Quantification of glutathione transverse relaxation time T 2 using echo time extension with variable refocusing selectivity and symmetry in the human brain at 7 Tesla

2018 ◽  
Vol 290 ◽  
pp. 1-11 ◽  
Author(s):  
Kelley M. Swanberg ◽  
Hetty Prinsen ◽  
Daniel Coman ◽  
Robin A. de Graaf ◽  
Christoph Juchem
2018 ◽  
Vol 80 (2) ◽  
pp. 452-461 ◽  
Author(s):  
Patrik O. Wyss ◽  
Claudio Bianchini ◽  
Milan Scheidegger ◽  
Ioannis A. Giapitzakis ◽  
Andreas Hock ◽  
...  

2012 ◽  
Vol 38 (5) ◽  
pp. 1224-1229 ◽  
Author(s):  
Jarunee Intrapiromkul ◽  
He Zhu ◽  
Ying Cheng ◽  
Peter B. Barker ◽  
Richard A.E. Edden

2017 ◽  
Vol 79 (3) ◽  
pp. 1260-1265 ◽  
Author(s):  
Dinesh K. Deelchand ◽  
Edward J. Auerbach ◽  
Naoharu Kobayashi ◽  
Małgorzata Marjańska

Geophysics ◽  
2019 ◽  
Vol 84 (2) ◽  
pp. MR73-MR84 ◽  
Author(s):  
Fatemeh Razavirad ◽  
Myriam Schmutz ◽  
Andrew Binley

We have evaluated several published models using induced polarization (IP) and nuclear magnetic resonance (NMR) measurements for the estimation of permeability of hydrocarbon reservoir samples. IP and NMR measurements were made on 30 samples (clean sands and sandstones) from a Persian Gulf hydrocarbon reservoir. We assessed the applicability of a mechanistic IP-permeability model and an empirical IP-permeability model recently proposed. The mechanistic model results in a broader range of permeability estimates than those measured for sand samples, whereas the empirical model tends to overestimate the permeability of the samples that we tested. We also evaluated an NMR permeability prediction model that is based on porosity [Formula: see text] and the mean of the log transverse relaxation time ([Formula: see text]). This model provides reasonable permeability estimations for the clean sandstones that we tested but relies on calibrated parameters. We also examined an IP-NMR permeability model, which is based on the peak of the transverse relaxation time distribution, [Formula: see text] and the formation factor. This model consistently underestimates the permeability of the samples tested. We also evaluated a new model. This model estimates the permeability using the arithmetic mean of log transverse NMR relaxation time ([Formula: see text]) and diffusion coefficient of the pore fluid. Using this model, we improved estimates of permeability for sandstones and sand samples. This permeability model may offer a practical solution for geophysically derived estimates of permeability in the field, although testing on a larger database of clean granular materials is needed.


1999 ◽  
Vol 91 (2) ◽  
pp. 93-100 ◽  
Author(s):  
Adolf Pfefferbaum ◽  
Edith V Sullivan ◽  
Maj Hedehus ◽  
Michael Moseley ◽  
Kelvin O Lim

Sign in / Sign up

Export Citation Format

Share Document