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On the hydrological role of the relief in the southern part of the Russian Plain

https://doi.org/10.31857/S0435-42812019346-56

Abstract

On the example of a southern  part of the Russian Plain the surface slope runoff, the runoff from the hydrographic network and snow melt river runoff are considered. Based on the analysis of the data by water balance stations and the correlation  of surface slope runoff values from different lands to the zonal river runoff value, the zonal values of the spring surface slope flow from separate lands located on loam and sandy loam soils are determined.  Within agricultural lands there are fall plowed fields and non-plowed  in autumn (stubble, layland, winter crops, perennial grasses). By the beginning of the spring flood, the soil at autumnplowed fields is loosened and reduces the runoff, while on the fields that were not plowed in the autumn soil is compacted.  In addition,  the microtopography created  by autumn  plowing also contributes  to the runoff reduction.  The smallest surface slope runoff occurs under the forest. Differences in runoff increase in the direction  from the southern  part of the forest zone to the steppe areas. Taking into account  the land composition  and the mechanical  composition  of the soils, the weighted average values of the surface slope runoff were obtained for the period of the long-time  average annual flow calculation (late 19th century and early 1960s). It is shown that subsequently there was a decrease in the spring surface slope runoff, initially as a result of the autumn plowing increase, and more recently, mainly as a result of changes in meteorological conditions, especially during the cold season (air temperature  rising, frequent thaws, increased infiltration). In the overall structure of the spring river flood, along with a decrease in the share of surface slope runoff, the share of surface runoff formed in the hydrographic network increases, and especially the flow of infiltration origin (verhovodka and underground runoff). In the steppe zone the structure of river flow has changed most significantly.

About the Authors

N. I. Koronkevich
Institute of Geography RAS
Russian Federation
Moscow.


S. V. Dolgov
Institute of Geography RAS
Russian Federation
Moscow.


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For citations:


Koronkevich N.I., Dolgov S.V. On the hydrological role of the relief in the southern part of the Russian Plain. Geomorfologiya. 2019;(3):46-56. (In Russ.) https://doi.org/10.31857/S0435-42812019346-56

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