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    Soil SettlementBy

    Kamal Tawfiq, Ph.D., P.E., F.ASCE

    Fall 2010

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    Soil Settlement:Total Soil Settlement = Elati! Settlement " Conoli#ation Settlement

    Stotal= Se" S!

    $oa# Ty%e &'i(i#) Fle*i+le

    Elati! Settlement o- mme#iate Settlement #e%en# on

    Settlement $o!ation &Cente- o- Co-ne-

    / Theo-y of Elati!ity

    Elati! Settlement

    Time De%en#e# Elati! Settlement &S!hme-tman a-tman etho# &1345/By: Kamal Tawfiq, Ph.D., P.E.

    Elati! ettlement o!!6- in an#y, ilty, an# !layey oil.

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    Elati! Settlement

    Se= &1 > ?2

    2

    &!o-ne- of the fle*i+le fo6n#ation

    Se= &1 > ?2

    &!ente- of the fle*i+le fo6n#ation

    By: Kamal Tawfiq, Ph.D., P.E.

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    By: Kamal Tawfiq, Ph.D., P.E.

    .0

    2.

    2.0

    1.

    1.0

    L / B

    .02 5 4 1031

    ,av,r

    ??a8

    ?-

    Fo- !i-!6la- fo6n#ation? = 1?a8= 0.5

    ?-= 0.55

    9al6e of ?, ?a8, an# ?-

    Bqo &1 > ?

    ESe =

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    By: Kamal Tawfiq, Ph.D., P.E.

    Elastic Settlement of o!ndation on Sat!rated Clay

    Gan+6, BHe--6m, an# KHae-nli &13 %-o%oe# an eq6ation fo- e8al6ation of thea8e-a(e elati! ettlement of fle*i+le fo6n#ation on at6-ate# !lay oil &PoionI-atio, >= 0.. 'efe--in( to Fi(6-e 1 fo- notation, thi eq6ation !an +e w-itten a

    Se= A1A2qoBE

    whe-e A1i a f6n!tion B an# $B, an# i a f6n!tion of D fB.Ch-itian an# Ca--ie- &1345 ha8e mo#ifie# the 8al6e of A1an# A2to ome e*tent, an# thee a-e%-eente# in Fi(6-e 2.

    1.0

    0.5

    0.3

    0

    DfB

    20110

    A2

    L/B =

    Sq6a-e

    L/B = 10

    Ci-!le

    2

    2.0

    1.

    010

    0.

    1.0

    10.1 100 1000

    H /B

    A1

    9al6e of A1 an# A2 fo- elati! ettlement !al!6lation &afte- Ch-itian an# Ca--ie-, 1345

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    Elastic Settlement "sin# t$e Strain %nfl!ence actor: @S!hme-tman a-tman etho# &1345J

    E*am%le:B x L

    EsDf Iz

    De%th,

    q= L Df&'1

    q

    &'2

    &'

    &'

    s3

    Is3

    A8e-a(e A8e-a(e E

    The 8a-iation of the t-ain infl6en!e fa!to- with #e%th+elow the fo6n#ation i hown in Fi(6-e 1.ote that, fo- q6a-e o- !i-!6la- fo6n#ation,

    = 0.1 at = 0= 0. at = 0.B

    = 0 at = 2B

    Simila-ly, fo- fo6n#ation with $B M 10

    = 0.2 at = 0= 0. at = B= 0 at = B

    Se = C1C2& q q N & E ;

    whe-e= t-ain infl6en!e fa!to-C1= a !o--e!tion fa!to- fo- the #e%th of fo6n#ation em+e#ment

    = 1 0. @q &q qJ

    C2= a !o--e!tion fa!to- to a!!o6nt fo- !-ee% in oil = 1 " 0.2 lo( &time in yea- 0.1q = t-e at the le8el of the fo6n#ationq = o8e-+6-#en %-e6-e = L Df

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    Elati! Pa-amete- of 9a-io6 Soil

    Oo6n(I o#6l6, E

    Ty%e of Soil Bm2 $+Bin2 PoionI 'atio,

    $ooe an# 10.C 2.1 1,00 C,00 0.20 0.0e#i6m #ene an# 14.2 24.0 2,00 ,000 0.2 0.0Dene an# C.0 .20 ,000 5,000 0.C0 0.Silty an# 10.C 14.2 1,00 2,00 0.20 0.0San# an# -a8el 3.00 142.0 10,0002,000 0.1 0.CSoft !lay 2.04 .15 C00 40e#i6m !lay .15 10.C 40 1,00 0.20 0.0Stiff !lay 10.C 2.1 1,00 C,00

    E&QBm2 = 4E= 2q!

    whe-e = tan#a-# %enet-ation n6m+e-q!= tati! !one %enet-ation -eitan!e

    ote: Any !onitent et of 6nit !an +e 6e#

    The Oo6n(I mo#6l6 of no-mally !onolia#ate# !lay !an +e etimate# a

    E= 20! to 00!

    Fo- o8e-!onoli#ate# !lay

    E= 40! to 1000!

    whe-e ! = 6n#-aine# !oheion of !layey oil

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    E*am%le:

    2

    12,000 20,000

    De%th, &m

    5

    ,000

    B x L = 3 m x 3m

    Es (k/m!"1.# m

    q = 1$0 k/m!

    %&'al

    0.!

    2 1.

    Iz= 0.5

    0.)

    00.1 0.$

    %*+a-+

    Iz

    = 14.5 Qm

    De%th &m R &m E&Q:Bm2 A8e-a(e &BE. K &mBQ:

    0 1 1 5,000 0.2 0.231 * 10

    1.0 1. 0. 10,000 0. 0.214 * 10

    1. 2. 10,000 0.F1 0.30 * 10

    .0 F 2 1F,000 0.111 0.13 * 10

    = 1.0 * 10

    C1= 1 0. &q B q q

    = 1 0. @ 14.F5 * 1. B 1F0 &14.5 * 1.J

    C2= 1 " 0.2 lo( &B0.1 = 1.

    en!e

    S! = C1. C2&q q &BE K

    = &0.3&1.@1F0&14.5*1.J&1.*10

    = 23.2*10m 2.3 mm

    0

    2B

    Tim+ = # y+as

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    ! !2

    St-ee# Rone

    Conoli#ation Settlement

    Conoli#ation Settlement &P-ima-y Conoli#ation = S!= &C!1"eo !. lo( @&Po" PPoJ

    #ei(n= Col6mn $oa#

    OverburdenPressure

    o

    By: Kamal Tawfiq, Ph.D., P.E.

    San#

    San#

    aly

    B

    *

    *

    StressDistribution

    o-mallyConoli#ate#Clay

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    2

    1

    p

    p

    Hsand

    Hclay

    /2 Hclay

    Cc

    Log PPo

    Void Ratio

    Log P

    P

    Void Ratio

    Po Po + P

    Cc H log po+pSultimate= H =Po1 + eo

    ( )

    Log P

    P

    Void Ratio

    Po Po +

    P

    2

    1

    p

    Hsand

    Hclay

    /2 Hclay

    Loading Unloading

    Po= sand Hsand+ ( clay! "ate#) Hclay/2

    $o#mallyConsolidated Soil

    Clay

    Sand

    Sand

    eo

    By: Kamal Tawfiq, Ph.D., P.E.

    Consolidation Settlement

    Sand

    Sand

    Sand

    Sand

    =CS H

    1 + eO P0

    Po + Plog( )

    % %

    % %

    %%

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    Cs H PcSultimate= H =Po 1 + eo

    ( ) logCc H

    +1 + eo

    logPc

    ( )Po + P2

    Log P

    P

    Void Ratio

    Po Po + P=Pc

    2

    1

    p2

    p2

    Hsand

    Hclay

    /2 Hclay

    2

    1

    p

    Hsand

    Hclay/2 Hclay

    Log P

    Void Ratio

    Po Pc

    P2

    Cs

    Cs

    Po + P2

    %&e soil 'ecomeoe#consolidated

    soil

    eo

    Re loading"it& Heay Load

    By: Kamal Tawfiq, Ph.D., P.E.

    %%

    %2

    %2%2

    %%

    = log ( ) +CS H

    1 + eO

    PCPo

    C C H

    1 + eO PC

    Po + Plog( )

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    Cs H PcSultimate= H =Po

    ( )1 + eo

    log

    Log P

    P

    Void Ratio

    Po Pc

    2

    1

    p2

    p2

    H sand

    Hclay/2 H clay

    2

    1

    p

    H sand

    H clay/2 H clay

    Log P

    Void Ratio

    Po Pc

    P 2

    C s

    Po + P2%&e soil 'ecomeoe#consolidated

    soil

    eo

    Re loading"it& lig&t Load

    By: Kamal Tawfiq, Ph.D., P.E.

    %

    %2%2

    %2

    %2

    = logCS H

    1 + eO Po

    Po + P ( )2

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    Log P

    Void Ratio

    CR = Pc/PoCR = 1CR * 1CR *

    o-mally Conoli#ate#

    ea8ily 8e- Conoli#ate#

    8e- Conoli#ate#

    Pc

    ,ete#mining %&e P#econsolidation P#essu#e (Pc)

    1

    -

    2

    .

    By: Kamal Tawfiq, Ph.D., P.E.

    Po

    0

    Caa(-an#e -a%hi!al etho#

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    #ei(n= Col6mn $oa#

    "o

    *++2P+ss+

    =Ex&+ss P+ 4a'+ P+ss+

    =Ex&+ss P+ 4a'+ P+ss+

    o

    Hdr = Hc

    5'+ss Dis'i'i2!: 1 m+'h

    6!= $aye- Thi!Qne

    By: Kamal Tawfiq, Ph.D., P.E.

    Rate o Consolidation

    Settlement at any time = Stime

    Stime= Sultimate U3 S6ltimate= &C!1"eo !. lo( @&Po" PPoJ

    U3 = (%)

    %= (c)

    %=(Hd#)

    2

    c t

    San#

    San#

    Caly

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    Rate o Consolidation

    Settlement at any time = Stime

    Stime= Sultimate U3

    U3 = (%)

    %=

    %= %ime 4acto#

    t = time (mont&5 day5 o# yea#)(H

    d#)2= ,#ainage Pat&

    Hd#= H o# H/2

    %= (c)

    (Hd#)2

    c t

    C= Coeicient o Consolidation

    Cv is obtained from laboratory testing

    Clay

    Sand

    Sand

    Clay

    Roc6

    Sand

    %"o "ay d#ainageHd#= Hclay/2

    ne "ay d#ainageHd#= Hclay

    From Tables

    By: Kamal Tawfiq, Ph.D., P.E.