scholarly journals Pore-space characterization of an altered tonalite by X-ray computed microtomography and the14C-labeled-polymethylmethacrylate method

2012 ◽  
Vol 117 (B1) ◽  
pp. n/a-n/a ◽  
Author(s):  
M. Voutilainen ◽  
M. Siitari-Kauppi ◽  
P. Sardini ◽  
A. Lindberg ◽  
J. Timonen
2017 ◽  
Author(s):  
Megan M. Smith ◽  
Susan A. Carroll ◽  
Amber Connor

2019 ◽  
Vol 155 ◽  
pp. 109748
Author(s):  
Yudong Xue ◽  
Qinglei Wang ◽  
Jianbao Hu ◽  
Haijun Zhou ◽  
Qingliang Shan ◽  
...  

2018 ◽  
Vol 44 (11) ◽  
pp. 12315-12328 ◽  
Author(s):  
Eva Gregorová ◽  
Tereza Uhlířová ◽  
Willi Pabst ◽  
Petra Diblíková ◽  
Ivona Sedlářová

2017 ◽  
Author(s):  
Jordi Cama ◽  
◽  
Gabriela Davila ◽  
Maria Garcia-Rios ◽  
Josep M. Soler

2018 ◽  
Vol 18 (3) ◽  
pp. 3-13
Author(s):  
Aline Maria Poças Belila ◽  
Michelle Chaves Kuroda ◽  
João Paulo Da Ponte Souza ◽  
Alexandre Campane Vidal ◽  
Osvair Vidal Trevisan

Carbonate rocks constitute a large number of petroleum reservoirs worldwide. Notwithstanding, the characterization of these rocks is still a challenge due to their high complexity and pore space variability, indicating the importance of further studies to reduce uncertainty in reservoir interpretation and characterization. This work was performed for coquina samples from Morro do Chaves Formation (Sergipe-Alagoas Basin), analogous to important Brazilian reservoirs. Computed tomography (CT) was used for three-dimensional characterization of rock structure. The neural network named Self-Organizing Maps (SOM) was used for CT images segmentation. According to our tests, CT demonstrated to be a consistent tool for quantitative and qualitative analysis of heterogeneous pore space, by the evaluation of porosity, connectivity and the representative elementary volume.


2008 ◽  
Vol 1124 ◽  
Author(s):  
Mikko Voutilainen ◽  
Suvi Lamminmäki ◽  
Jussi Timonen ◽  
Marja Siitari-kauppi ◽  
Daniel Breitner

AbstractEvaluation of the transport and retardation properties of rock matrices that serve as host rock for nuclear waste repositories necessitates their thorough pore-space characterization. Relevant properties to be quantified include the diffusion depth and volume adjacent to water conducting features. The bulk values of these quantities are not sufficient due to the heterogeneity of mineral structure on the scale of the expected transport/interaction distances. In this work the 3D pore structure of altered granite samples with porosities of 5 to 15%, taken next to water conducting fractures at 180 200 m depth in Sievi, Finland, was studied. Characterization of diffusion pathways and porosity were based on quantitative autoradiography of rock sections impregnated with C14-labelled polymethylmethacrylate (PMMA). Construction of 3D structure from PMMA autoradiographs was tested. The PMMA method was augmented by field emission scanning electron microscopy and energy-dispersive X-ray analyses (FESEM/EDAX) in order to study small pore-aperture regions in more detail and to identify the corresponding minerals. The 3D distribution of minerals and their abundances were determined by X-ray microtomography. Combining the mineral specific porosity found by the PMMA method with these distributions provided us with a 3D porosity distribution in the rock matrix.


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