Organic and organo-mineral colloids in discontinuous permafrost zone
On-going permafrost thaw in discontinuous permafrost regions produces significant amounts of small permafrost subsidence and depressions, while large lakes are likely to drain into streams and rivers. The intensification of permafrost thaw may alter the size distribution and chemical composition of...
Опубликовано в: : | Geochimica et cosmochimica acta Vol. 188. P. 1-20 |
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Другие авторы: | , , , |
Формат: | Статья в журнале |
Язык: | English |
Предметы: | |
Online-ссылка: | http://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000575401 Перейти в каталог НБ ТГУ |