A comparative investigation on the analytical properties and nanostructure of the Sargelu and Asmari reservoirs

Publish Year: 1402
نوع سند: مقاله ژورنالی
زبان: English
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JR_JRCC-5-15_001

تاریخ نمایه سازی: 6 اسفند 1402

Abstract:

The objective of this research was to gain insight into the composition and nanostructure of two shale formations, Sargelu and Asmari. Among the techniques used are X-ray diffractometry (XRD), X-ray fluorescence (XRF), thermogravimetric analysis (TGA), field emission scanning electron microscopy (FESEM), Fourier-transform infrared spectroscopy (FTIR), FESEM focused ion beam (FIB), and transmission electron microscopy (TEM). According to the XRD results, the main components of both shales were calcite, quartz, and kaolinite. CaO, SiO۲, and Fe۲O۳ were the most common components in both reservoirs, according to the XRF analysis, while P۲O۵, SrO, and MoO۳ were only found in the Asmari formation. According to the TGA study, organic matter and other probable carbonate components comprised ۳۷% of the Sargelu and ۴۰.۵% of the Asmari shales. The organic functional groups were detected using FTIR in both samples. Subsequently, various microscopy techniques were utilized to examine different pores, cracks, and nanostructures in each formation.The objective of this research was to gain insight into the composition and nanostructure of two shale formations, Sargelu and Asmari. Among the techniques used are X-ray diffractometry (XRD), X-ray fluorescence (XRF), thermogravimetric analysis (TGA), field emission scanning electron microscopy (FESEM), Fourier-transform infrared spectroscopy (FTIR), FESEM focused ion beam (FIB), and transmission electron microscopy (TEM). According to the XRD results, the main components of both shales were calcite, quartz, and kaolinite. CaO, SiO۲, and Fe۲O۳ were the most common components in both reservoirs, according to the XRF analysis, while P۲O۵, SrO, and MoO۳ were only found in the Asmari formation. According to the TGA study, organic matter and other probable carbonate components comprised ۳۷% of the Sargelu and ۴۰.۵% of the Asmari shales. The organic functional groups were detected using FTIR in both samples. Subsequently, various microscopy techniques were utilized to examine different pores, cracks, and nanostructures in each formation.

Authors

Wenjun He

Research Institute of Exploration and Development, PetroChina Xinjiang Oilfield Company, Karamay, China

Yamin Wang

Institute of Energy, Peking University, Beijing, China

Liang Zhong

Operation Area of Fengcheng Oilfield, PetroChina Xinjiang Oilfield Company, Karamay, China

Seyed Ali Delbari

Department of Engineering Sciences, Faculty of Advanced Technologies, University of Mohaghegh Ardabili, Ardabil, Iran

Abbas Sabahi Namini

Department of Engineering Sciences, Faculty of Advanced Technologies, University of Mohaghegh Ardabili, Ardabil, Iran

Dokyoon Kim

Department of Bionano Engineering, Hanyang University, Ansan ۱۵۵۸۸, Republic of Korea and Institute of Nanosensor Technology, Hanyang University, Ansan ۱۵۵۸۸, Republic of Korea

Ho Won Jang

g Department of Materials Science and Engineering, Research Institute of Advanced Materials, Seoul National University, Seoul ۰۸۸۲۶, Republic of Korea

Mohammadreza Shokouhimehr

Institute of Nanosensor Technology, Hanyang University, Ansan ۱۵۵۸۸, Republic of Korea AND Department of Materials Science and Engineering, Research Institute of Advanced Materials, Seoul National University, Seoul ۰۸۸۲۶, Republic of Korea