geotechnic (consoliadation)

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  • 8/20/2019 Geotechnic (Consoliadation)

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    CONSOLIDATION

    TEST

    MOHD AMRI BIN RAMZICF 140081

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    Consolidation Settlement

    • It occurs due to te !rocess o" te consolidation#

    • Cla$ and Or%anic soil are most !rone to consolidation

    settlement#• Consolidation is te !rocess o" reduction in &olume

    due to lost o" 'ater under an increased load#

    • It is a time related !rocess occurrin% in saturated soil($ drainin% 'ater "rom &oid#

    • It is o"ten con"used 'it Com!action#

    • Consolidation teor$ is re)uired to !redict (ot rateand ma%nitude o" settlement#

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    *at is Consolidation+

    • *en a saturated soil is loaded e,ternall$- te'ater is s)uee.ed out o" te soil and te soilsrin/s#

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    Conce!t o" Consolidation

    • As te time !asses- te 'ater comes out o" tesoil &oid and so te &olume o" soil decreases- tisis cause o" te settlement#

    The decrease in volume of soil = The volume of

    squeezed out water

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    Settlement due to

    consolidation

    • Settlement is te &erticall$ do'n'ard mo&ement

    o" structure due to te srin/a%e in &olume o" soildue to consolidation

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    Settlementoid ratio

    Relation• 2)uatin% te t'o e,!ression "or a&era%e &ertical

    strain-

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    Settlement &s# 3ime•  3is leads to settlement occurrin% o&er a lon% time-

    'ic could (e se&eral $ears- de!endin% u!on te!ermea(ilit$ o" te soil

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    Oedometer test

    • 3e soil caracteristics durin% onedimensionalconsolidation or s'ellin% can (e determined ($te oedometer test#

    •An oedometer test measures asoil5s consolidation !ro!erties#

    •Oedometer tests are !er"ormed ($ a!!l$in%di6erent loads to a soil sam!le  and measurin%

    te de"ormation res!onse#• 3e results "rom tese tests are used to !redicto' a soil in te 7eld 'ill de"orm in res!onse to acan%e in e6ecti&e stress#

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    Conce!t

    • Oedometer tests are desi%ned to simulate te onedimensional de"ormation and draina%e conditions tat soilse,!erience in te 7eld#

    •  3o simulate tese conditions- ri%id con7nin% rin%s are usedto !re&ent lateral dis!lacement o" te soil sam!le#

    • :orous stones are !laced on te to! and (ottom o" tesam!le to allo' draina%e in te &ertical direction#

    •  3o (etter simulate onedimensional strain- a diameterto

    ei%t ratio in te sam!le o" ;

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    M23HOD 3O D232RMIN2 3H2 CO2FFICI2N3

    OF CONSO=IDA3ION

    •  3ere are t'o metods "or determinin% te coe>cient

    o" consolidationcient o" consolidation can (e determined ($tis e)uation-

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     3a$lor metod

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    Casa%rande metod

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     32S3 :ROC2D9R2

    1#Measure te internal diameter ?D@ and te ei%t o" te rin%- usin%

    internal &ernier cali!ers#E#*ei%t te rin% to te nearest 0#01% ?mR@#;#Cuttin% te s!ecimen and trimmin% into rin%#4#Determine te initial moisture content "rom trimmin% soil##Determine te 'ei%t o" rin% and s!ecimen ?m1@

    #Determine te mass o" (ul/ s!ecimen ?m@ to te nearest 0#01%usin% tis e)uationm G m1  mR

    •. 

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     32S3 :ROC2D9R2

    #:lace te consolidation rin% and s!ecimen ?cuttin%ed%e u!!ermost@ centrall$ on te !orous disc#8#Fit te rin% retainer and cell (od$ and ten !lace

    te u!!er !orous disc centrall$ on to! o" tes!ecimen#

    #:lace te consolidation cell centrall$ in !osition onte !lat"orm o" te macine (ase#

    10#=i"t te end o" te (eam to allo' te loadin% $o/eto (e raised to te &ertical !osition and adJust te

    loadin% stem ($ scre'in% it do'n'ards until teend en%a%es closel$ in te recess on te to! o" teloadin% ca!

    11#Attac te com!ression dial %au%e to te arm onte su!!ort !ost#

    1E#Add 'ei%t ?E# /%@ care"ull$ to te load an%er

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     32S3 :ROC2D9R2

    1;#Add 'ater at room tem!erature to te celland ma/e sure tat te s!ecimen and u!!er!orous disc are com!letel$ su(mer%ed#

    14#*ind do'n te (eam su!!ort and at tesame time start te cloc/#

    1#O(ser&e te com!ression %au%e readin%sand te cloc/- and record te readin%s on aconsolidation test "orm at te selected time

    inter&als#1#:lot te readin%s o" te com!ression a%ainst

    time to a lo%aritmic scale and a%ainsts)uareroottime#

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    SI=3 C=AK R2S9=32LAM:=2

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    SI=3 C=AK R2S9=32LAM:=2

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    Conclusion

    • Consolidation is a !rocess 'ic soil decrease

    in &olume#

    • Occurs 'en stress is a!!lied to a soil tatcause te soil !article to !ac/ to%eter moreti%tl$- tere"ore reducin% its (ul/ &olume#

    • Oedometer is one o" te e)ui!ment tat use"or determinin% te consolidation !arameters