摘要：W artykule omówiono wybrane metody interpretacji litodynamicznej środowiska fluwialnego. Przedstawionometody oceny rangowej energii prądu, metody analizy trendów sedymentacyjnych w zakresie zmian wskaźnikówuziarnienia w procesie sedymentacji fluwialnej, modele interpretacji morfodynamicznej i transportu ziaren. Metodyte zostały poddane ocenie merytorycznej na wybranych przykładach badań własnych i literatury.
其他摘要：The grain size parameters (mean size, sorting, skweness, kurtosis, median and first percentile) could be usedfor the lithodynamic interpretation of fluvial environment. Dependency between a particle size and a sedimentologiccondition in the fluvial environment have been defined (Ruby, 1933; Hjulström, 1935; Morris, 1957; Poole, 1957;Aipołow, 1963; Passega, 1964; Sundborga, 1967; Royse, 1968; Braithwaite, 1973; Southard and Boguchwal; 1973,Baker 1974; Kaniecki, 1976; Miller et. al, 1977; Koster, 1978; Middelton and Southard, 1978; Baba and Komar, 1981;Froehlich, 1982; Costa, 1983; Williams, 1983; Eschner and Kichner, 1984; Młynarczyk, 1985; Maizels, 1989;O’Connor, 1993; Mazumder 1994; Le Roux 1977, 2002; Ferguson and Church 2004). Shear and settlement velocitycould be calculated on the base of the grain size. Sediment trend analysis will be used to the change of a grain sizecomposition during erosion, transport and accumulation. Condition of the grain transport (traction, saltation and suspension)and energy flow regime will be evaluated on the based of the grain size parameters dependency diagrams.With the use of these diagrams the morphodynamic zones (erosion, balance and deposition) could be estimated. Selectedmethods of the fluvial environment lithodynamic interpretation were collected and decrypted in this article.
