Water-rock-ore Interaction (on Example: Major Bakchar Iron-ore Deposit – Western Siberia, Russia); Procedia Earth and Planetary Science; Vol. 17 : 15th Water-Rock Interaction International Symposium, WRI-15

Water-rock-ore Interaction (on Example: Major Bakchar Iron-ore Deposit – Western Siberia, Russia); Procedia Earth and Planetary Science; Vol. 17 : 15th Water-Rock Interaction International Symposium, WRI-15

Bibliografiset tiedot
Parent link:Procedia Earth and Planetary Science.— , 2009-
Vol. 17 : 15th Water-Rock Interaction International Symposium, WRI-15.— 2017.— [P. 690-693]
Päätekijä: Lepokurova О. Е. Olesya Evgenyevna
Yhteisötekijä: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
Muut tekijät: Ivanova I. S. Irina S.
Yhteenveto:Title screen
The paper includes data of the enclosing sediment, iron ore and groundwater composition within Bakchar iron ore cluster. Based on the water chemical composition analysis the thermodynamic equilibrium was calculated for enclosing sediment–groundwater–secondary sediments system, and being correlated to existing geological data. According to thermodynamic calculations, water is non-equilibrium to primary enclosing rock aluminosilicate minerals in which they dissolve and, consequently, are enriched by these chemical elements: Fe, Ca, Mg, K, Na, Si, Al, Mn and others. These accumulated elements in the solution provide clay-water equilibrium, carbonate-water equilibrium, Fe oxides and hydrooxides-water equilibrium.
Kieli:englanti
Julkaistu: 2017
Aiheet:
электронный ресурс
труды учёных ТПУ
железо
грунтовые воды
Бакчарское месторождение
Западная Сибирь
система вода-порода-руда
Linkit:https://doi.org/10.1016/j.proeps.2016.12.155
Aineistotyyppi: Elektroninen Kirjan osa
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=655202

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