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Soil memory: Types of record, carriers, hierarchy and diversityстатья
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: 27 февраля 2017 г.
- Авторы: Targulian V.O., Goryachkin S.V.
- Журнал: Revista Mexicana de Ciencias Geologicas
- Том: 21
- Год издания: 2004
- Издательство: Universidad Nacional Autonoma de Mexico
- Местоположение издательства: Mexico
- Первая страница: 1
- Последняя страница: 8
- Аннотация: The concept of palimpsest-wise soil memory and record is generally characterized in comparison with the book-wise memory and record of sedimentary rocks. Soil systems have a capacity for storing information about environmental factors and pedogenic processes that have been acting for a period of pedogenesis. The main mechanisms of soil memory and record formation are those sets of pedogenic processes that generate the solid phase products and features within the multiphase soil system. The main types of solid-phase carriers of soil memory and their spatial/temporal hierarchy within the soil system are briefly described. The phenomena of isomorphism and polymorphism of soil record carriers in regard to the pedogenic processes should be realized when we try to decode and understand the information stored in soil memory. Each specific type of climate could not be imprinted in only one type of pedon. When reading the record in the soil system under one type of climate, it is obligatory to account for the diversity of solid phase soil horizons and pedons induced by the diversity of parent materials (lithodiversity), topography (topodiversity), biota (biodiversity) and duration of pedogenesis (chronodiversity).
- Добавил в систему: Горячкин Сергей Викторович
Прикрепленные файлы
| № | Имя | Описание | Имя файла | Размер | Добавлен |
|---|---|---|---|---|---|
| 1. | Полный текст | Dialnet-SoilMemory-821583.pdf | 169,8 КБ | 11 марта 2017 [votargulian] |