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The Formation of Soil Cover Patterns on Tidal Marshes of the Arctic of Russiaстатья
Дата последнего поиска статьи во внешних источниках: 8 апреля 2022 г.
- Авторы: Tseits M.A., Marechek M.S.
- Журнал: Moscow University Soil Science Bulletin
- Том: 76
- Номер: 5
- Год издания: 2021
- Издательство: Allerton Press Inc.
- Местоположение издательства: United States
- Первая страница: 273
- Последняя страница: 282
- Аннотация: Soils and soil cover on accumulative tidal sea marshes develop under periodic alternation of thalassogenic (marine) and terrigenic factors. The spatial distribution of marsh soils is also controlled by both general and specific (thalassogenic) factors. Open coasts are mainly formed by wave processes and have unidirectional trends in the distribution of pedogenic conditions: perpendicular to the shoreline. Therefore, different soils are aligned as strips along the shoreline. The coasts of shallow seas with strongly indented shorelines have a wide gently sloping intertidal zone. Wind waves have little effect on the distribution of coastal sediments; low-energy tidal waves are the main factor responsible for the transfer of mineral and organic particles. The striated pattern of soil distribution can be significantly complicated or not manifested at all.The aim of this work was to define the specific factors of the soil cover formation on soft seacoasts of the Arctic seas of Russia. We conclude that such thalassogenic factors as creeks, boulders, sea ice, and salvage timber and algae emissions had major effects on the soil cover pattern. The factors controlling soil distribution vary among the seacoasts. They also frequently interact with each other having an emergent effect on soil cover pattern.
- Добавил в систему: Цейц Михаил Александрович
Прикрепленные файлы
| № | Имя | Описание | Имя файла | Размер | Добавлен |
|---|---|---|---|---|---|
| 1. | Полный текст | The Formation of Soil Cover Patterns on Tidal Marshes of the Arctic of Russia | document.pdf | 2,8 МБ | 11 ноября 2022 [zeits] |
| 2. | Первая страница | BSSM273-1.pdf | 43,1 КБ | 21 января 2022 [zeits] |