River bottom balance: Difference between revisions
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|definition=Dynamically stable condition of a loose gravel bed, due to a well-adjusted sediment balance (sediment transport, abrasion and sanding equal sediment removal). This may cause temporary local shifts in bottom hight with long-term fluctuations around a mean value. | |||
|name_de=Sohlengleichgewicht | |name_de=Sohlengleichgewicht | ||
}} | }} | ||
Latest revision as of 13:42, 5 May 2017
Definition
Dynamically stable condition of a loose gravel bed, due to a well-adjusted sediment balance (sediment transport, abrasion and sanding equal sediment removal). This may cause temporary local shifts in bottom hight with long-term fluctuations around a mean value.