Ground water regimes containing country rock minerals in Southern Kuzbass (case study: Narysk-Ostashkin)

Bibliographic Details
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 33 : Contemporary Issues of Hydrogeology, Engineering Geology and Hydrogeoecology in Eurasia.— 2016.— [012003, 6 p.]
Main Author: Domrocheva E.
Corporate Author: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
Other Authors: Lepokurova О. Е. Olesya Evgenyevna
Summary:Title screen
The paper describes the calculation results revealing groundwater in equilibrium to carbonates and aluminosilicate minerals of country rocks in Narysk-Ostashkinsk area. It was proved that groundwater is in nonequilibrium to primary (endogenous) minerals in which they dissolve, however are in equilibrium to clays and carbonates which precipitate in the groundwater. The groundwater composition varies.
Published: 2016
Series:Hydrogeochemistry
Subjects:
Online Access:http://dx.doi.org/10.1088/1755-1315/33/1/012003
http://earchive.tpu.ru/handle/11683/33994
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=649461
Description
Summary:Title screen
The paper describes the calculation results revealing groundwater in equilibrium to carbonates and aluminosilicate minerals of country rocks in Narysk-Ostashkinsk area. It was proved that groundwater is in nonequilibrium to primary (endogenous) minerals in which they dissolve, however are in equilibrium to clays and carbonates which precipitate in the groundwater. The groundwater composition varies.
DOI:10.1088/1755-1315/33/1/012003