Ground water regimes containing country rock minerals in Southern Kuzbass (case study: Narysk-Ostashkin); IOP Conference Series: Earth and Environmental Science; Vol. 33 : Contemporary Issues of Hydrogeology, Engineering Geology and Hydrogeoecology in Eurasia

Bibliografische gegevens
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.]
Hoofdauteur: Domrocheva E.
Coauteur: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
Andere auteurs: Lepokurova О. Е. Olesya Evgenyevna
Samenvatting: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.
Taal:Engels
Gepubliceerd in: 2016
Reeks:Hydrogeochemistry
Onderwerpen:
Online toegang:http://dx.doi.org/10.1088/1755-1315/33/1/012003
http://earchive.tpu.ru/handle/11683/33994
Formaat: Elektronisch Hoofdstuk
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=649461
Omschrijving
Samenvatting: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