Computer-controlled, portable pulsed NMR instrument and method of use

Claim 1

Automatic apparatus for swiftly determining fluid-flow properties of a rock sample based on NMR response of hydrogen nuclei of interstitial fluids within pore spaces of said sample in which DC field inhomogeneity and phase background jitter are used to increase data-throughput efficiency (DTE) comprising: (a) magnet means for producing a DC magnetic field acting on said rock sample, said magnetic field having an intensity of at least 1 kilogauss and an inhomogeneity of at least D gauss to provide a series of nuclear magnetization build-ups associated with said interstitial fluids within said sample as a function of time; (b) RF coil means acting at right angles to said DC magnetic field; (c) transmitter means including digital control means for generating a first series of digital control codes associated with a series of RF magnetic pulses of selected frequency, amplitude and duration, connected to said RF coil means to produce said series of RF magnetic pulses for interrogating said sample, said amplitude of each pulse being controlled to be at least greater than the variation D in said DC field over said sample; (d) receiver means connected to said digital control means and to said RF coil means for generating via a second series of digital control codes associated with a plurality of time windows, output signals proportional to said nuclear magnetic resonance response of said interstitial fluids; (e) said transmitter means including said digital control means having a phasal background jitter characteristic associated therewith that randomly varies with time so that said sample can be repetitively interrogated to serially indicate nuclear magnetization relaxation without need for applying rescrambling reversing RF magnetic field pulses prior to the start of each magnetization build-up cycle.

Claim 8

A method for swiftly determining fluid-flow properties of a rock sample based on nuclear magnetic resonance (NMR) response of hydrogen nuclei of interstitial fluids within said sample in which DC field inhomogeneity and phasal background jitter are used to increase data-throughput efficiency (DTE) comprising: (a) storing digital control codes associated with (i) control of a series of interrogation RF magnetic pulses of selected frequency, duration and magnitude and (ii) generation of a plurality of time windows for detection of a plurality of NMR response signals; (b) placing the rock sample in a steady DC magnetic field having a strength of at least 1 kilogauss and an inhomogeneity of at least D gauss to provide a series of nuclear magnetization build-ups associated with said interstitial fluids; (c) under control of said control codes, subjecting said sample to interrogation by said series of RF magnetic field pulses having in addition to said selected frequency, duration and magnitude values, a phasal background jitter characteristic that is random with time, to cause reorientation of each of said series of built-up magnetizations, the magnitude of each of said pulses being greater than the variation D in strength in said DC field over said sample; and (d) automatically detecting after interrogation in accordance with said control codes, said plurality of nuclear magnetic resonance (NMR) signals indicative of nuclear magnetization relaxation, each of said NMR signals occurring between pulses of said RF magnetic field without need for application of reversing RF field pulses prior to the start of each magnetization build-up cycle.

Claim 9

A method for swiftly determining fluid-flow properties of a rock sample based on nuclear magnetic resonance (NMR) response of hydrogen nuclei of interstitial fluids within said sample in which DC field inhomogeneity and phasal background jitter are used to increase data-throughput efficiency (DTE) comprising: (a) storing digital control codes associated with (i) control of a series of interrogation RF magnetic pulses of selected frequency, duration and magnitude and (ii) generation of a plurality of time windows for detection of a plurality of NMR response signals; (b) placing the rock sample in a steady DC magnetic field having a strength of at least 1 kilogauss and an inhomogeneity of at least D gauss to provide a series of nuclear magnetization build-ups associated with said interstitial fluids; (c) under control of said control codes, subjecting said sample to interrogation by said series of RF magnetic field pulses having in addition to said selected frequency, duration and magnitude values, a phasal background jitter characteristic that is random with time, to cause reorientation of each of said series of built-up magnetizations, the magnitude of each of said pulses being greater than the variation D in strength in said DC field over said sample; and (d) automatically detecting after interrogation in accordance with said control codes, said plurality of nuclear magnetic resonance (NMR) signals indicative of nuclear magnetization relaxation, each of said NMR signals occurring between pulses of said RF magnetic field without need for application of reversing RF field pulses prior to the start of each magnetization build-up cycle.

Claim 12

A method for swiftly determining fluid-flow properties based on NMR response of hydrogen nuclei of interstitial fluid within rock samples, which properties may include porosity, permeability, recoverable fluid content, large-pore specific surface, argillaceous specific surface, or any combination or subcombination of these properties, in which DC field inhomogeneity and random phasal background jitter are used to increase data-throughput efficiency (DTE), of a measuring system comprising: (a) storing digital control codes associated with (i) control of a series of interrogation RF magnetic pulses of selected frequency duration and magnitude and (ii) generation of a plurality of time windows for detection of a plurality of NMR response signals; (b) placing the rock sample in a steady DC magnetic field having a strength of at least 1 kilogauss and an inhomogeneity of about D gauss to aid in providing a series of nuclear magnetizations build-ups associated with said interstitial fluid within said rock sample, said each nuclear magnetization having a preferential alignment parallel to said DC magnetic field; (c) subjecting said sample on a sequential basis in accordance with said control codes, to said series of RF magnetic pulses to cause reorientation of said magnetization to preferred alignments offset from said DC field, said amplitude of said interrogation pulses being greater than the variation D in strength of said DC field over the sample; (d) automatically detecting after interrogation, in accordance with said control codes, NMR responses associated with precession of said magnetization build-ups about axes substantially parallel of said DC field magnetic field within said plurality of time windows, each of said windows occurring within an interval between two of said interrogation pulses and within subintervals beginning at a fixed delayed time after cessation of each of said interrogation pulses; and (e) automatically repeating steps (c)-(d) in accordance with different digital control codes whereby a different predetermined average repetition rate for said interrogation pulses is used to obtain at least a second statistically-improved signal representing nuclear magnetization relaxation in said DC magnetic field within at least a different average time interval between said interrogation pulses, whereby flow properties of said sample can be indicated.

Claim 13

A method for swiftly determining fluid-flow properties based on NMR response of hydrogen nuclei of interstitial fluid within rock samples, which properties may include porosity, permeability, recoverable fluid content, large-pore specific surface, argillaceous specific surface, or any combination or subcombination of these properties, in which DC field inhomogeneity and random phasal background jitter are used to increase data-throughput efficiency (DTE), of a measuring system comprising: (a) storing digital control codes associated with (i) control of a series of interrogation RF magnetic pulses of selected frequency duration and magnitude and (ii) generation of a plurality of time windows for detection of a plurality of NMR response signals; (b) placing the rock sample in a steady DC magnetic field having a strength of at least 1 kilogauss and an inhomogeneity of about D gauss to aid in providing a series of nuclear magnetizations build-ups associated with said interstitial fluid within said rock sample, said each nuclear magnetization having a preferential alignment parallel to said DC magnetic field; (c) subjecting said sample on a sequential basis in accordance with said control codes, to said series of RF magnetic pulses to cause reorientation of said magnetization to preferred alignments offset from said DC field, said amplitude of said interrogation pulses being greater than the variation D in strength of said DC field over the sample; (d) automatically detecting after interrogation, in accordance with said control codes, NMR responses associated with precession of said magnetization build-ups about axes substantially parallel of said DC field magnetic field within said plurality of time windows, each of said windows occurring within an interval between two of said interrogation pulses and within subintervals beginning at a fixed delayed time after cessation of each of said interrogation pulses; and (e) automatically repeating steps (c)-(d) in accordance with different digital control codes whereby a different predetermined average repetition rate for said interrogation pulses is used to obtain at least a second statistically-improved signal representing nuclear magnetization relaxation in said DC magnetic field within at least a different average time interval between said interrogation pulses, whereby flow properties of said sample can be indicated.