environmentПриродообустройствоPrirodoobustrojstvo1997-6011РГАУ-МСХА10.26897/1997-6011-2024-2-79-82environment-496Research ArticleГИДРАВЛИКА И ИНЖЕНЕРНАЯ ГИДРОЛОГИЯHYDRAULICS AND ENGINEERING HYDROLOGYК вопросу вычисления соотношения объема поверхностного стока воды, гидропотенциала предгорных территорий и общего количества осадковOn the question of calculating the ratio of the volume of surface water runoff, the hydro potential of foothill areas and the total amount of precipitationhttps://orcid.org/0000-0003-1180-1535АсадовХ. Г. AsadovH. H. 

Хикмет Гамид оглы Асадов, д-р техн. наук, профессор

г. Баку

Hikmet H. ogly Asadov, DSc (Eng), professor

Baku

asadzade@rambler.ruСулейманова Е. Д. SuleymanovaE. D. 

Егане Джалал гызы Сулейманова, канд. техн. наук, зам. директора по научной работе ОКБ Космического приборостроения

г. Баку

Egane D. gyzy Suleymanova, CSc (Eng), Deputy director on scientific work of OCB of aerospace instrumentation engineering

Baku

АхмедоваР. А. AkhmedovaR. A. 

Рена Афрас гызы Ахмедова, старший инженер

г. Баку

Rena A. gyzy Akhmedova, senior engineer

Baku

Национальное Аэрокосмическое АгентствоАзербайджанNational Aerospace AgencyAzerbaijan202430052024027982Copyright © Асадов Х.Г., Сулейманова  .Д., Ахмедова Р.А., 20242024Асадов Х.Г., Сулейманова  .Д., Ахмедова Р.А.Asadov H.H., Suleymanova E.D., Akhmedova R.A.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://environment.timacad.ru/jour/article/view/496

В статье рассматривается анализ соотношения объема поверхностного стока, гидропотенциала предгорного ландшафта и общего количества осадков. Проведен критический анализ по известной методике определения количественной оценки поверхностного стока при заданных величинах показателей суммарного осадка и гидрологического потенциала местности ландшафта. Цель работы – выявление двузначности получаемых результатов по известной методике и разработка графоаналитического метода вычисления основных показателей гидрорежима предгорного ландшафта. В качестве базового был использован известный метод CN кривых, используемый для вычисления поверхностного стока в предгорных бассейнах ландшафтов. Разработан графоаналитический метод для вычисления требуемого количества осадков при заданных значениях показателей гидрологического удержания. Предлагаемый метод может быть использован при гидрологических расчетах в целях прогнозирования ожидаемого поверхностного стока участков предгорного ландшафта.

The article is devoted to the analysis of the ratio of the volume of surface runoff, the hydro potential of the foothill landscape and the total amount of precipitation. A critical analysis was carried out using a well-known method for determining the quantitative assessment of surface runoff at given values of total precipitation and hydrological potential of the terrain of the landscape. The purpose of this work is to identify the ambiguity of the results obtained using a well-known technique and to develop a graph-analytical method for calculating the main indicators of the hydro regime of the foothill landscape. Research methods. The well-known CN curve method used to calculate surface runoff in foothill basins of landscapes is used as a base method. The results obtained. A graph-analytical method has been developed to calculate the required amount of precipitation for given values of hydrological retention indicators. Conclusions. The proposed method can be used in hydrological calculations in order to predict the expected surface runoff of areas of the foothill landscape.

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The authors declare that there are no conflicts of interest present.