МОРФОЛОГИЯ И УСЛОВИЯ ФОРМИРОВАНИЯ РУСЕЛ БАЛОЧНЫХ РУЧЬЕВ (НА ПРИМЕРЕ РУЧЬЕВ ЧОЛОХОВСКИЙ И ЯЗВИЦЫ, БАССЕЙН СРЕДНЕЙ ПРОТВЫ)

Abstract

The factors of rivulets' channel formation are mostly not the same as those of large and middle rivers. Incised meanders are characteristic of rivulets. The bottom erosion or accumulation velocity consists n*0.1 mm/y, the lateral erosion velocity - n*1 mm/y at the areas of flow incision.