A compact model, the modified stretched exponential (MSE), for characterization of transverse and longitudinal NMR relaxation of fluid in saturated porous media is presented. The MSE model exhibits the theoretically correct long- and short-time behavior, and its general applicability for representing transverse-relaxation data is demonstrated for a wide range of rock lithologies and saturating fluids at various magnetic field strengths and echo times. The model also provides a reliable and sample-independent method for signal back-extrapolation, which is necessary for quantitative petrophysical NMR measurements, and overcomes the limitations of the well-known stretched-exponential model. (C) 1996 Academic Press, Inc
New down-hole nuclear magnetic resonance (NMR) measurement and interpretation techniques have substa...
A theory of the nuclear magnetic relaxation of fluids in the pore spaces of sedimentary rocks at low...
The determination of penetration depth and distribution of water at surfaces is essential to knowled...
This thesis forms part of a continuing programme of research to investigate the application of NMR t...
Nuclear magnetic resonance (NMR) measurements are widely used to quantify storage and fluid-transpor...
Nuclear magnetic resonance (NMR) relaxation time measurements are affected by pore structure and sat...
In the present study, we investigate the relationship between the relaxation rate and the filling fa...
¹H NMR techniques have gained extensive acceptance in petrophysics for the evaluation of fluid-satur...
Advanced nuclear magnetic resonance (NMR) imaging methodologies have been developed to determine por...
ABSTRACT Nuclear magnetic resonance ͑NMR͒ relaxation times of geologic materials are closely related...
Nuclear magnetic resonance (NMR) relaxation experimentation is an e ective technique for non-destruc...
This thesis considers the relationship between NMR relaxation-diffusion responses and permeability f...
Two often used permeability models, which are based on logarithmic mean of relaxation time distribut...
NMR interpretation is usually based on models that neglect the presence of pendular rings and the di...
[1] For characterizing water flow in the vadose zone, the water retention curve (WRC) of the soil mu...
New down-hole nuclear magnetic resonance (NMR) measurement and interpretation techniques have substa...
A theory of the nuclear magnetic relaxation of fluids in the pore spaces of sedimentary rocks at low...
The determination of penetration depth and distribution of water at surfaces is essential to knowled...
This thesis forms part of a continuing programme of research to investigate the application of NMR t...
Nuclear magnetic resonance (NMR) measurements are widely used to quantify storage and fluid-transpor...
Nuclear magnetic resonance (NMR) relaxation time measurements are affected by pore structure and sat...
In the present study, we investigate the relationship between the relaxation rate and the filling fa...
¹H NMR techniques have gained extensive acceptance in petrophysics for the evaluation of fluid-satur...
Advanced nuclear magnetic resonance (NMR) imaging methodologies have been developed to determine por...
ABSTRACT Nuclear magnetic resonance ͑NMR͒ relaxation times of geologic materials are closely related...
Nuclear magnetic resonance (NMR) relaxation experimentation is an e ective technique for non-destruc...
This thesis considers the relationship between NMR relaxation-diffusion responses and permeability f...
Two often used permeability models, which are based on logarithmic mean of relaxation time distribut...
NMR interpretation is usually based on models that neglect the presence of pendular rings and the di...
[1] For characterizing water flow in the vadose zone, the water retention curve (WRC) of the soil mu...
New down-hole nuclear magnetic resonance (NMR) measurement and interpretation techniques have substa...
A theory of the nuclear magnetic relaxation of fluids in the pore spaces of sedimentary rocks at low...
The determination of penetration depth and distribution of water at surfaces is essential to knowled...