The complete or partial penetration of soil by piles is one of the effective methods of building on swelling soils, which are widespread in Povolzh'ye, Kazakhstan, Siberia, Crimea, and Zakavkaz'ye where many lightly loaded agricultural buildings are raised on them (1). The interaction between piles and swelling soils is distinguished by characteristic peculiarities. When a frozen swelling soil rises, the pile is displaced upward, and when wetted, its strength characteristics and the bearing capacity of the piles are diminished. The length of the piles should, in conformity with standards (2), be assigned proceeding from conditions whereby the bearing capacity is guaranteed and their uplift does not exceed the allowable value for the structure. The first condition is verified by computing the bearing capacity with allowance for the reduction in the resistance of the swelling soil against the lateral surface. The soil's coefficient of strength reduction is set equal to 0.5 for all conditions, although in our opinion, it should be differentiated as a function of the type of soil and the pile structures. It is expedient to compute the bearing capacity on the basis of allowable pile settlements with allowance for slump-type settlements of the swelling soil. A method of calculating pile uplift, where the effect of the type of swelling soil and pile length is defined more precisely, is cited in (2) for evaluation of the second condition. According to E. A. Sorochan, V. S. Sazhin et al., the shape and geometric dimensions of the pile's section, the type of pile (precast, or cast-in-place), etc. exert a major influence on pile uplift. Moreover, the method used to calculate pile uplift in (2) is based on correlation relationships, and is therefore limited by the framework of experimental field investigations. It is impossible to extrapolate for short piles, which are most effective in agricultural construction. The author therefore proposes an original method for calculating pile uplift in swelling soils, which is based on differential equations of the theory of thermoelasticity. To determine pile uplift, let us examine the case when a pile cuts completely through a layer of swelling soil (see Fig. 1 ). For its incomplete penetration, the total uplift h o is the sum of the uplift h e of the soil layer beneath the end of the pile, and the uplift h due to frictional forces along its lateral surface. The latter are determined just as in the first case.
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