Pore-scale modelling of NMR relaxation for the characterization of wettability

2006 ◽  
Vol 52 (1-4) ◽  
pp. 172-186 ◽  
Author(s):  
S.H. Al-Mahrooqi ◽  
C.A. Grattoni ◽  
A.H. Muggeridge ◽  
R.W. Zimmerman ◽  
X.D. Jing
2020 ◽  
Author(s):  
Peleg Haruzi ◽  
Regina Katsman ◽  
Matthias Halisch ◽  
Nicolas Waldmann ◽  
Baruch Spiro

Abstract. This paper presents a detailed description and evaluation of a multi-methodological petrophysical approach for the comprehensive multiscale characterization of reservoir sandstones. The suggested methodology enables the identification of Darcy-scale permeability links to an extensive set of geometrical, textural and topological rock descriptors quantified at the pore scale. This approach is applied to the study of samples from three consecutive sandstone layers of Lower Cretaceous age in northern Israel. These layers differ in features observed at the outcrop, hand specimen, petrographic microscope and micro-CT scales. Specifically, laboratory porosity and permeability measurements of several centimetre-sized samples show low variability in the quartz arenite (top and bottom) layers but high variability in the quartz wacke (middle) layer. The magnitudes of this variability are also confirmed by representative volume sizes and by statistical anisotropy analyses conducted on micro-CT-imaged 3D pore geometries. Two scales of porosity variability are revealed by applying variogram analysis to the top layer: fluctuations at 150 μm are due to variability in the pore size, and those at 2 mm are due to the occurrence of high- and low-porosity bands occluded by iron oxide cementation. This millimetre-scale variability is found to control the laboratory-measured macroscopic rock permeability. Good agreement between the permeability upscaled from the pore-scale modelling and the estimates based on laboratory measurements is shown for the quartz arenite (top) layer. The proposed multi-methodological approach leads to an accurate petrophysical characterization of reservoir sandstones with broad ranges of textural, topological and mineralogical characteristics and is particularly applicable for describing anisotropy at various rock scales. The results of this study also contribute to the geological interpretation of the studied stratigraphic units.


2020 ◽  
Author(s):  
Ryan Payton ◽  
Yizhuo Sun ◽  
Andrew Kingdon ◽  
Saswata Hier-Majumder

2021 ◽  
Vol 235 ◽  
pp. 116500
Author(s):  
Yongli Wu ◽  
Qinfu Hou ◽  
Zheng Qi ◽  
Aibing Yu

Author(s):  
Matthew A. Stetz ◽  
José A. Caro ◽  
Sravya Kotaru ◽  
Xuejun Yao ◽  
Bryan S. Marques ◽  
...  

2022 ◽  
Vol 13 (1) ◽  
Author(s):  
Albert A. Smith ◽  
Alexander Vogel ◽  
Oskar Engberg ◽  
Peter W. Hildebrand ◽  
Daniel Huster

AbstractBiomolecular function is based on a complex hierarchy of molecular motions. While biophysical methods can reveal details of specific motions, a concept for the comprehensive description of molecular dynamics over a wide range of correlation times has been unattainable. Here, we report an approach to construct the dynamic landscape of biomolecules, which describes the aggregate influence of multiple motions acting on various timescales and on multiple positions in the molecule. To this end, we use 13C NMR relaxation and molecular dynamics simulation data for the characterization of fully hydrated palmitoyl-oleoyl-phosphatidylcholine bilayers. We combine dynamics detector methodology with a new frame analysis of motion that yields site-specific amplitudes of motion, separated both by type and timescale of motion. In this study, we show that this separation allows the detailed description of the dynamic landscape, which yields vast differences in motional amplitudes and correlation times depending on molecular position.


2009 ◽  
Vol 83 (1) ◽  
pp. 151-169 ◽  
Author(s):  
Nasiru A. Idowu ◽  
Martin J. Blunt

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