A Method for Calculating Matrix Suction of Homogeneous Foundation under Back Peak Rainwater Infiltration
A matrix suction and foundation technology, applied in the field of calculation of unsaturated foundation matrix suction, can solve problems that cannot be solved by matrix suction, and achieve the effect of simple calculation process
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Embodiment 1
[0033] The calculation model of the present invention is as figure 2 shown. Based on the unsaturated seepage governing equation, the analytical solution of the transient unsaturated permeability coefficient and matrix suction of the homogeneous foundation with groundwater in the deep and peak rainwater infiltration after encountering the surface is obtained through Laplace transform. The magnitude of matrix suction provides a convenient and quick calculation method, and the steps of the method are as follows.
[0034] (1) Determine the initial matrix suction distribution state of the foundation: for a homogeneous foundation with groundwater in the deep, A The matrix suction distribution corresponding to the stable seepage field formed by infiltration is taken as the initial state of the foundation, and the corresponding matrix suction calculation formula is:
[0035]
[0036] Where: h m,0 is the initial matric suction at z, in cm; β is the desaturation coefficient, in c...
Embodiment 2
[0052] The following engineering case is used to further illustrate a method for calculating the suction force of the homogeneous foundation matrix under the post-peak rainwater infiltration effect announced by the present invention:
[0053] For an unsaturated homogeneous foundation, the distance l between the groundwater level and the surface is 5m, and the physical and mechanical parameters of the soil are as follows: saturated permeability coefficient k s is 0.36cm / h, desaturation coefficient β is 0.00165 / cm, water storage capacity (θ s -θ r ) is 0.27cm 3 / cm 3 , residual water content θ r 0.20cm 3 / cm 3 . There was no rainfall in the previous period, and the rain intensity in the previous period was q A 0cm / h; later encountered heavy rain with a total rainfall of 48mm, and the rainfall lasted for 12h. In the later stage of rainfall, the rain intensity variation coefficient a was 0.05cm / h 2 , the initial rain intensity q 0 It is 0.1cm / h.
[0054] Based on the abo...
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