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...
| Опубликовано в: : | Geoderma Vol. 429. P. 116256 (1-12) |
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| Другие авторы: | , , , , , , , |
| Формат: | Статья в журнале |
| Язык: | English |
| Предметы: | |
| Online-ссылка: | http://vital.lib.tsu.ru/vital/access/manager/Repository/koha:001009378 |
