Identification of clay minerals in reservoir rocks by FTIR spectroscopy

Manylion Llyfryddiaeth
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 43 : Problems of Geology and Subsurface Development.— 2016.— [012004, 4 p.]
Prif Awdur: Vu Cong Khang
Awduron Corfforaethol: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра геологии и разработки нефтяных месторождений (ГРНМ), Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра геологии и разведки полезных ископаемых (ГРПИ)
Awduron Eraill: Korovkin M. V. Mikhail Vladimirovich, Ananieva L. G. Ludmila Gennadievna
Crynodeb:Title screen
Clay minerals including kaolinite, montmorillonite and bentonite in oil and gas reservoir rocks are identified by absorption spectra obtained via Fourier Transform Infrared (FTIR) spectroscopy. Bands around 3695, 3666, 3650 and 3630 cm{-1} and bands around 3620 and 3400 cm{-1} are the most diagnostically reliable for kaolinite and montmorillonite, respectively; also absorption bands in the region of 1200...955 cm{-1} are equally diagnostic for all the clay minerals studied.
Cyhoeddwyd: 2016
Cyfres:Mineralogy, Geochemistry and Petrography
Pynciau:
Mynediad Ar-lein:http://dx.doi.org/10.1088/1755-1315/43/1/012004
http://earchive.tpu.ru/handle/11683/35141
Fformat: Electronig Pennod Llyfr
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=650798

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