Quantitative characterization and micro-CT mineral mapping of natural fissural enamel lesions

2016 ◽  
Vol 46 ◽  
pp. 23-29 ◽  
Author(s):  
Mahdi Shahmoradi ◽  
Michael V. Swain
2013 ◽  
Vol 671-674 ◽  
pp. 1830-1834
Author(s):  
Yun Tao Ji ◽  
Patrick Baud ◽  
Teng Fong Wong ◽  
Li Qiang Liu

The pore structure in intact and inelastically deformed Indiana limestone have been studied using x-ray microtomography imaging. Guided by detailed microstructural observations and using Multi-level Otsu’s thresholding method, the 3D images acquired at voxel side length of 4 μm were segmented into three domains: solid grains, macropores and an intermediate zone dominated by microporosity. Local Porosity can be defined to infer the porosity of each voxel. The macropores were individually identified by morphological processing and their shape quantified by their sphericity and equivalent diameter. With this segmentation, we obtained statistics on macropores on intact and deformed Indiana limestone which shows that inelastic compaction was followed by a significant reduction in the number of macropores. And also our results revealed the great potentiality to produce a quantitative analysis on porous material with the aid of micro CT images.


Author(s):  
Jun KATAGIRI ◽  
Takashi MATSUSHIMA ◽  
Hidetaka SAOMOTO ◽  
Mori UTSUNO ◽  
Yasuo YAMADA

Geofluids ◽  
2020 ◽  
Vol 2020 ◽  
pp. 1-13
Author(s):  
Boli Wang ◽  
Xisen Zhao ◽  
Wen Zhou ◽  
Bin Chang ◽  
Hao Xu

The pore connectivity and distribution of moveable fluids, which determines fluid movability and recoverable reserves, are critical for enhancing oil/gas recovery in tight sandstone reservoirs. In this paper, multiple techniques including high-pressure mercury intrusion porosimetry (MIP), nuclear magnetic resonance (NMR), scanning electron microscopy (SEM), and microcomputer tomography scanning (micro-CT) were used for the quantitative characterization of pore structure, pore connectivity, and movable fluid distribution. Firstly, sample porosity and permeability were obtained. Pore morphology and the 3D distribution of the pore structures were analyzed using SEM and micro-CT, respectively. The pore-size distribution (PSD) from NMR was generally broader than that from MIP because this technique simply characterized the connected pore volume, whereas NMR showed the total pore volume. Therefore, an attempt was made to calculate pore connectivity percentages of pores with different radii (<50 nm, 50 nm–0.1 μm, and 0.1 μm–1 μm) using the difference between the PSD obtained from MIP and NMR. It was found that small pores (r<0.05 μm) contributed 5.02%–18.00% to connectivity, which is less than large pores (r>0.05 μm) with contribution of 36.60%–92.00%, although small pores had greater pore volumes. In addition, a new parameter, effective movable fluid saturation, was proposed based on the initial movable fluid saturation from NMR and the pore connectivity percentage from MIP and NMR. The results demonstrated that the initial movable fluid saturation decreased by 14.16% on average when disconnected pores were excluded. It was concluded that the effective movable fluid saturation has a higher accuracy in evaluating the recovery of tight sandstone reservoirs.


2009 ◽  
Vol 22 (01) ◽  
Author(s):  
T Rodt ◽  
C von Falck ◽  
R Halter ◽  
M Diensthuber ◽  
M Galanski ◽  
...  
Keyword(s):  

Author(s):  
M Kampschulte ◽  
A Dannenmaier ◽  
AC Langheinrich ◽  
T Bschleipfer ◽  
W Weidner ◽  
...  
Keyword(s):  

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