Флювиальный процесс и динамика балочных систем

Аннотация

A close connection between erosion and alluviation is a matter of common knowledge. Little is known, however, on the mechanism which binds the mutually excluding trends into a dialectically undivided process, the known f act being thus of no theoretical nor practical use. Mutual penetration of the incompatible trends results in spontaneous activation of the opposite processes (erosion and alluviation). A process goes up to certain limit and on having reached it assumes inverse direction - which accounts for the «spontaneous evolution» and «self-regulation» phenomena.