Dispersed ice of permafrost peatlands represents an important source of labile carboxylic acids, nutrients and metals

Thawing of frozen organic and mineral soils and liberation of organic carbon (OC), macro- and micro-nutrients and trace elements from pore ice in high latitude regions represent a potentially important but poorly quantified retroactive linkage to climate warming. This is especially true for permafro...

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Bibliographic Details

Published in:	Geoderma Vol. 429. P. 116256 (1-12)
Other Authors:	Kuzmina, Daria M., Lim, Artem G., Loiko, Sergey V., Shefer, Nikita, Shirokova, Liudmila S., Julien, Frédéric, Rols, Jean-Luc, Pokrovsky, Oleg S.
Format:	Article
Language:	English
Subjects:	вечномерзлые торфяники грунтовые воды лед углекислый газ карбоновые кислоты микроэлементы статьи в журналах
Online Access:	http://vital.lib.tsu.ru/vital/access/manager/Repository/koha:001009378