In previous major earthquakes, the damage and collapse of structures located in lique ed eld which caused by site failure a common occurrence, and the problem of evaluation and disscusion on site liquefaction and the seismic stability is still a key topic in geotechnical earthquake engineering. To study the in uence of the presence of structure on the seismic stability of lique able sites, a series of shaking table tests on lique able free eld and non-free eld with the same soil sample was carried out. It can be summarized from experimental results as following. The natural frequency of non-free eld is larger and the damping ratio is smaller than that of free eld. For the weak seismic loading condition, the dynamic response of sites show similar rules and trend. For the strong ground motion condition, soils in both experiments all lique ed obviously and the depth of liquefaction soil in the free eld is signi cantly greater than that in the non-free eld, besides, porewater pressure in the non-free eld accumulated relately slow and the dissapited quikly from analysis of porewater pressure ratios(PPRs) in both experiments. The amplitudes of lateral displacements and acceleration of soil in the non-free eld is obviously smaller than that in the free eld caused by the effect of presence of the structure. In a word, the presence of structures will lead to the increase of site stiffness, site more di cult to liquefy, and the seismic stability of the non-free site is higher than that of the free site due to soil-structure interaction.