presentation 2007 lazar gheorghe 3409

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    SOIL LIQUEFACTION

    -Presentation-

    SPECIAL FOUNDATIONS

    Student:

    LAZAR Gheorghe

    Group 3409

    PROJECT ADVISOR:

    Assoc. Prof. Eng., Ph.D. Irina

    LUNGU

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    Liquefaction is a process in which the

    seismic shear waves cause an increase in

    the pore water pressure in a cohesionlesssoil stratum. This increase in pore pressure

    reduces the effective stress confining the

    soil. This reduction causes a reduction ofshear modulus of the soil, which in turn,

    results in increased soil deformation.

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    Key Elements of Soil Liquefaction

    Engineering

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    Ground failures associated to

    liquefaction

    1. Loss of bearing strengththe ground can liquefy and lose its ability to support structures.

    Fig. 1. Niigata -

    JapanThese tilted

    buildings and

    liquefaction in this

    area are probably

    the most well known

    examples of

    liquefaction and loss

    of bearing strength

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    2. Lateral spreading

    - the ground can slide down very gentle slopes or toward stream banks

    riding on a buried liquefied layer.

    Fig.2. Lateral-spreading

    induced failure of a dike in

    Nantou

    Fig.3. Lateral spreading and settlement of

    a concrete dike

    3 S d b il

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    3. Sand boils

    - sand-laden water can be ejected from a buried liquefied layer and erupt

    at the surface to form sand volcanoes; the surrounding ground often

    fractures and settles.

    Fig.5. Widespread sand boiling in

    Zhangbin Industrial Park

    Fig.4. Large scale sand boiling in

    Zhangbin Industrial Park, Zhanghua

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    4. Flowfailuresearth moves down steep slope with large displacement and

    much internal disruption of material.

    5. Groundoscillationthe surface layer, riding on a buried liquefied layer, is

    thrown back and forth by the shaking and can be severely deformed.

    6. Flotation

    light structures that are buried in the ground (like pipelines,sewers and nearly empty fuel tanks) can float to the surface when they are

    surrounded by liquefied soil.

    7 S ttl t

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    7. Settlement

    -when liquefied ground re-consolidates following an earthquake, the

    ground surface may settle or subside as shaking decreases and the

    underlying liquefied soil becomes more dense.

    Tilting of a resident building in Wufeng

    Settlement on a street of Nantou City

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    Ground improvement and structural solutions that are available to reduce hazard from liquefaction.General Category Mitigation Methods Notes

    I. Excavation and/or compactiona. Excavation and disposal of liquefiable soilsb. Excavation and recompactionc. Compaction (for new fil l)

    II. In-situ ground densification

    a. Compaction with vibratory probes (e.g.: Vibroflotation,

    Terraprobe, etc.)b. Dynamic consolidation (Heavy tamping)c. Compaction pilesd. Deep densification by blastinge. Compaction grouting

    Can be coupled with

    installation of gravel columns Can also provide

    reinforcement

    III. Selected other types of ground

    treatment

    a. Permeation groutingb. Jet groutingc. Deep mixingd. Drains

    o Gravel drainso Sand drainso Pre-fabricated strip drains

    e. Surcharge pre-loadingf. Structural fills

    Many drain installation

    processes also provide in-situ

    densification.

    IV. Berms, dikes, sea walls, and

    other edge containment

    structure/systemsa. Structures and/or earth structures built to provide edge

    containment and thus to prevent large lateral spreading.

    V. Deep foundations a. Piles (installed by driving or vibration)b. Piers (installed by drilling or excavation)

    Can also provide ground

    densification

    VI. Reinforced shallow foundations

    a. Grade beamsb. Reinforced matc. Well-reinforced and/or post-tensioned matd. "Rigid" raft

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    REFERENCES:

    i. Liquefaction, Flow, and Associated Ground Failure -T. Lesl ie Youd, United States Department of theInterior

    ii. Recent advances in soil liquefaction engineering: Aunified and consistent framework R.B. Seed, K .O.

    Cetin, R.E.S. Moss , A .M. Kammerer, J. Wu, J . M.Pestana, M. F. Riemer, R.B . Sanc io , J.D. Bray, R.E. Kayen, and A . Faris, 26th Annual ASCE Los

    Angeles Geotechnical Spring Semina,April 30,2003

    iii. http://geomaps.wr.usgs.gov/sfgeo/liquefaction/ iv. Seismic Design Criteria for soil liquefaction J.M.Ferri t to, NAVAL FACILITIES ENGINEERINGSERVICE CENTER June 1997

    v. Characteristics of liquefied sands during Mino-

    Owari, Tohnankai and Fukui Earthquakes

    HideakiKish ida

    http://geomaps.wr.usgs.gov/sfgeo/liquefaction/http://geomaps.wr.usgs.gov/sfgeo/liquefaction/