“…ISA was further extended to capture the influence of a larger number of consecutive cycles before reaching the critical state and thus reducing the strain or pore water pressure accumulation by Poblete et al [28]. This version of ISA has been incorporated in different works for sand comprising benchmark simulations [11,17,20,39], for clays without rate dependency [7,8] as well as incorporating the rate dependency of fine-grained soils [9,32,35]. On the other hand, IGS was improved by Wegener and Herle [38] to describe accumulation effects more realistically, and subsequently, a similar modification as proposed by Poblete et al [28] for ISA was incorporated into the IGS by Duque et al [3] to improve the simulations under larger number of repetitive cycles.…”