Reply to "comment on 'Quantifying solid-fluid interfacial phenomena in porous rocks with proton nuclear magnetic resonance' [J. Appl. Phys. 59, 2788 (1986)]"

Research output: Contribution to journalArticle

Abstract

Near orthogonality relations are presented for an inversion algorithm [J. Appl. Phys. 5, 2788 (1986)] utilized in inverting nuclear magnetic resonance relaxation curves to obtain decay rate distributions. These relations are used to determine resolution limitations of this method. Previously reported experimental results which show anomalous magnetization and shifts in the inverted decay rate distributions in porous rocks occurring at 60%-80% water saturation may be the result of a surface tension driven disjointing of the water films along the pore walls.

Original languageEnglish (US)
Number of pages1
JournalJournal of Applied Physics
Volume63
Issue number4
DOIs
StatePublished - Dec 1 1988
Externally publishedYes

Fingerprint

proton magnetic resonance
decay rates
rocks
nuclear magnetic resonance
fluids
orthogonality
water
interfacial tension
inversions
porosity
saturation
magnetization
shift
curves

ASJC Scopus subject areas

  • Physics and Astronomy(all)

Cite this

@article{86de33342be24ce597cda80ae6137858,
title = "Reply to {"}comment on 'Quantifying solid-fluid interfacial phenomena in porous rocks with proton nuclear magnetic resonance' [J. Appl. Phys. 59, 2788 (1986)]{"}",
abstract = "Near orthogonality relations are presented for an inversion algorithm [J. Appl. Phys. 5, 2788 (1986)] utilized in inverting nuclear magnetic resonance relaxation curves to obtain decay rate distributions. These relations are used to determine resolution limitations of this method. Previously reported experimental results which show anomalous magnetization and shifts in the inverted decay rate distributions in porous rocks occurring at 60{\%}-80{\%} water saturation may be the result of a surface tension driven disjointing of the water films along the pore walls.",
author = "Ehud Schmidt",
year = "1988",
month = "12",
day = "1",
doi = "10.1063/1.339994",
language = "English (US)",
volume = "63",
journal = "Journal of Applied Physics",
issn = "0021-8979",
publisher = "American Institute of Physics Publising LLC",
number = "4",

}

TY - JOUR

T1 - Reply to "comment on 'Quantifying solid-fluid interfacial phenomena in porous rocks with proton nuclear magnetic resonance' [J. Appl. Phys. 59, 2788 (1986)]"

AU - Schmidt, Ehud

PY - 1988/12/1

Y1 - 1988/12/1

N2 - Near orthogonality relations are presented for an inversion algorithm [J. Appl. Phys. 5, 2788 (1986)] utilized in inverting nuclear magnetic resonance relaxation curves to obtain decay rate distributions. These relations are used to determine resolution limitations of this method. Previously reported experimental results which show anomalous magnetization and shifts in the inverted decay rate distributions in porous rocks occurring at 60%-80% water saturation may be the result of a surface tension driven disjointing of the water films along the pore walls.

AB - Near orthogonality relations are presented for an inversion algorithm [J. Appl. Phys. 5, 2788 (1986)] utilized in inverting nuclear magnetic resonance relaxation curves to obtain decay rate distributions. These relations are used to determine resolution limitations of this method. Previously reported experimental results which show anomalous magnetization and shifts in the inverted decay rate distributions in porous rocks occurring at 60%-80% water saturation may be the result of a surface tension driven disjointing of the water films along the pore walls.

UR - http://www.scopus.com/inward/record.url?scp=36549097466&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=36549097466&partnerID=8YFLogxK

U2 - 10.1063/1.339994

DO - 10.1063/1.339994

M3 - Article

VL - 63

JO - Journal of Applied Physics

JF - Journal of Applied Physics

SN - 0021-8979

IS - 4

ER -