多孔性
扫描电子显微镜
方解石
傅里叶变换红外光谱
磁导率
矿物学
材料科学
碳酸钙
化学工程
球霰石
碳酸盐
复合材料
化学
膜
冶金
工程类
文石
生物化学
作者
Elizabeth Teresita Romero-Guzmán,Lázaro Raymundo Reyes-Gutiérrez,Jaime Klapp,Héctor Hernández‐Mendoza
出处
期刊:Journal of Minerals and Materials Characterization and Engineering
[Scientific Research Publishing, Inc.]
日期:2018-01-01
卷期号:06 (01): 38-49
被引量:1
标识
DOI:10.4236/jmmce.2018.61004
摘要
The aim of this work was to obtain the physicochemical properties by SEM, XRD, FTIR analyses and the surface characteristics from carbonate outcrops cores such as pore diameter, surface area, porosity and permeability. The methods used to characterize them were Scanning Electron Microscopy, SEM; X Ray Diffraction, DRX; Fourier Transform Infrared Spectroscopy, FTIR. The porosity and permeability of natural vuggy fractured porous medium from core samples was determined obtained in the laboratory with conventional procedures. The cores have smooth and rough surfaces with porous with several sizes. Some crystals appear in preferential zones mainly composed by calcium, carbon and oxygen. Apparently into free spaces were found the organic materials, organic residues of crude oil. The cores have smooth and rough surfaces with porous with several sizes. Some crystals appear in preferential zones composed by calcium, carbon and oxygen. Apparently into free spaces were found the organic materials, organic residues of crude oil. The main inorganic compound in cores is calcite, (CaCO3). The porosity was for porous core 26% and for solid core 8.5%. The values obtained show that the cores have permeability where the fluid migrates through the particles at 2.23 × 10-4 cm/s.
科研通智能强力驱动
Strongly Powered by AbleSci AI