Year: 2024
Type: article
Abstract: The scientific work highlights engineering groupings (classifications) of basins in which mudflow can occur, and new designs of mudflow protection structures. Effective anti-mudflow measures for specific specified cases are in many cases determined by a number of unrelated variables, the main of which are: the genesis and type of mudflow formed in the basin, the structure of its channel network and the size of the estimated (maximum) mudflow flow. Therefore, it is practically impossible to create a single universal classification of villages covering all sides of the mudflow process, consisting of measures against the formation of a mudflow phenomenon – protection from the mudflow of economic and recreational facilities located in a mudflow-prone area. You can make a universal grouping, only, for example, genetic or stone, etc. The most effective measures to combat the formation of mudflows resulting from intense and prolonged heavy rains are the regulation of stormwater, pressure reduction and its distribution. For this purpose, the following conservation works are considered, i.e. – planting shrubs and grasses in parts of a mountain or watershed ridge, dividing them into terraces in the form of small channels, channels connecting and diverting mudflow, preservation and development of a fertile soil layer, as well as various measures aimed at protecting the slopes of other structures from erosion.
Source: Mechanics and Technologies
DOI: 10.55956/dwox8304
Language: English
Subfield: Soil Science
Domain: Life Sciences
Open Access status: bronze
OpenAlex ID: W4404833180
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