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Some parameters of the soil exchange complex in the boreal soils of Russiaстатья
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: 16 января 2019 г.
- Авторы: Belousova N.I., Meshalkina J.L.
- Журнал: Eurasian Soil Science
- Том: 33
- Номер: 8
- Год издания: 2000
- Издательство: Maik Nauka/Interperiodica Publishing
- Местоположение издательства: Russian Federation
- Первая страница: 828
- Последняя страница: 840
- Аннотация: patial regularities in the distribution of three parameters of soil exchange complex - cation exchange capacity, pH of salt suspensions, and the degree of soil unsaturation with bases - are analyzed on the basis of published data on 555 profiles of mesomorphic loamy soils in the boreal zone of Russia. These data are included into the "Boreal" database. It is shown that spatial (lateral) differentiation of these parameters is mainly dictated by the lithological factor. The role of zonal (climate-controlled) factor is less distinct and rather ambiguous. Podzolic soils can develop from both poor (low exchange capacity) and rich (high exchange capacity) rocks. In some regions, texture-differentiated soils display nonstandard distribution of pH and base saturation values in their profiles.
- Добавил в систему: Мешалкина Юлия Львовна