2020
DOI: 10.1051/e3sconf/202016306002
|View full text |Cite
|
Sign up to set email alerts
|

The structure of the Karay river basin by the longitudinal slopes of the river beds and the average gradients of water catchments slopes

Abstract: The problems of water lag time during flood forecasting, the rate of pollution spreading over the basin area in the event of industrial accidents, the transport of suspended and dissolved substances by rivers, and planning of erosion control measures are very relevant today. Within the framework of the basin approach, an elementary water catchment can be adopted as an elementary unit for the analysis of a particular territory. At the same time, river bed slopes determine the power of the water flow, and the av… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
2
0

Year Published

2023
2023
2024
2024

Publication Types

Select...
1
1

Relationship

0
2

Authors

Journals

citations
Cited by 2 publications
(2 citation statements)
references
References 5 publications
0
2
0
Order By: Relevance
“…However, it is important to consider the antecedent conditions that can affect the storage capacity of the basin (Macrae et al 2010). These conditions include the hydraulic conductivity of soils and the elevation of the water table (Bukovskiy et al 2020). During dry periods, when the storage capacity of the basin is high, a greater amount of precipitation is expected to be retained.…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…However, it is important to consider the antecedent conditions that can affect the storage capacity of the basin (Macrae et al 2010). These conditions include the hydraulic conductivity of soils and the elevation of the water table (Bukovskiy et al 2020). During dry periods, when the storage capacity of the basin is high, a greater amount of precipitation is expected to be retained.…”
Section: Discussionmentioning
confidence: 99%
“…7. Sediment rates determined by the Wallingford model were 357.02 m³/km²/year and 387.38 m³/km²/year for Main Kandar Dam and Auxiliary Kandar Dam, respectively.…”
mentioning
confidence: 92%