OpenGeoRock
5.6

Notation and glossary

Describes OGR Slip2D 0.1.235

The documentation uses a single notation from the first chapter to the last. Below, the symbols are grouped by subject with their meanings and units, and a glossary defines the slope-stability and program terms used in the other pages. Where a symbol has two meanings in different chapters, both are given.

5.6.1Conventions#

  • Units. SI throughout: lengths in m, forces in kN per metre of slope (the analysis is two-dimensional, in plane strain), stresses and pressures in kPa, unit weights in kN/m³, angles in degrees. The program stores and computes in these units whatever unit system its window displays.
  • Axes. xx grows to the right and yy upwards; a slope fails from left to right when the ground falls to the right.
  • Effective quantities carry a prime: c′c', ϕ′\phi', σn′\sigma'_n.
  • Slices are numbered i=1…ni = 1 \dots n; a symbol with the index ii belongs to slice ii, and vectors are set in bold (Wi\mathbf{W}_i).
  • A dash (—) in the unit column marks a dimensionless quantity.

5.6.2Symbols#

Slices, forces and the factor of safety#

Table 5.6.1 Symbols of the method of slices.
SymbolMeaningUnit
FFfactor of safety—
Ff, FmF_f,\ F_mfactor of safety from force equilibrium and from moment equilibrium—
F0F_0factor of safety of Janbu's simplified method, before the correction—
f0f_0Janbu's correction factor, f0=1+b1[d/L−1.4 (d/L)2]f_0 = 1 + b_1\left[d/L - 1.4\,(d/L)^2\right]—
b1b_1coefficient of f0f_0 for the type of soil: 0.69 cohesion only, 0.31 friction only, 0.50 both—
d, Ld,\ Llargest perpendicular distance from the chord to the slip surface, and length of the chord joining the two ends of the surfacem
n, in,\ inumber of slices; index of a slice—
WWweight of the slice (vertical load on it)kN/m
bbwidth of the slicem
lllength of the base of the slice, l=bsec⁡αl = b\sec\alpham
α\alphainclination of the base of the slice°
β\betainclination of the ground surface above the slice (for the reliability index, see Table 5.6.4)°
RRradius of a circular slip surfacem
N, N′N,\ N'total and effective normal force on the basekN/m
S, SmS,\ S_mavailable and mobilised shear force on the base, Sm=S/FS_m = S/FkN/m
UUpore-water force on the base, U=u lU = u\,lkN/m
E, XE,\ Xinterslice normal and shear forceskN/m
Z, θZ,\ \thetainterslice resultant and its inclination (for the volumetric water content, see Table 5.6.2)kN/m, °
λ\lambdascale factor of the interslice force function, X=λf(x) EX = \lambda f(x)\,E—
f(x)f(x)interslice force function (f≡1f \equiv 1 in Spencer's method)—
ttposition along the slip surface, normalised from 0 at one end to 1 at the other, at which ff is evaluated—
mαm_\alphadenominator of the base normal force in Bishop's method, mα=cos⁡α+sin⁡αtan⁡ϕ′/Fm_\alpha = \cos\alpha + \sin\alpha\tan\phi'/F—
nαn_\alphathe same in Janbu's methods, nα=mαcos⁡αn_\alpha = m_\alpha\cos\alpha—
HHnet external horizontal force on a slice, positive in the sense of sliding (for the total head, see Table 5.6.2)kN/m
TTsupport forcekN/m
kh, kvk_h,\ k_vhorizontal and vertical seismic coefficients; kvk_v positive downwards—
ε\varepsilonconvergence tolerance—
σn, σn′\sigma_n,\ \sigma'_ntotal and effective normal stress on the basekPa
τ, τf, τm\tau,\ \tau_f,\ \tau_mshear stress; shear strength; mobilised shear stress, τm=τf/F\tau_m = \tau_f/FkPa
σt\sigma_ttensile strength allowed at a slice basekPa

Water, pore pressure and seepage#

Table 5.6.2 Symbols of pore pressure, groundwater and unsaturated soil.
SymbolMeaningUnit
uupore pressure (at the middle of the base of a slice)kPa
γw\gamma_wunit weight of water (9.81 by default)kN/m³
hhvertical distance from a point up to the water table or piezometric line of its materialm
HuH_upore-pressure coefficient of a water surface, u=γwHuhu = \gamma_w H_u h; 1 by default, cos⁡2\cos^2 of the inclination of the water surface with Auto HuH_u—
rur_upore-pressure ratio, u=ru σvu = r_u\,\sigma_v, with σv\sigma_v the vertical stress over the point: its depth below the ground surface times the unit weight of its material, plus any water ponded above; external loads are not included—
Bˉ\bar{B}Skempton's coefficient for the pore pressure of an undrained change of vertical stress, Δu=Bˉ Δσv\Delta u = \bar{B}\,\Delta\sigma_v—
HHtotal head, H=y+PH = y + Pm
PPpressure head, P=u/γwP = u/\gamma_wm
ψ\psisuction, positive where the pore pressure is negative: suction head or matric suction, according to the permeability modelm or kPa
ksk_ssaturated hydraulic conductivity (permeability)m/s
krk_rrelative hydraulic conductivity of the unsaturated soil, k=krksk = k_r k_s—
θ\thetavolumetric water content, in the seepage equations—
ϕb\phi^bangle of the increase of shear strength with matric suction (phi_b in the program)°
AEV\mathrm{AEV}air-entry value: matric suction up to which the soil is treated as saturated, the suction acting through ϕ′\phi'; the suction above it adds a cohesion (ψ−AEV)tan⁡ϕb(\psi - \mathrm{AEV})\tan\phi^bkPa

Strength models#

Table 5.6.3 Symbols of the strength models.
SymbolMeaningUnit
c′, ϕ′c',\ \phi'effective cohesion and effective friction anglekPa, °
cu (su)c_u\ (s_u)undrained shear strengthkPa
γ, γsat\gamma,\ \gamma_{sat}unit weight, and saturated unit weight used below the water surface when the material asks for itkN/m³
σv′\sigma'_veffective vertical stresskPa
σci\sigma_{ci}uniaxial compressive strength of the intact rockkPa
GSI\mathrm{GSI}Geological Strength Index of the rock mass—
mim_iHoek–Brown constant of the intact rock—
DDdisturbance factor of the rock mass—
mb, s, am_b,\ s,\ aHoek–Brown constants of the rock mass: mb=mi e(GSI−100)/(28−14D)m_b = m_i\,e^{(\mathrm{GSI}-100)/(28-14D)}, s=e(GSI−100)/(9−3D)s = e^{(\mathrm{GSI}-100)/(9-3D)}, a=12+16(e−GSI/15−e−20/3)a = \tfrac12 + \tfrac16\left(e^{-\mathrm{GSI}/15} - e^{-20/3}\right)—
mmconstant of the classic Hoek–Brown criterion (with ss)—
JRC\mathrm{JRC}joint roughness coefficient—
JCS\mathrm{JCS}joint wall compressive strengthkPa
ϕr\phi_rresidual friction angle of a joint°
A, S, m, OCRA,\ S,\ m,\ \mathrm{OCR}SHANSEP constant term, strength ratio, exponent and overconsolidation ratio: su=A+σv′ S OCRms_u = A + \sigma'_v\,S\,\mathrm{OCR}^m, with a lower bound—
KKvertical stress ratio: τf=K σv′\tau_f = K\,\sigma'_v, with a minimum strength—

Seismic, probabilistic and design symbols#

Table 5.6.4 Symbols of seismic, probabilistic and partial-factor analysis.
SymbolMeaningUnit
KyK_ycritical (yield) seismic coefficient: the khk_h that brings FF down to its target value, 1 by default—
PF\mathrm{PF}probability of failure: fraction of the samples with F<1F < 1—
β\betareliability index, β=(μF−1)/σF\beta = (\mu_F - 1)/\sigma_F for a normal distribution of FF, or computed from ln⁡F\ln F for a lognormal one—
μF, σF\mu_F,\ \sigma_Fmean and standard deviation of the sampled factors of safety—
γG, γQ\gamma_G,\ \gamma_Qpartial factors on permanent and on variable actions—
γc′, γϕ′\gamma_{c'},\ \gamma_{\phi'}partial factors on the effective cohesion and on tan⁡ϕ′\tan\phi'—
γcu\gamma_{cu}partial factor on the undrained shear strength—
γγ\gamma_{\gamma}partial factor on the unit weight—
γR;e\gamma_{R;e}partial resistance factor of a slope (earth resistance)—
γτ\gamma_{\tau}factor that OGR Slip2D applies to the strength of models that cannot be split into c′c' and tan⁡ϕ′\tan\phi'; EN 1997-1 does not define it—

5.6.3Glossary#

Table 5.6.5 Terms used in this documentation.
TermDefinition
Active supportA support whose force reduces the driving force; it is not divided by the factor of safety.
Admissibility checkA check made after the factor of safety of a surface has converged (tensile stress, m-alpha) that can reject the surface.
Agent bridgeThe local connection through which an MCP server works on the model open in the program window.
Back analysisThe calculation of the horizontal support force needed to reach a target factor of safety.
Block Search objectA window, line, point or polyline from which the Block Search takes the vertices of non-circular trial surfaces.
Critical surfaceThe admissible slip surface with the lowest factor of safety among those analysed (with the lowest KyK_y in a seismic coefficient analysis).
Design approachA combination of partial factors of Eurocode 7: DA1 combinations 1 and 2, DA2 and DA3.
Drawdown lineThe lowered water level of a rapid-drawdown analysis.
Effective stressTotal stress minus pore pressure; the stress that governs the drained strength of a soil.
External boundaryThe closed polygon that outlines the whole soil or rock mass of a model.
Factor of safetyThe number by which the shear strength must be divided for the sliding mass to be just in equilibrium.
Failure directionThe direction in which the mass slides: left to right when the ground falls to the right.
Focus objectA window, line, point or tangent that restricts the trial surfaces a search considers, before they are evaluated.
Hydraulic conductivityThe ratio between the flow per unit area and the hydraulic gradient (Darcy); also called permeability in this documentation.
Interslice forceThe force exerted between two neighbouring slices, with a normal component EE and a shear component XX.
Limit equilibriumThe state in which the shear strength divided by the factor of safety just balances the forces that drive the sliding mass.
Line of thrustThe line through the points of application of the interslice resultants.
Material boundaryAn open polyline, from edge to edge of the external boundary, that divides the mass into regions; a closed one inside the mass is a lens.
Matric suctionPore-air pressure minus pore-water pressure; in the program, the negative pore pressure of an unsaturated zone, taken as positive.
Method of slicesThe division of a sliding mass into vertical slices whose equilibrium is written one by one.
Mobilised shear strengthThe shear strength divided by the factor of safety: the part of it needed for equilibrium.
Newmark displacementThe permanent displacement of a rigid block sliding on the slip surface, the double integral of the part of an acceleration record above the critical acceleration.
Over-design factorWhat the analysis reports when partial factors are applied to its inputs: it must exceed 1, and it is not a factor of safety.
Partial factorA factor that divides a strength, or multiplies an action, in a design to a standard.
Passive supportA support whose force is added to the resisting force, and so is divided by the factor of safety.
Phreatic surfaceThe surface at which the pore pressure is zero (atmospheric); in a section, the water table.
Piezometric lineA line whose height above a point gives the pore pressure there, u=γwHuhu = \gamma_w H_u h, for the materials assigned to it.
Pore pressureThe pressure of the water in the pores of the ground.
Probability of failureThe fraction of the Monte Carlo or Latin hypercube samples whose factor of safety is below 1.
Pseudo-static analysisA representation of earthquake loading by constant forces proportional to the static weight, khWk_h W and kvWk_v W.
Rapid drawdownA lowering of the water level against a slope faster than the soil can drain, so that its pore pressures do not follow the new level.
RegionAn area of the model bounded by the external and material boundaries and filled by one material; regions are computed, not drawn.
Reliability indexThe number of standard deviations that separate the mean factor of safety from 1.
Seepage faceThe part of the boundary where water leaves the ground at atmospheric pressure; its extent is part of the solution.
Sensitivity analysisThe factor of safety of the critical surface recomputed as one input runs through its range, the others held at their mean values.
SliceA vertical strip of the sliding mass, narrow enough for its base to be treated as straight.
Slip surfaceThe surface along which the mass is assumed to slide: a circle, or a polyline for a non-circular surface.
Slope limitsThe stretch of ground surface within which a trial surface must start and end.
Stale resultA result computed on a model that has changed since.
Tension crackA vertical crack at the crest, with no tensile strength, that may hold water.
Transient analysisA groundwater analysis in stages over time, with a factor of safety for each stage that asks for one.
Water tableThe line of the phreatic surface; below it, u=γwHuhu = \gamma_w H_u h for the materials assigned to it.
Weak layerA polyline with a strength of its own, along which a non-circular slip surface can travel instead of crossing it.

The sources of the methods and models named on this page are listed in Section 5.7; the theory behind each symbol is in chapter 3, starting with Section 3.1.