In Singapore, two thirds o f the land area is underlain by residual soils. One distinct characteristic o f residual soils is its unsaturated nature. The relationships o f shear modulus and damping ratio with shear strain for residual soils may differ from transported soils and have not been fully investigated. This study aims to investigate shear stiffness and damping ratio properties o f residual soils under cyclic simple shear loading in both saturated and unsaturated conditions.To date, there is no standard for cyclic simple shear test. Two commercial NGI-type cyclic simple shear apparatuses were evaluated using a "standard" sand, Ottawa 20-30. The evaluation revealed that there was a rocking movement on the top platen experienced by both apparatuses. As a result o f rocking, the shear modulus below shear strain o f 0.03% was much lower than that reported in the literature, and thus a cut-off shear strain for the cyclic simple shear apparatuses was suggested to be 0.03%. For a stiffer sand specimen tested, the rocking became more significant, resulting in lower shear modulus at shear strains ranging from 0.03% to 0.1%. A correction factor based on actual horizontal displacement ratio, Rδ , was proposed to correct the shear modulus. In addition, the evaluation also found that there was friction load and friction energy in the cyclic simple shear apparatuses. The friction load was corrected for shear modulus determination following the suggestion by ASTM D6528-07 (2007). A detailed correction procedure on friction energy was described for damping ratio determination. If the friction energy was left uncorrected, the damping ratio o f the soil with shear strain will not follow an orderly trend.Unsaturated soil specimens for cyclic simple shear tests were prepared using the pressure plate apparatus. To eliminate uncertainty with regards to the equilibrium matric suction, the equilibrium time o f soil specimens in the pressure plate test was investigated. Independent matric suction measurement using a high suction tensiometer was performed during the equilibrium process. Corrected rates o f gravimetric water content change o f 0.15 %/day and o f 0.08 %/day were suggested vi