apuntes correcciones spt

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    Load

    Relative Density of Sand, D r 0 0.2 0.4 0.6 0.8 1.0

    A. General Shear

    B. Local Shear

    C. Punching Shear

    S e t

    t l e m e n

    t

    Load

    S e t

    t l e m e n

    t

    Load

    S e t

    t l e m e n

    t

    Ultimate Load

    DepthSurface

    0

    1

    2

    3

    4

    5

    R e l a t

    i v e

    D e p

    t h o

    f F o u n

    d a t

    i o n

    D / B

    ^

    Test at Greater

    Test

    Modes of Failure of Model Footings in Chattahoochee

    General

    Local Shear

    Shear

    PunchingShear

    B^ = B for a Square or Circular Footing.

    B^ = 2BL/(B+L) for a Rectangular Footing.

    Modes of Bearing Capacity Failure (76) Sand (20,76)

    A dapted from Vesic (197 3) JSMFD, ASCE, 99(SMI)

    Very loose Very Dense

    140

    Loose Medium Dense

    0

    10

    20

    30

    40

    50

    60

    130

    120

    100

    90

    80

    70

    60

    50

    40

    30

    20

    10

    0

    N

    N r

    N q

    S t a n

    d a r

    d P e n e t r a

    t i o n

    R e s

    i s t a n c e

    N ,

    b l o w s /

    f t

    B e a r i n g

    C a p a c

    i t y

    F a c

    t o r s ,

    N r

    a n d N

    q110

    28 30 32 34 36 38 40 42 44

    Angle of Internal Friction, , degrees

    Curves showing the relationship between bearing-capacity factorsand , as determined by theory, and rough empirical relationshipbetween bearing capacity factors or and values of standard

    penetration resistance N.

    Adapted from Peck, Hanson & Thornburn (1974)

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    SPT N Value (Blows/30cm)0 20 40 60 80 100

    1

    0

    D r = 80%

    Dr = 40%

    2

    3

    v o ( k g

    / c m

    2 )

    Gibbs & Holtz (1957)Peck & Bazaraa (1969)Marcuson & Bieganousky (1976)

    Schultze & Melzer (1965)

    V e r

    t i c a

    l S t r e s s ,

    Fig. 47. Empirical correlations between standard penetrationresistance and relative density for cohesionless soils.

    Adapted from Ladd et al. (1977) 9 th ICFMFE

    N, Blows/Foot

    0 40 80 120 160 200

    DR

    DR /

    0

    2

    4

    6

    8

    = 100 %(Gibbs and Holtz)

    Points omitted in thisarea

    = 100 %(Bazaraa)

    E f f e c

    t i v e

    O v e r

    b u r d e n

    P r e s s u r e ,

    K i p s

    S q u a r e

    F o o

    t

    10

    Dry Cohesionless Soil

    Submerged CoarseCohesionless Soil

    Results of Standard Penetration Tests for Very Dense SandsAdapted from Peck & Bazarra (1969)

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    45

    40

    A n g

    l e o

    f I n t e r n a l

    F r i c t

    i o n

    ` ( D e g r e e s

    )

    35

    30

    25

    20

    R e l a t i v e D e

    n s i t y1 0 0 %

    i n t h i s ra nge

    a n d

    0

    2 5 %

    5 0 %

    7 5 %

    ( )

    ` Obtained from effectivestress failure envelopesapproximate correlation

    is for cohesionlessmaterials without

    plastic fines

    MLSM

    SP

    SWGP

    GW

    Angle of Internal Friction Vs Density For Coarse Grained Soils

    Material Type

    75 80 90 100 110 120 130 140 150

    Dry Unit Weight ( D

    ), PCF(G = 2.68)

    1.2 1.1 1.0 0.9 0.8 0.75 0.7 0.65 0.6 0.55 0.5 0.45 0.4 0.35 0.3 0.25 0.2 0.15

    Void Ratio, e

    0.55 0.5 0.45 0.4 0.35 0.3 0.25 0.2 0.15

    Porosity, n

    Correlations Of Strength Characteristics For Granular Soils

    Adapted from NAVFAC DM-7.1 (5/82) p 7.1 - 149

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