Equilibrium of nitrogen-rich spring waters of the Baikal Rift Zone with host rock minerals as a basis for determining mechanisms of their formation

التفاصيل البيبلوغرافية
Parent link:Geochemistry International
Vol. 53, iss. 8.— 2015.— [P. 713-725]
مؤلف مشترك: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
مؤلفون آخرون: Shvartsev S. L. Stepan Lvovich, Zamana L. V., Plyusnin A. M., Tokarenko O. G. Olga Grigorievna
الملخص:Title screen
This paper presents calculations of equilibria between nitrogenrich hot springs of the Baikal RiftZone (BRZ) and a secondary mineral assemblage (carbonate, fluoride, clay, zeolite, and other minerals). Theresults confirm the equilibrium–nonequilibrium character of the nitrogen spring water–rock system. Unlikeother water types, the system evolves under conditions of continuous incorporation of chemical elementsreleased from the host minerals into the newly formed secondary minerals. This allows the system to remaindynamically stable with no increase in salinity, despite continued water–rock interaction. The main factorresponsible for this state of the system is a deficiency of acids, i.e., high pH. As a result, the disturbance ofrelationships between concentrations of aqueous species compared to the starting composition of dissolvedsolids produces a deficiency of some elements (Ca, Mg, Fe, Al, etc.) and an excess of other elements (Na, Si,F, etc.).
Режим доступа: по договору с организацией-держателем ресурса
اللغة:الإنجليزية
منشور في: 2015
الموضوعات:
الوصول للمادة أونلاين:http://dx.doi.org/10.1134/S0016702915060087
التنسيق: الكتروني فصل الكتاب
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=644368

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