COEM 6012 Coursework#2_2015

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  • 7/23/2019 COEM 6012 Coursework#2_2015

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    Derek Gay 2015-09-16 COEM 6012 Coursework #2

    COEM 6012 CONSTRUCTION GEOTECHNICS

    Coursework #2 2015-09-16

    1. Develop a computer solution (Excel, MATLAB, Fortran95, C/C++, or other) to implement the numerical

    finite difference solution for the 1D consolidation of a compressible soil layer 12 m thick subjected to a

    uniform surface loading of 100 kN/m2over its depth (site fill). The computer solution must be capable of

    modelling both doubly and singly drained layers. In this algorithm the value of R must be a variable, where

    R = cv*t/z2

    cv= coefficient of consolidation, m2/month

    z = depth increment length (m)

    t = time step in months = (R*z2/cv)

    For this problem, assume a single uniform layer, with a uniformly distributed stress change with depth, where

    cv= 0.15 m2/month and R = 0.5.

    (i)

    Create a 1D finite difference grid, for z = 3.0, 2.0, 1.0, 0.5 m. For each grid spacing

    determine t calculate and compute and plot pore pressures vs depth at times, t = 8, 16, 32, 64,128 months for a doubly and singly drained soil [to do this you must first determine the

    number of time-steps to be executed in each case, using the stability condition at R=0.5]. In

    the numerical solution the number of time-steps would not yield the exact times indicated.

    Round the number of steps up.

    (ii) Using Equation 1.18 (Consolidation notes) determine the theoretical pore pressure distributions

    over depth, for the actual times (rounded up) and compare these to the numerical solutions;

    calculating the % error at each node point. Change the value of R = 0.505 and comment on the

    stability and accuracy of the solution for part (i).

    (iii) For z = 0.5 m determine the average degree of consolidation U%over the full depth of the

    layer, at the times t = 4, 8, 16, 32, 64, 128, 256 months using the area approximation method

    (Trapezoidal Rule) and plot the graphs of Time Factor vs U% Consolidation, for both the

    double and single drainage conditions. Using Equation 1.21 (Consolidation notes 2015)

    determine the theoretical %U and Time Factor values and compare these to the numerically

    computed values.

    (iv) For z = 0.5 m and for both the double and single drainage conditions, determine the average

    degree of consolidation U%over a depth of 3.5 m at the times indicated in (iii) above using the

    area approximation method (Trapezoidal Rule). Plot the relationships of Time Factor vs U%

    Consolidation for this condition. Compare these relationships/graphs with those obtained in

    part (iii) above [where the U% Consolidation values were averaged over the full layer depth].

    (v) If the average mvfor the layer varies from, mv= 1.8 x 10-3

    m2/kN at the top and mv= 1.0 x

    10-3

    m2/kN at the bottom, plot thelog10(time) vs settlementcurves for conditions encountered

    in (iii) and (iv) above.

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    Derek Gay 2015-09-16 COEM 6012 Coursework #2

    2. (a) Develop a MATLAB, Python, Fortran95, C/C++, algorithm/script to determine the average stress

    distribution zand x, under the

    (i) centreline of an Embankment,

    (ii)

    centreline of a Tank foundation.The program must treat embankment height, width, side slopes, tank radius, loading and soil

    parameters as input variables.

    (b) Continue this algorithm to include the numerical solution of 1D consolidation. Using this algorithm,

    redo question (1) part (iv) using the non-linear mean stress distribution, (z+x)/2, at the centreline of

    both the (i) embankment (ii) tank. Use (i) the maximum embankment height is 6 m, = 21 kN/m3,

    embankment top width 10 m and a 1:3 side slopes and for (ii) tank radius = 5 m, filled with water to 10

    m.

    Submission Date: Qu.1 September 25

    th

    2015, 4:30 pmSubmission Date: Qu.2 October 1st2015, 4:30 pm

    Late Submissions would be penalised by 2.5%/day up to a maximum of 25% after which,

    submissions would attract an F