that all events are %overned by 'astevents.

    Probabilistic Anal@nvolves all deterministic events ith a nite 'robabilocc$rrence (all 'ossible events). @t also a''lies statistmethods to determine the seismic ris2.

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    Probabilistic Seismic Hazar Analysis Method

    irst 'ro'osed by /ornell (8).

    /om'osed o& ive (C) Ste's as 'resented by Kramer (and Ba2er (;>C).

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    Ste's &or Probabilistic Seismic Hazard Ana(PSHA)

    • @denti&y So$rce Dones &or 4arth,$a2es in an area. #h$s deteso$rce to site distances.

    • /ond$ct *$tenber%-0ichter

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    Statistical 3 Probability #heory @nvolved inProbabilistic Seismic Hazard Analysis Met

    • 1iscrete 3 /ontin$o$s0andom Eariables

    • Probability Mass 3 1ensity$nctions (PM 3 P1 )

    /$m$lative 1ensity $nctions(/1)

    • Probability 1istrib$tions(Poisson and 6ormal)

    • /onditional Probabilities

    • Total roba

    • B

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    Probabilistic Seismic Hazard Analysi#otal Probability #heorem

    #his can then be ada'ted to the analysis o& seismic haas &ollos:

    •  

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    *$tenber%-0ichter 0ec$rrence

    Ma%nit$de

    Ghere: is the rate o& earth,$a2es ith a ma%nit$de %reater than m occ$r

     and are constants estimated &rom re%ression analysis o& 'ast seismic data

    0ate o& e7ceedin% a %iven ma%nit$de:

     (/1)

    Probability o& a %iven ma%nit$de occ$rrin%

    •  

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    So$rce to Site 1istance

    Probability o& an earth,$a2e occ$rrin% at a %iven dist

    #he so$rce zone m$st be s$bdivided into smaller areaHence the 'robability is calc$lated as a ratio o& a smaarea to the total zonal area.

    •  

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    *ro$nd Motion Prediction 4,$at

    (*MP4) &or Ma%nit$de and 1istaSam'le *ro$nd Motion Prediction 4,$ation:

    Probability o& e7ceedin% a *ro$nd Motion %iven a 'artic$ma%nit$de and distance:

    Ghere: is the normal c$m$lative distrib$tion &$nction

     is the mean s'ectral acceleration (%) val$e

    is the standard deviation o& s'ectral acceleration (%) val$es

    •  

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    /ombination o& All 0ates an

    Probabilities

     Ann$al 0ate o& 47ceedance o& a *ro$nd Motion %iven both earth,$ma%nit$de and distance:

    •  

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    1ea%%re%ation 3 Bayes5

    #heoremBayes5 #heorem $ses conditional 'robability:•  

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    1ea%%re%ation 3 Bayes5

    #heoremGhen ada'ted to Probabilistic Seismic Hazard Assessment yi•  

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    Probabilistic Seismic Hazard Analysis &or *renada

     A''lyin% the a&orementioned ste's accordin% to the /orne(8) Method.

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    *renada

    $apital% St. *eor%e5sopulation% >>>>>

    aris!es%

    Sister &sles%/arriaco$ 3 Petite

    Martini,$e

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    Selection o&So$rce Dones

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    ShalloSo$rce Dones

    (>-"> 2m)

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    @ntermediate

    So$rceDones (">-

    !>> 2m)

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     Eerication o& So$rce Done

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     Eerication o& So$rce Done

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     Eerication o& So$rce Done

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     Eerication o& So$rce Done

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    *$tenber%-0ichter

    0elationshi's&or So$rce Dones

    -I

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    1iscrete P1 o&Ma%nit$des &or

    So$rce Dones -I

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    S$bdivision o& So$rce Done

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    *ro$nd Motion Prediction 4,$at(*MP4)

    Pea2 *ro$nd AccelerationP*A(%)

    • is described as the motionthat a 'article on the %ro$nd

    ill e7'erience.

    •Both are meas$red as $nits

    o& acceleration d$e to %ravity(%) mJs;

    • #y'ical accelerations: >.>C%to %

    • >.>>C% barely &elt >.>C%

    $n'leasant >.C% o$ld

    S'ectral Acceleration

    • is described as the motiob$ildin% a''ro7imately e7'

    • @t is modelled by a 'armassless vertical rod havin%

    nat$ral 'eriod o& vibrat

    • Hence is more $se&$l &ren%ineerin% st

    • Period o& vibration o& a str$>. times the n$mber

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    4nd 0es$lt o& ProbabilisticSeismic Hazard Analysis

    /ombination o& 0ates and Probabilities to com'leProbabilistic Seismic Hazard Analysis (PSHA)

    1ea%%re%ation o& Seismic 0is2

    A i S i t & /i il 4 i

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     American Society o& /ivil 4n%ineers AS/4 "->C

    Minim$m 1esi%n

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     American Society o& /ivil 4n%ineers AS/4 "->C

    Minim$m 1esi%n

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    /alc$lation o& 0et$rn Perio

    Ghere: is the 'robability o& a seismic event occ$rrin%in C> years)

     is the rate o& rec$rrence o& a seismic event

     is the ret$rn 'eriod &or a seismic event (;I"C years)

    •  

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    Hazard/$rve at

    >.; Seconds 

    Shos contrib$tiono& Dones

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    Hazard /$rveat .>

    Seconds

    Shos contrib$tion o&Dones

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    0es$lts &rom Hazard /$rve

    Spectral

     Acceleration

    $orresponding

    To Return

    eriod o '()*

     years

    +' Seconds -+ Secon

    >.> % >.> %

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    1ea%%re%ation o& Seismic 0is2 &or Dones 3>.; Seconds

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    1ea%%re%ation o& Seismic 0is2 &or Dones ! 3 I aSeconds

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    1ea%%re%ation o& Seismic 0is2 &or Dones ! 3.> Seconds

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    1ea%%re%ation o& Seismic 0is2 &or Dones ! 3.> Seconds

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    S$mmary o& 1ea%%re%ation0es$lts

    .one

    +' Seconds -+ Se

    Ma%nit$de 1istance(2m)

    Ma%nit$de

    (Shallo - 6orth o&

     Eenez$ela) I.C-C.> ;> C.>-C.C; (#oba%o) I.C-C.> >> C.>-C.C

    ! (4ast o& #rinidad) .>-.C ;>> .>-.C

    I (@ntermediate - 6orth o& Eenez$ela)

    I.C-C.> > C.>-C.C

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    0ecommendations

    • /ollect s$?icient stron% motion records &or/aribbean re%ion and develo' a *ro$nd MotPrediction 4,$ation s'ecic to the re%ion.

    • A''ly *ro$nd Motion Prediction 4,$ations &r

    re%ions aro$nd the Gorld ith a similar &a$ltty'e to the /aribbean.

    • /om'are res$lts o& the above recommendatio veri&y res$lts.

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    /oncl$sion

    • Probabilistic Seismic Hazard Analysis (PSHA) is an a''romethod &or assessin% seismic ris2.

    • 1ea%%re%ation o& 0is2 is also a''ro'riate since it yields ms'ecic res$lts as it re%ards the ma%nit$de and so$rce todistance associated ith the e7ceedance o& a s'ectral

    acceleration SA(%) as re,$ired by the AS/4 "->C.•  Altho$%h the /aribbean re%ion has a hi%h level o& seismic

    active the s'ectral acceleration e7'ected &or *renada isrelatively lo.

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    N$estionsO

    #han2 o$.