“…In this method, a bulk sample of soil, road dust, or other media is separated into its constituent particle size fractions (that is, G-analysis [97]), and then, for each G-fraction, a sequential extraction of HM chemical fractions (F-analysis) is carried out. Due to the laboriousness and complexity of interpretation of the obtained results, this approach is used not so often and is mainly devoted to the study of agricultural [98] and roadside soils [99], road dust [55,57,100], bottom sediments [101], and atmospheric aerosols [102,103]. For example, in six particle size fractions of road dust (<63 µm, 63-125 µm, 125-250 µm, 250-500 µm, 500-1000 µm, 1000-2000 µm) in the Palolo Valley, Hawaii, USA, the distribution of sequentially extracted by the BCR method acid-soluble, reducible, oxidizable, and residual fractions of Al, Zn, Pb, and Cu were analyzed [84], that is, 6G × 4F = 24 GF-fractions of each element were studied.…”