Water–rock interaction within the oligotrophic peat bog (part of the Vasyugan Swamp, Western Siberia)

Water–rock interaction within the oligotrophic peat bog (part of the Vasyugan Swamp, Western Siberia)

Bibliographic Details
Parent link:E3S Web of Conferences
Vol. 98 : 16th International Symposium on Water-Rock Interaction (WRI-16) and 13th International Symposium on Applied Isotope Geochemistry (1st IAGC International Conference).— 2019.— [01045, 6 p.]
Corporate Author: Национальный исследовательский Томский политехнический университет Инженерная школа природных ресурсов Отделение геологии
Other Authors: Savichev O. G. Oleg Gennadievich, Mazurov A. K. Aleksey Karpovich, Rudmin M. A. Maksim Andreevich, Soldatova E. A. Evgeniya Aleksandrovna
Summary:Title screen
Geochemical conditions of the formation of various minerals were studied within the oligotrophic pine-shrub and sphagnum peat bog. It was shown that at least two complex barriers function within the peat deposit. These barriers correspond to the changes in the advective and diffusion transfer of substances and promote the immobilization of Fe and a number of other chemical elements. The upper complex geochemical (redox, sulfide and sorption) barrier occurs approximately at the depths of 0.40 to 1.25 m. The lower complex geochemical (alkaline and sorption) and mechanical barriers are located at the bottom part of the peat deposit (the depth of 2.25–2.50 m).
Published: 2019
Subjects:
электронный ресурс
труды учёных ТПУ
торф
торфяные месторождения
барьеры
Online Access:http://earchive.tpu.ru/handle/11683/57305
https://doi.org/10.1051/e3sconf/20199801045
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=660704

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