SOIL MECHANICS - CHAPTER 32 pot

SOIL MECHANICS - CHAPTER 32 pot

SOIL MECHANICS - CHAPTER 32 pot

... Arnold Verruijt, Soil Mechanics : 32. LATERAL STRESSES IN SOILS 178 32. 3 Elastic material A possible approach to the behavior of soils is to consider it as an elastic material. ... elasticity. Arnold Verruijt, Soil Mechanics : 32. LATERAL STRESSES IN SOILS 179 In some older publications equation (32. 18) has been proposed as a generally applicable relation for soil and rock. Tha...

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SOIL MECHANICS - CHAPTER 12 pot

SOIL MECHANICS - CHAPTER 12 pot

... at small stress. The branch of soil mechanics studying these relations is critical state soil mechanics. It may be interesting to mention that during cyclic loads soils usually tend to contract ... normal force can only be a compres- sive force. Tension can not be transmitted, unless the soil particles are glued together. Such soils do exist (e.g. calcareous soils near the coast of...

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SOIL MECHANICS - CHAPTER 13 potx

SOIL MECHANICS - CHAPTER 13 potx

... 0. 13.3 A non-linear material In the previous chapter it has been argued that soils are non-linear and non-elastic. Furthermore, soils are often not isotropic, because during the formation of soil deposits ... Verruijt, Soil Mechanics : 13. TANGENT-MODULI 82 ε zz = − 1 E [σ zz − ν(σ xx + σ y y )]. The minus sign has again been introduced to account for the sign convention for the stre...

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SOIL MECHANICS - CHAPTER 14 pot

SOIL MECHANICS - CHAPTER 14 pot

... semi-logarithmic paper on the basis of the common logarithm. The formula then is ε = − 1 C 10 log( σ σ 1 ). (14.5) Typ e of soil C C 10 sand 5 0-5 00 2 0-2 00 silt 2 5-1 25 1 0-5 0 clay 1 0-1 00 4-4 0 peat ... be determined for a particular soil, in the lab oratory. The circumstance that there are two forms of the formula, with a factor 2.3 between the Arnold Verruijt, Soil...

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Soil mechanics - Chapter 16 pot

Soil mechanics - Chapter 16 pot

... TO N:Z=K/N:P=0:C =-1 :J=0 180 J=J+1:C=-C:JJ=2*J-1:JT=JJ*JJ*PP*TT 190 P=P+(A*C/JJ)*COS(JJ*PI*Z/2)*EXP(-JT) 200 IF JT<20 THEN GOTO 180 210 PRINT " z/h = ";Z;" - p/po = ";P 220 ... measuring the pore pressures, and then waiting Arnold Verruijt, Soil Mechanics : 16. ANALYTICAL SOLUTION 99 100 CLS:PRINT "One-dimensional Consolidation" 110 PRINT "Anal...

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Soil mechanics - Chapter 19 pot

Soil mechanics - Chapter 19 pot

... on Terzaghi’s logarithmic compression formula, see Chapter 14. It can be considered that the deformation considered in that chapter (for sand soils) is a special case of the more general case ... prepared by the application of a sand layer on a soft soil layer of 7.6 m thickness, it has b e en found from tests on the soft soil that the de- formation after one day is 1.1 %, and after 1...

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SOIL MECHANICS - CHAPTER 22 potx

SOIL MECHANICS - CHAPTER 22 potx

... incremental stresses are taken equal to those in the field. For Arnold Verruijt, Soil Mechanics : 22. SHEAR TEST 132 the mechanism of a toppling book row is produced, just as a row of bo oks in ... horizontal stress and the vertical stress can both be measured accurately. It may be mentioned that in soil mechanics practice laboratory tests can sometimes be considered as scale tests of...

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SOIL MECHANICS - CHAPTER 34 pot

SOIL MECHANICS - CHAPTER 34 pot

... (34.13) The equations of equilibrium in x- and z-direction now are Q − T sin θ − N cosθ = 0, (34.14) W −N sin θ + T cos θ = 0. (34.15) Arnold Verruijt, Soil Mechanics : 34. COULOMB 193 After elimination ... Arnold Verruijt, Soil Mechanics : 34. COULOMB 192 away from the soil. During that deformation the lateral force will decrease. Eventually ... graphical and numerical methods have...

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SOIL MECHANICS - CHAPTER 36 potx

SOIL MECHANICS - CHAPTER 36 potx

... Z>1 THEN F=F-KP*(Z-1) 270 Q=-KA*Z*Z/2:IF Z>A THEN Q=Q+T 280 IF Z>1 THEN Q=Q+KP*(Z-1)*(Z-1)/2 290 M=-KA*Z*Z*Z/6:IF Z>A THEN M=M+T*(Z-A) 300 IF Z>1 THEN M=M+KP*(Z-1)*(Z-1)*(Z-1)/6 310 ... TRZ=TRZ+G*DZ:PR=PR+W*DZ:SRZ=TRZ-PR:SRX=CA*SRZ:TRX=SRX+PR 260 F(I)=TRX-TLX:FF=(F(I)+F(I-1))*DZ2:Q(I)=Q(I-1)-FF 270 M(I)=M(I-1)+(Q(I)+Q(I-1))*DZ2:MT=MT+FF*(Z-DA-DZ2):NEXT I 280 WHILE MT>0:N=N+1...

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SOIL MECHANICS - CHAPTER 37 pot

SOIL MECHANICS - CHAPTER 37 pot

... applies to saturated soil, with the groundwater level coinciding with the soil surface. Derive a similar equation for homogeneous dry soil. Then compute the value of d/h for dry soil, with γ = 16 ... C=8*(KSA/KSP)*(1+D)^5/(20*(1+D)^ 2-1 5*D-12*D*D) 180 IF C<0 THEN PRINT "No solution":END 190 C=C^(1/3):E=ABS(C-D):D=C:IF E>0.000001 THEN 170 200 PRINT USING A$;"d/h =...

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