Выдержка
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.
| Язык оригинала | Английский |
|---|---|
| Номер статьи | 012004 |
| Журнал | IOP Conference Series: Earth and Environmental Science |
| Том | 43 |
| Номер выпуска | 1 |
| DOI | |
| Состояние | Опубликовано - 11 окт 2016 |
Отпечаток
ASJC Scopus subject areas
- Environmental Science(all)
- Earth and Planetary Sciences(all)
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Identification of clay minerals in reservoir rocks by FTIR spectroscopy. / Khang, Vu Cong; Korovkin, Mikhail V.; Ananyeva, Ludmila G.
В: IOP Conference Series: Earth and Environmental Science, Том 43, № 1, 012004, 11.10.2016.Результат исследований: Материалы для журнала › Статья
}
TY - JOUR
T1 - Identification of clay minerals in reservoir rocks by FTIR spectroscopy
AU - Khang, Vu Cong
AU - Korovkin, Mikhail V.
AU - Ananyeva, Ludmila G.
PY - 2016/10/11
Y1 - 2016/10/11
N2 - 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.
AB - 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.
UR - http://www.scopus.com/inward/record.url?scp=84997771299&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84997771299&partnerID=8YFLogxK
U2 - 10.1088/1755-1315/43/1/012004
DO - 10.1088/1755-1315/43/1/012004
M3 - Article
AN - SCOPUS:84997771299
VL - 43
JO - IOP Conference Series: Earth and Environmental Science
JF - IOP Conference Series: Earth and Environmental Science
SN - 1755-1307
IS - 1
M1 - 012004
ER -