Characteristics of the development of collapse in loess soils with time. 1F, 1T, 7R

Characteristics of the development of collapse in loess soils with time. 1F, 1T, 7R

170A Shear deformation characteristics pressure during compression of water-saturated peat. In Russian. 3R. ARKHANGEL .LESOTEKHN. INST .TRUDY,V37,19...

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170A

Shear deformation characteristics

pressure during compression of water-saturated peat. In Russian. 3R. ARKHANGEL .LESOTEKHN. INST .TRUDY,V37,1973 ,P27-33.

See also abstract: 1856. 17o6 CORNET,FH Analysis of the deformation of saturated porous rocks in comlression. Report. Figs,Tabls,Refs. MISSOL~I RIVER DIV. CORPS ENGIN~S,OMAHA, MRD-4-75, JULY 1975,290P • An investigation of the mechanical influence of interstitial fluids on the deformation process of saturated rocks has been conducted to determine the domain of validity of l~eviously published theories. Equilibrium equations for fluid saturated materials in whlch the fluid is at rest or flows according to Dsrcy's law were derived. For this purpose s a new characterization of porosity has beau proposed for analyzing porosity variations within a rock nmss. In view of the results obtained, three effective stress theories for the analysis of elastic deformation in saturated rocks are discussed. 17o7

CHAPPEd, BA

MAUNSEI~ GEOTECH. SERV .Mk~~OURNE, AUS

The effects of constraints on the deformational response of slip along planar Joints. IOF,IIR. INT .J .ROCK MECH.MIN. SC I. GEOMECH .ABSTR. ,V12, N9, SEPT. 1975,P265- 270.

1708 RABINoVICH, IG URINOV, MI Characteristics of the development of collapse in loess soils with time.IF,iT,TR. SOIL MECH.FOUND.~GNG,Vll, NS, SEPT-OCT .1974, P331-333.

Granular materials and influence of interlocking 1709 SHANDOR,W SURKOV, YA CH~KASOV, II Influence of adsorbed gases and water on the interactions between the grains of loose soils.4F,iT,4R. SOIL MECH .FOUND.~GNG, VII, NS, S~f-OCT. 1974, PB20-324.

Time-dependent behavior 1710 SINGH,DP BANARAS HINDU UNIV.VARANASI, IND A study of creep of rocks. 7F,1BR. INT. J .ROCK MECH .M~N.SC I. GEOMECH .ABSTR., V12, N9, SEPT. 1975,P271-276 •

Compressibility,swelling and consolidation 1711 BONDAR~KO, NF K O V A L ~ , NP KHUDIAKOV, AD Calculating the non-linear consolidation process in peat bearing ground using digital computers. In Russian. 5R. ARKHANGEL. L E S O T ~ . INST. TRUDY, V37,1973, PI2 -17. 1712 MORARESKUL, NN BRONIN,VN SOKOLOV, VD Experimental studies of the process of chsnge in pore

1713 SELMHR.OLSEN, R ROKOENG~, K About swelling tests and stability of clay zones in hard rock. Conference. IIF,TR. PROC .THIRD CONGRESS, INT.SOC .ROCK MECH. ,DENVER, 1974, V2, PART B, 197~, PI061-I068. 1714 MUSTAFAEV,AA CHIGNIEV, GD NAZ IROVA, GR Rheological nature of the deformations caused by swelling in cls~s and by collapse in loess soils. 4F,1T,14R. SOIL MECH. FOUND. ~GNG, Vll, N5, S~I~T-OCT .1974, P325 -330. It is demonstrated that the swelling deformations caused by collapse are related not only to surface phe~omema in the pore spaces of the soll but also to complex physicochemical processes which occur inside the crystal structure of the mineral particles of these soils.

Experimental and numerical techniques. 1715 WORONOW, A UN IV. HOUSTON, TEXAS, USA A new technique for determining the preferred failure angle of brittle rock. 9F,6R. INT. J .ROCK MECH.MIN. SC I. GEOMECH.ABSTR., V12, N9, SEPT. 1975,P289-293. 1716 BURMAN ,BC HOLLINGSWORTH 3SYDNEYIAUS Development of a numerical model for discontlnua. 15F,34R. AUST. GEOMECH. J. V64, N1,1974, P13 - 22. Numerical s1~11atlon of dlscontinua is achieved through development of the finite element technique. The essential feature of the method is the reco@~ition of the ms4or importance of interblock displacement while intrablock deformations are treated as second order affects. The mechanics of a jointed medium is related to rigid body displacements of adjacent block centroids through rectilinear elements which simulate normal s ~ tangential compliance of the units. Full account is taken of nonlinear interactions between blocks. Normal interaction between blocks allows for limited tensile strength, locking in both compressional and rotational modes, and unstable hinge formation. 1717 LAVROV, IV ROMANCHUK, VE SNORODINOV,MI Use of radioisotope methods for investigation of submarine deposits .2F,IR. SOIL MECH .FOUND. ENGNG, Vll, N5, SEPT-OCT. 1974, P33h-338.

Classification and identification 1718 GALAI, BF Correlations between plasticity indices of clays.14R. SOIL MECH. FOUND. ~GNG,VII, N4, JULY-AUG. 1974, P257- 258.