Cover Page

SOIL PROPERTIES AND THEIR CORRELATIONS

 

SECOND EDITION

Michael Carter

Geotechnical Consultant (Retired), UK

Stephen P. Bentley

Cardiff University, UK

 

 

 

 

 

 

 

 

 

logo.gif

Preface

The aims of this book are to provide a summary and discussion of commonly used soil engineering properties and to give correlations of various engineering properties.

The book includes:

  • a compendium of published correlations;
  • discussions of the reliability, accuracy and usefulness of the various correlations;
  • practical advice on how soil properties are used in the assessment and design of geotechnical problems, including basic concepts, and limitations on their use that need to be considered; and
  • descriptions of the measurement of soil properties, and how results are affected by the method of measurement and the expertise of technicians carrying out the testing.

A consideration in describing the various properties has been an awareness by the authors that many geotechnical engineers and engineering geologists have little, if any, hands‐on experience of laboratory testing, and are often unaware of the procedures used to obtain the various soil properties and of the effects of poor or inappropriate practice.

The properties are also described in relation to their use in geotechnical analysis, in a way that we hope will give students and younger engineers an in‐depth appreciation of the appropriate use of each property and the pitfalls to avoid, and should also provide a useful reminder to more experienced professionals.

Many soil correlations were established in the early decades of soil mechanics, with there being no need to repeat the work once correlations had been established and verified by sufficient researchers. As a consequence, the correlations given in this book span a wide range of time, a few as far back as the 1930s, but we have also presented more recent work where this adds useful information. However, our intention in selecting correlations is to present those that will be of wide practical application, and the book is not intended as a research review. To aid their use in spreadsheet calculations, we have derived mathematical expressions to fit many of the correlations that were originally given only graphically. We have also tried to keep the work independent of national design codes, but it inevitably contains references to practices that are more prevalent in the English‐speaking world. Where references are made to classification systems and associated codes we have, where possible, included references to both UK and US practice.

We envisage and recommend that correlations be used in two ways: firstly, to obtain values of a property that has not been measured; and secondly, to provide additional values where some direct measurements of the property have been made. In the first case, where no values of a particular property have been directly measured, the values obtained from correlations should be viewed with caution and treated as preliminary, especially where the property value is critical to the predicted performance of a design. Where correlations are used in combination with direct measurements to provide supplementary values, the accuracy and reliability of the correlations can usually be verified, fine‐tuning the correlation if necessary, which may allow the values obtained by correlation to be viewed with more confidence.

While every care has been taken in the preparation of this book, with the very large amount of information that has been assembled it is possible that some errors have occurred; users should satisfy themselves that the information presented is correct. The authors can take no responsibility for consequences resulting from any errors in the book. The views expressed about the reliability and accuracy of correlations, typical values and other published information are based on the authors’ own experience and may not accord with those of other geotechnical specialists.

Acknowledgements

In creating a compendium of published correlations, we had to seek permission from many authors around the globe; for her role in this important and painstaking task, the authors would like to thank Carol Clark. Bringing together such a large number of disparate items of information from many sources also involved a great deal of checking, and our thanks go to ex‐colleagues Jason Williams and Max Lundie for their checking of some of the work, and especially to Mark Campbell who read through the entire script, noting errors and giving many helpful suggestions.

List of Symbols

SymbolName of variableTypical units (SI)*
αA scaling factor for estimating footing settlements from plate bearing test results.D
αA factor for estimating values of coefficient of volume compressibility from static cone test results.D
αAdhesion factor, for pile calculations.D
αA factor used to estimate the pull‐out resistance of a soil reinforcement grid.D
ΔpA distance above or below the A‐line on a standard plasticity chart.%
θAngle of a plane, from the direction of maximum principle stress, on which stresses act.Degrees
μViscosity of permeant for general seepage calculations.kN.s/m2
νPoisson's ratio.D
πRatio of the circumference of a circle to its diameter (≈3.14159).D
ρSettlement.m, mm
σDirect stress.kPa (kN/m2)
σ'Effective direct stress.kPa (kN/m2)
σ1, σ2, σ3Maximum, intermediate and minimum principal stresses.kPa (kN/m2)
σnEffective earth pressure, used in soil nail calculations.kPa (kN/m2)
σv, σ'vVertical stress, or overburden pressure, in total and effective stress terms, respectively.kPa (kN/m2)
τShear stress.kPa (kN/m2)
γBulk density of soil.kN/m3
γdDry density of soil.kN/m3
γdmaxMaximum dry density, for relative density calculations.kN/m3
γdminMinimum dry density, for relative density calculations.kN/m3
γpDensity of permeant for general seepage equation.kN/m4
γsubSubmerged density of soil.kN/m3
γwDensity of water.kN/m3
ϕAngle of shearing resistance (general, or in total stress terms).Degrees
ϕ'Effective stress angle of shearing resistance.Degrees
ϕdDrained angle of shearing resistance.Degrees
ϕrResidual angle of shearing resistance (general).Degrees
aAir voids content of soil.%
aComponent of influence factor Ic for estimating settlements of footings on sands.D
AArea (nominal) of soil water flow.m2
AA correction factor for rod energy ratio in the standard penetration test.D
APercentage passing a 2.4 mm sieve, used in the calculation of suitability index.%
AA constant used in the estimation of swelling potential from plasticity index.D
AcActivity value (of a clay).D
ApEnd area of penetration cone in a 1standard penetration test.mm2
AsEnd area of penetration cone in a dynamic probe.mm2
avCoefficient of compressibility. (See also mv, coefficient of volume compressibility.)m2/MN
bComponent of influence factor Ic for estimating settlements of footings on sands.D
BFooting width.m
BA constant used in the estimation of swelling potential from plasticity index.D
cShape factor in general seepage calculations.D
cCohesion.kPa (kN/m2)
CPercentage finer than 0.002 mm, used in the calculation of activity for a clay.D
c'Effective stress cohesion.kPa (kN/m2)
C1Constant used in Hazen's formula to estimate the coefficient of permeability.D
CBRCalifornia Bearing Ratio.%
CcCoefficient of curvature (coefficient of grading).D
Cc, CrCompression index, recompression index, respectively.D
cdDrained cohesion.kPa (kN/m2)
CIConsistency index.%
CNCorrection factor for overburden pressure, applied to SPT N‐values.D
cuUndrained cohesion, shear strength.kPa (kN/m2)
CuCoefficient of uniformity.D
cvCoefficient of consolidation.cm2/s, m2/year
CαSecondary compression index.(log10 time)–1
Cαε , C'Modified secondary compression index (sometimes referred to simply as the secondary compression index).(log10 time)–1
dMaximum length of drainage path in consolidation calculations.m
DDepth of foundation (when calculating allowable bearing pressures on sands).m
D10The 10% particle size, also called the effective size.mm (or μm)
D30, D60The 30% and 60% particle sizes, respectively.mm (or μm)
DnThe particle size at which n% of the material is finer. See also D10, D30, D60.mm (or μm)
DrRelative density (of granular soils).D
DsAn effective particle size for permeability estimates, usually taken as D10.mm
eVoids ratio.D
eThe natural number, approximately 2.718.D
EYoung's modulus (also called the elastic modulus).kPa, MPa
e1, e2Initial and final voids ratios in consolidation testing.D
EdDeformation modulus (also called the constrained modulus).kPa, MPa
emaxMaximum voids ratio, for relative density calculations.D
eminMinimum voids ratio, for relative density calculations.D
ERrRod energy ratio in standard penetration test.D
FThe percentage passing the 75 μm sieve, used in the calculation of AASHTO classification group index.%
fl, fs, ftShape, layer thicknes and time factors, respectively, for estimating settlements of footings on sands.D
FpDrop distance of monkey (falling hammer) in a dynamic probe.mm
FsDrop distance of monkey (falling hammer) in a standard penetration test.mm
GShear modulus.kPa, MPa
GsSpecific gravity of soil solidsD
hThickness of specimen in consolidation testing.mm
HThickness of a compressible layer in consolidation testing.m
iHydraulic gradient in soil water flow.D
IcInfluence factor for estimation of settlements of footings on sands.D
IrRigidity index, used in rate‐of‐settlement estimates based on static piezocone test results.D
IrSwell index, used in the estimation of swelling pressure.D
kCoefficient of permeability.m/s, m/year
KA constant used in the estimation of swelling potential from plasticity index.D
K0Coefficient of earth pressure at rest.D
KdDepth factor for allowable bearing pressures on sands.D
KsEarth pressure coefficient use in driven pile calculations.D
LFooting length.m
LILiquidity index.%
LLLiquid limit.%
mMoisture (water) content of soil.%
MpMass of monkey (falling hammer) in a dynamic probe.kg
MsMass of monkey (falling hammer) in a standard penetration test.kg
mvCoefficient of volume compressibility. (See also av, coefficient of compressibility.)m2/MN
nPorosity of soil.D
nA factor used to estimate undrained shear strength from consistency index or liquidity index.D
NSPT N‐value; blows of standard hammer to drive the SPT sampler or cone 300 mm.Blows
N1SPT N‐value corrected for overburden pressure.Blows
N1(60)SPT N‐value corrected for overburden pressure and to a rod energy ratio of 60%.Blows
N60SPT N‐value corrected for rod energy ratio, ERr. (the “60” refers to standardisation to 60% rod energy.)Blows
NcorrectedSPT N‐value corrected for silts and fine sands below the groundwater table.Blows
NkA factor used in the estimation of undrained shear strength from static cone tip resistance.D
O40, O80Pore diameters at which 40% and 80% of the pores are finermm, μm
OCROverconsolidation ratio.D
pPrevious maximum overburden pressure, used in estimating settlements of footings on sands.D
p1, p2Initial and final pressures used in a stage of consolidation testing.kPa (kN/m2)
PIPlasticity index.%
PLPlastic limit.%
PMPlasticity modulus.%
PpPenetration for each blow count in a dynamic probe.mm
PsPenetration for each blow count in a standard penetration test.mm
qQuantity of flow of water through soil per unit time.m3/s, m3/year
qBearing pressure.kPa (kN/m2)
qaAllowable bearing pressure.MPa (MN/m2)
qcMeasured cone resistance (pressure) in static cone tests.kPa (kN/m2)
quUltimate bearing capacity.kPa (kN/m2)
RComponent of influence factor ft for estimating settlements of footings on sands.D
SDegree of saturation.%
SSwelling potential.%
s, suUndrained shear strength.kPa (kN/m2)
StSensitivityD
SLShrinkage limit.%
tTime, used in calculations or rates of consolidation and secondary compression.s, years
t1, t2Start and end times for secondary compression calculations.s, years
TvBasic time factor, used in calculations or rates of consolidation.D
uPore water pressure.kPa (kN/m2)
UDegree of consolidation.D
vNominal velocity of flow of water through soil.m/s, m/year
vtTrue velocity of flow of water through soil.m/s, m/year
WLWWeighted liquid limit, used in the estimation of swelling potential.%
WwWeight of water (in the model soil sample).g
YRate of frost heave.mm/day

* D = dimensionless; % values are also essentially dimensionless.

List of Property Values and Correlations in the Tables and Figures

image
image
image