The main objective of this research was to contribute to the evaluation of the influence of the grain shape on the hydraulic conductivity (k) of sands. For that, laboratory tests were carried out on a sample from Ipanema Beach sand (D10 = 0.28 mm, D30 = 0.34 mm, D50 = 0.41 mm, D60 = 0.45 mm, CNU = 1.61 e CC = 0.92), composed by sub-rounded to rounded grains (sphericity = 0.65 and roundness = 0.70), and on a sample of glass microspheres, Drop-On II A type (sphericity = 0.95 and roundness = 0.95), prepared with the same grain size distribution of the sand. The experimental program comprised: (a) cleaning and processing of the samples; (b) microscopic analysis to evaluate the grain shape; (c) grain-size analysis by sieving; (d) reconstitution of the grain-size distribution of the glass microspheres sample; (e) glass microspheres specific gravity (Gs); (f) maximum void ratio tests, by method B of ABNT (2020), and minimum and intermediate void ratio tests, by MSP method of Miura and Toki (1982); and (g) constant head permeability tests in rigid-wall permeameter and in flexible-wall permeameter. For both samples, it was experimentally verified the validity of the linear relationship between the hydraulic conductivity (k) and e (3)/(1+e), being e the void ratio, in agreement with the theoretical formulations proposed by Kozeny-Carman (1927) and by Taylor (1948). For a given void ratio, it was observed that the hydraulic conductivity of the glass microsphere sample is higher than that of the sample from Ipanema Beach sand.