Hydrogenous mineral neoformations in Tomsk water intake facility from underground sources

Bibliografske podrobnosti
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 33 : Contemporary Issues of Hydrogeology, Engineering Geology and Hydrogeoecology in Eurasia.— 2016.— [012017, 6 p.]
Corporate Authors: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ), Национальный исследовательский Томский политехнический университет (ТПУ) Управление программ развития (УПР) Центр мониторинга и рейтинговых исследований (Центр МИР)
Drugi avtorji: Dutova E. M. Ekaterina Matveevna, Vologdina I., Pokrovsky D., Nalivayko N. G. Nina Grigorievna, Kuzevanov K. I. Konstantin Ivanovich, Pokrovsky V. D. Vitaly Dmitrievich
Izvleček:Title screen
The article considers study outcomes of hydrogenous mineral neoformations precipitated on deferrization filters of Tomsk water intake facility from underground sources. Compositionally, these precipitations are colloform and polymineral including ferrous, carbonate and aluminosilicate mineral phases. Ferrous phase predominates and embraces ferric hydroxides (ferrihydrate, goethite, hematite and lepidocrocite) and ferrous hydrophosphates (vivianite, strengite, strunzite and rockbridgeit). Carbonate and aluminosilicate minerals are calcite and kaolinite-group, respectively.
Jezik:angleščina
Izdano: 2016
Serija:Hydrogeochemistry
Teme:
Online dostop:http://dx.doi.org/10.1088/1755-1315/33/1/012017
http://earchive.tpu.ru/handle/11683/33977
Format: Elektronski Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=649472
Opis
Izvleček:Title screen
The article considers study outcomes of hydrogenous mineral neoformations precipitated on deferrization filters of Tomsk water intake facility from underground sources. Compositionally, these precipitations are colloform and polymineral including ferrous, carbonate and aluminosilicate mineral phases. Ferrous phase predominates and embraces ferric hydroxides (ferrihydrate, goethite, hematite and lepidocrocite) and ferrous hydrophosphates (vivianite, strengite, strunzite and rockbridgeit). Carbonate and aluminosilicate minerals are calcite and kaolinite-group, respectively.
DOI:10.1088/1755-1315/33/1/012017