Гидролого-морфометрические характеристики овражно-балочных систем центра Русской равнины
Аннотация
The interrelations of gully-balka systems morphometry and hydrological characteristics are analyzed. Runoff transformations were calculated, using morphometric parameters of drainage basins and observations at one of the typical gully-balka watersheds in the control part of the Russian Plain. The relation between mean-maximal runoff and stream's order of the upper links of the drainage network has been obtained: Qn = Q1Nn, where Qn - runoff of the nth order stream, Q1 - runoff of the 1st order stream, n - empirical coefficient. "n" equals to 2,7 for mean-maximal runoffs, it differs in regions with different natural conditions and depends mainly on morphometry of basins of low orders. It changes also with time.
Об авторах
В. П. БондаревРоссия
Е. Ф. Зорина
Россия
С. Н. Ковалев
Россия
Рецензия
Для цитирования:
Бондарев В.П., Зорина Е.Ф., Ковалев С.Н. Гидролого-морфометрические характеристики овражно-балочных систем центра Русской равнины. Геоморфология. 2000;(2):52-58.
For citation:
Bondarev V.P., Zorina E.F., Kovalev S.N. Hydrological-morphometric characteristics of gully-balka systems in the central part of Russian Plain. Geomorfologiya. 2000;(2):52-58.
Послать статью по эл. почте 