Method of calculation largest expenditure raise of alluvium mud torrets and floods (on the example, of the rivers Lenkoran natural area)

The influnce of the main natural factors on mud formation is considered in the article. The coefficients of disturbace of the surface of the river watersheds of mud flows are 0.06-0.08. The total area of the mud flow foci of Vlachay, Lankaranchay and Tangerud ranges from 11 to 72 km2, and to the cone of the removal 6.4-8.1 km2. The relationship between the values of the largest charges of suspended sediments and the largest water discharge, the average height of the catchment area, the basin area and the natural regulation of rivers has been revealed. A set of parameters integrally reflects the increase in the largest water factors. The analysis of the connection shows that with the increase in the largest water discharge, the average height of the catchment area, the largest discharge of suspended sediments increases, and with the increase in the catchment area and the natural control of the drain. Specific hydrological conditions dictate the need for the dependence present in the form of 3 equations. This allows us to more fully illuminate this issue in contrast to previous studies and develop a methodology for its calculation.