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Plenty of sediment-transport equations and models have been proposed for the estimation of bedload volumes and rates in mountain streams. Some of the more ‘modern’ equations incorporate explicit considerations of complex phenomena (e.g., hiding/e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bd192b2a8d74a64cc1f8d711238d3b80
https://doi.org/10.5194/icg2022-74
https://doi.org/10.5194/icg2022-74
