Mineralogical and Geochemical Features of a Peat Deposit in the Eutrophic Obskoye Fen under Anthropogenic Load (Western Siberia); Doklady Earth Sciences; Vol. 492, iss. 1

Detalles Bibliográficos
Parent link:Doklady Earth Sciences
Vol. 492, iss. 1.— 2020.— [P. 320-322]
Autor Corporativo: Национальный исследовательский Томский политехнический университет Инженерная школа природных ресурсов Отделение геологии
Otros Autores: Savichev O. G. Oleg Gennadievich, Rudmin M. A. Maksim Andreevich, Mazurov A. K. Aleksey Karpovich, Nalivayko N. G. Nina Grigorievna, Sergienko V. I. Valentin, Semiletov I. P. Igor Petrovich
Sumario:Title screen
The chemical composition and mineral inclusions in peats and the underlying soils of the eutrophic Obskoye fen (Western Siberia, Tomsk Region) are studied. The basic pattern of a change in the mineralogical and geochemical conditions at depth consists in domination of hydroxides on top of the peat deposit and sulfides at the bottom. The geochemical reduction barrier is formed at the bottom of the peat deposit. Its functioning is related to increased concentrations of U and Hg. The markedly pronounced influence exerted by sewage discharge is associated with an increase in the Na concentration in acid extracts from peats and additional accumulation of the mixture of suspended, colloidal, and dissolved forms of some metals in the boggy environment.
Режим доступа: по договору с организацией-держателем ресурса
Lenguaje:inglés
Publicado: 2020
Materias:
Acceso en línea:https://doi.org/10.1134/S1028334X20050219
Formato: Electrónico Capítulo de libro
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=663509