Response of Carbon Mineralization to Nitrogen Application in Cryogenic Soils
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URI (для ссылок/цитирований):
https://link.springer.com/article/10.1134/S1067413617060066https://elib.sfu-kras.ru/handle/2311/110650
Дата:
2017-12Журнал:
Russian Journal of EcologyКвартиль журнала в Scopus:
Q3Квартиль журнала в Web of Science:
Q4Библиографическое описание:
Matvienko, A. I. Response of Carbon Mineralization to Nitrogen Application in Cryogenic Soils [Текст] / A. I. Matvienko, M. I. Makarov, A. I. Fertikov, I. V. Sviderskaya, O. V. Menyailo // Russian Journal of Ecology. — 2017. — Т. 48 (№ 6). — С. 472-476Текст статьи не публикуется в открытом доступе в соответствии с политикой журнала.
Аннотация:
Cryogenic soils are formed on permafrost and
cover 60–65% of the territory of Russia [1]. A specific
feature of cryogenic forest ecosystems in Eurasia is
that they are dominated by larch, and these ecosystems
are very sensitive to disturbances. Increasing
Nitrogen input is a global trend [2] that will inevitably
affect northern forests of Siberia [3, 4]. Moreover,
nitrogen in boreal forests of Sweden is applied to stimulate
the growth of trees, which leads to additional carbon
accumulation in the biomass. However, the problem
concerning the effect of additional nitrogen input
(with precipitation or fertilizers) on organic matter
mineralization in soils of the cryogenic series has not
been studied sufficiently