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- W2306770123 abstract "The grain size parameters (mean size, sorting, skwe ness, kurtosis, median and first percentile) could be used for the lithodynamic interpretation of fluvial envi ronment. Dependency between a particle size and a sedimentologic condition in the fluvial environment have been defi ned (Ruby, 1933; Hjulstrom, 1935; Morris, 1957; Poole, 1957; Aipoow, 1963; Passega, 1964; Sundborga, 1967; Royse, 1968; Braithwaite, 1973; Southard and Boguchwal; 1973, Baker 1974; Kaniecki, 1976; Miller et. al, 1977; Ko ster, 1978; Middelton and Southard, 1978; Baba and Komar, 1981; Froehlich, 1982; Costa, 1983; Williams, 1983; Eschner and Kichner, 1984; Mynarczyk, 1985; Maizels, 1989; O'Connor, 1993; Mazumder 1994; Le Roux 1977, 2002; Ferguson and Church 2004). Shear and settlement velocity could be calculated on the base of the grain size. Sediment trend analysis will be used to the change of a grain size composition during erosion, transport and accumulat ion. Condition of the grain transport (traction, sa ltation and sus- pension) and energy flow regime will be evaluated o n the based of the grain size parameters dependency diagrams. With the use of these diagrams the morphodynamic zones (erosion, balance and deposition) could be esti mated. Se- lected methods of the fluvial environment lithodyna mic interpretation were collected and decrypted in this article." @default.
- W2306770123 created "2016-06-24" @default.
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- W2306770123 date "2010-01-01" @default.
- W2306770123 modified "2023-09-27" @default.
- W2306770123 title "Litodynamiczna interpretacja środowiska fluwialnego na podstawie wska źników uziarnienia - przegląd wybranych metod Lithodynamic interpretation of fluvial environment based on grain size composition's parameters - review of selected methods" @default.
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