LIU Fei-yu, ZHANG Tao, SHI Jing
China Journal of Highway and Transport. 2017, 30(5): 38-43.
Aiming at the paucity of research on the effect of cyclic shear on shear behavior of reinforced soil interface, a series of cyclic direct shear tests of Sandwich reinforced soil were performed by a large-scale direct shear device. The effect of shear rate, thickness of thin sand layer, cyclic shear amplitude and vertical stress on the cyclic shear behavior of Sandwich reinforced soil was investigated by Geogrid, Fujian standard sand and remolded clay with 28% water ratio, when the vertical stresses were 30, 60 and 90 kPa respectively and the shear displacement amplitudes were 3, 6 and 9 mm respectively with shear rates of 1, 2, 5 and 10 mm·min-1 respectively as well as the thickness of thin sand layer being 4, 6,8, 10, 12 and 14 mm respectively. The results show that when the thickness of thin sand layer increases from 2 mm to 14 mm, the peak shear stress on soil-geogrid interface increases from 54.3 kPa to 67.9 kPa and then decreases to 59.4 kPa. When the thickness of thin sand layer is 8mm, the peak shear stress on soil-geogrid interface reaches a maximum value, namely, 67.9 kPa. When the shear rate is 1 mm·min-1, soil-geogrid interface mainly shows the shear hardening. The increase amplitude of the peak shear stress is large in the first few cycle numbers and gradually decreases with the increase of cycle number. When the shear rate is more than 1 mm·min-1, the shear softening phenomena begin to appear on soil-geogrid interface and the more obvious the phenomena become, the higher the shear rate is. With shear amplitude increasing from 3 mm to 9 mm, the alternation of shear dilatation and contraction becomes more and more obvious and the final value of shear contraction increases with the increase of shear amplitude. When the vertical stresses are 30, 60, 90 and 120 kPa, the corresponding peak shear stresses on soil-geogrid interface are 32.6, 43.2, 60.4 and 82.9 kPa respectively, which show that the peak shear stress on soil-geogrid interface increases with the increase of vertical stress.