| dc.contributor.author | Yavkin, Vyacheslav | |
| dc.contributor.author | Khodan, Halyna | |
| dc.date.accessioned | 2022-11-14T09:41:09Z | |
| dc.date.available | 2022-11-14T09:41:09Z | |
| dc.date.issued | 2022 | |
| dc.identifier.uri | https://archer.chnu.edu.ua/xmlui/handle/123456789/5341 | |
| dc.description.abstract | In the vertical structure of the river basin, the dominant formation is the
soil. Conditions for the transformation of water supply to the surface of the
basin are determined by the ability of the soil to give or, contrarily, retain
a significant proportion of precipitation. The soil column in the process of
formation of the flood hydrograph performs the functions of moisture
transfer by two opposite signs of the vertical component: filtration and
evaporation. The laws of infiltration were considered by us in the previous
section, where it was found that the leading parameter of the infiltration
process in addition to the intensity of rain is the filtration coefficient | uk_UA |
| dc.language.iso | en | uk_UA |
| dc.publisher | Iasi | uk_UA |
| dc.subject | Key words: Infiltration, particle size distribution, soil moisture, porosity, filtration coefficient | uk_UA |
| dc.title | Principles of estimating soil moisture parameters in the basin. | uk_UA |
| dc.type | Article | uk_UA |
