|
ИСТИНА |
Войти в систему Регистрация |
ИСТИНА ИНХС РАН |
||
The Signs and the Role of Structures of Subsurface Flow in Permafrost Zoneстатья
Информация о цитировании статьи получена из
Web of Science,
Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 23 сентября 2021 г.
- Авторы: Chesnokova I.V., Bezdelova A.P., Sergeev D.O., Tananaev N.I., Grishakina E.A.
- Журнал: Water Resources
- Том: 48
- Номер: 5
- Год издания: 2021
- Издательство: Maik Nauka/Interperiodica Publishing
- Местоположение издательства: Russian Federation
- Первая страница: 804
- Последняя страница: 812
- DOI: 10.1134/s0097807821050067
- Аннотация: The subsurface runoff in the permafrost zone shows considerable structural and seasonal specifics. The structural features are due, on the one hand, to the lithologically determined permeable zones of rock massifs and, on the other hand, the permeability governed by lithology. This permeability is a seasonal factor of water flow from the territory, and now it is the focus of studies in various aspects. The structural character is determined by the history of its geological and geocryological development: the runoff structures are most often inherited by the position of rocks of coarser lithological composition or features associated with former geocryological processes (fracturing, formation of cryogenic textures, local thermokarst, etc.). The spatial heterogeneity of the above-permafrost runoff was studied in the European North and in the mountains of the Northern Transbaikalia.
- Добавил в систему: Тананаев Никита Иванович