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Laboratory Testing of Fatigue Crack Growth in Geosynthetically ...

Laboratory Testing of Fatigue Crack Growth in Geosynthetically ...

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924 Andrzej Pożarycki and Tomasz Garbowski / Procedia Eng<strong>in</strong>eer<strong>in</strong>g 57 ( 2013 ) 922 – 928To determ<strong>in</strong>e the elastic parameters <strong>of</strong> the section, the homogenization method described <strong>in</strong> [18, 20] is used here. Due tothe negligible stiffness <strong>of</strong> geocomposites, the calculation was carried out only for the geogrid (Table 1a). The geometry <strong>of</strong>the sample was prepared similar to the size <strong>of</strong> A4 format.Table 2 Results <strong>of</strong> macroscopic geometry measurements GG8550The rema<strong>in</strong><strong>in</strong>g parameters needed to determ<strong>in</strong>e the characteristics <strong>of</strong> theequivalent layer are calculated from the formulas:Width <strong>of</strong> rib, mma1a21.5 1.5Grid size, mmb1b225 25Thickness <strong>of</strong> ribg1g21.5 1.5Distance between ribs, mma1 + b1 a1 + b126.5 26.5ua1= u =( a + b )1 21 1a ⋅g ⋅ ( a + b )1 1 1 1, p 1= p2=( a1+ b1) ⋅ ( a1+ b1) ⋅2g1, p1+ p2 + pm+ pp= 1(1)where: u 1= u2, p 1= p2- respectively percentage <strong>of</strong> the ribs area <strong>in</strong> the width and length <strong>of</strong> the grid and their volumefraction <strong>in</strong> the grid structure,p p content <strong>of</strong> space unfilled by the matrix,p m part <strong>of</strong> matrix <strong>in</strong> total volume <strong>of</strong> grid,Consider<strong>in</strong>g the model <strong>of</strong> geogrid, which uses the values <strong>of</strong> geometrical measurements and the parameters declared bythe manufacturer (gathered <strong>in</strong> Table 1) a secant modulus was calculated by Equation (2):Fm1E = ⋅u g ⋅εwhere:F m maximum tensile force kN/m,u i part <strong>of</strong> the material <strong>in</strong> the strip <strong>of</strong> the grid mm/mmg i thickness <strong>of</strong> the rib <strong>in</strong> the „i th ” direction mm,є m grid elongation at break mm/mm.i i m=11 778 MPa (2)F<strong>in</strong>ally, us<strong>in</strong>g the method which converts the basic features <strong>of</strong> the geogrids, from the real model to its surrogate, anequivalent E K modulus and Poisson’s ratio <strong>of</strong> HMA composite with re<strong>in</strong>forcement can be calculated [18].2 2 2mm−ν− ν2κ+ pmE[2(1 −ν−2 ν ) κ + 3 p (7 −8 ν) κ+ 45 p ]EK( E, ν, pm, κ ) =12(1 2 ) 45[MPa]where:E AC stiffness, MPa;E k Composite stiffness (AC + Geogrid), MPa;E zi Geogrid stiffness along “i” direction;2(1−ν−2 ν ) κ+ 15ν⋅p E Eνk( ν, pm, κ ) = , κ = p + p4(1 −ν−2 ν2) κ+ 15 pm z1 z21 2m E E, (3)

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