Hydrogenous mineral neoformations in Tomsk water intake facility from underground sources; IOP Conference Series: Earth and Environmental Science; Vol. 33 : Contemporary Issues of Hydrogeology, Engineering Geology and Hydrogeoecology in Eurasia

গ্রন্থ-পঞ্জীর বিবরন
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.]
সংস্থা লেখক: 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)
অন্যান্য লেখক: Dutova E. M. Ekaterina Matveevna, Vologdina I., Pokrovsky D., Nalivayko N. G. Nina Grigorievna, Kuzevanov K. I. Konstantin Ivanovich, Pokrovsky V. D. Vitaly Dmitrievich
সংক্ষিপ্ত: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.
ভাষা:ইংরেজি
প্রকাশিত: 2016
মালা:Hydrogeochemistry
বিষয়গুলি:
অনলাইন ব্যবহার করুন:http://dx.doi.org/10.1088/1755-1315/33/1/012017
http://earchive.tpu.ru/handle/11683/33977
বিন্যাস: বৈদ্যুতিক গ্রন্থের অধ্যায়
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=649472
বিবরন
সংক্ষিপ্ত: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.
ডিওআই:10.1088/1755-1315/33/1/012017