Chemical elements migration in water-travertin system (Tomsk region, Russia) [Электронный ресурс]

Авторы: Lepokurova O.   (ИНГГ СО РАН)  
дата публикации: 2019
To assess the mobility of chemical elements in carbonate, formation processes have calculated the water migration coefficient -Kx and the geochemical mobility coefficient -Kn. The series of geochemical mobility were constructed. The elements that can be deposited and that can be accumulated in water have been distinguished. It is shown that anionic elements - Cl, S, Br, I, U, As, as well as elements such as Na, Mg, Mo, Zr well pass into solution from rocks and remain in the water. Elements such as Ca, Fe, Al, Mn, Si, Ba, Zn, Pb, Co, Hg, Ti, La, Ag, Sn, Cr are most fully deposited in travertines.
первоисточник: E3S Web of Conferences. 16th International Symposium on Water-Rock Interaction (WRI-16) and 13th International Symposium on Applied Isotope Geochemistry (1st IAGC International Conference) (Tomsk, Russia, July 21-26, 2019)
страницы: 07014-07014
внешние ссылки:
WoS   WoS (цитирование)






полный текст статьи