A multicoil nmr data acquisition apparatus and processing method for performing three-dimensional magnetic resonance imaging in a static magnetic field without the application of controlled static magnetic field gradients. A preferred application relates specifically to the detection and localization of groundwater using the Earth's magnetic field. Multicoil arrays are used in both transmit and receive modes. and coherent data processing algorithms applied to the data to generate three-dimensional nmr spin density estimates. Disclosed are methods for acquiring nmr data using an array of at least two transmit and receive coils, and for processing such multicoil data to estimate the three-dimensional nmr spin density distributions.

Patent
   RE43264
Priority
Jul 09 2003
Filed
Mar 01 2010
Issued
Mar 27 2012
Expiry
Jul 09 2024
Assg.orig
Entity
Small
3
35
all paid
1. A method of obtaining a localized nuclear magnetic resonance Nuclear magnetic Resonance (nmr) signal from a sample a subsurface three dimensional (3D) volume in a static magnetic field using an array of two or more magnetic field transmitting coils, and an array of two or more magnetic field receiving coils, the method comprising:
a) generating a single an alternating current excitation pulse on one or more transmitting coils, each of said transmitting coils of the array, providing a spatially distinct an inhomogeneous magnetic field in the three dimensional (3D) volume;
b) acquiring nmr signals on two or more magnetic field receiving coils of the array of magnetic field coils;
c) applying a plurality of excitation pulses to each transmitting coil or combination of transmitting coils, wherein each excitation pulse has a unique pulse moment defined as the product of the pulse amplitude and pulse length, and wherein the nth pulse moment pm(n) is not equal to (2n−1)*pm(1); and repeating steps a and b using a plurality of excitation pulses, wherein the plurality of excitation pulses produce magnetic fields in the 3D volume, wherein at least one excitation pulse is produced by a transmitting coil of the array that is spatially distinct from another transmitting coil geometry or location, and wherein at least one excitation pulse comprises a pulse moment that is unique from a pulse moment of another excitation pulse, and wherein an nth pulse moment pm(n) is not equal to (2n−1)*pm(1); and
d) constructing a localized nuclear magnetic resonance nmr signal as a linear combination of nmr signals obtained using two or more transmitting coils or combinations of transmitting coils, two or more receiving coils, and two or more pulse moments for each transmitting coil excitation pulses corresponding to a plurality of different transmitting coil geometries or locations and a plurality of different pulse moments.
0. 21. A multi-channel Nuclear magnetic Resonance (nmr) data acquisition apparatus that uses an array of magnetic field coils to obtain a localized nmr signal from a three dimensional (3D) volume in a static magnetic field, comprising:
a computer;
one or more signal generators and power amplifiers configured to produce alternating current excitation pulses on one or more coils;
an array of coils, wherein:
one or more of the coils of the array are configured to produce magnetic fields in a three-dimensional (3D) volume in response to excitation pulses produced by the one or more signal generators and power amplifiers, wherein at least one excitation pulse is produced by a coil that is spatially distinct from another coil geometry or location, and wherein at least one excitation pulse comprises a pulse moment that is unique from a pulse moment of another excitation pulse, and wherein an nth pulse moment pm(n) is not equal to (2n−1)*pm(1); and
two or more of the coils of the array of coils are configured to receive nmr signals produced in the 3D volume in response to the produced magnetic fields;
a multi-channel Analog to Digital (AD) data acquisition device configured to receive nmr signals via the coils configured to receive nmr signals, convert received nmr signals to digital signals, and output the digital signals to the computer;
wherein the computer is configured to record the digital signals produced by the AD data acquisition device; and
wherein the computer is configured to construct a localized nmr signal as a linear combination of nmr signals obtained using excitation pulses corresponding to a plurality of different transmitting coil geometries or locations and a plurality of different pulse moments.
2. The method according to claim 1, wherein constructing the localized nmr signal is obtained comprises using a matched filtering data processing method comprising:
a) computing the an expected tip angle and phase of a precessing unit-valued magnetic moment at the sample a location in the 3D volume, for each applied combination a plurality of combinations of magnetic field transmitting coils coil locations and pulse moments;
b) computing the expected amplitude and phase of each a forward-modeled nmr signal, each forward-modeled signal resulting from the modeled detection of the precessing unit-valued magnetic moment at the hypothetical sample corresponding to the location by each of magnetic field receiving coils in the 3D volume, and representing said expected amplitude and phase as a complex scalar;
c) arranging the set of said complex scalar values as a vector matched filter vector h, wherein each complex scalar represents the expected amplitude and phase of the signal response for a unit valued magnetic moment at the sample location for a given combination of transmit coil or coils, receive coil, and pulse moment;
d) computing a conjugate matched filter vector h* formed as a complex conjugate value of h of the vector matched filter vector; and
e) computing the localized nmr signal s as the a linear combination of the recorded acquired nmr signals wherein each recorded signal bj is weighted by its respective nmr signals in the combination are weighted by conjugate matched filter vector coefficients hj*: s=Σjhj*bj.
3. The method according to claim 2, wherein the localized nmr signal is obtained using an adaptive filtering data processing method comprising:
a) computing a matched filter vector h according to claim 2;
b) arranging the set of recorded nuclear magnetic resonance data as a matrix b with M×L×P rows, wherein each row is the sampled nuclear magnetic resonance signal recorded at one magnetic field receiving coil for one combination of transmitting coils and pulse moment;
c) computing a data correlation matrix

RBB=BBH
 where the superscript H denotes conjugate transpose;
d) computing the inverse RBB−1 of the full-rank data correlation matrix RBB;
e) computing the adaptive filter vector m=h RBB−1/(h RBB−1 hH)1/2;
f) computing a conjugate adaptive filter vector m* formed as a complex conjugate value of m; and
g) computing the localized nmr signal s as the linear combination of the recorded nmr signals wherein each recorded signal bj is weighted by its respective conjugate adaptive filter vector coefficient mj*: s=Σjmj*bj wherein constructing the localized nmr signal further comprises applying an adaptive filtering data processing method to determine the location of an nmr signal source.
4. The method according to claim 3 2, wherein the elements of the vector matched filter vector h are equal to a fixed constant scalar value for nmr data recorded on one a first receive coil only, and wherein the elements of the vector matched filter vector h are zero for nmr data recorded on all other receive coils.
5. The method according to claim 1, wherein the localized nmr signal is obtained using a linear inverse/least-squares data processing method comprising:
a) selecting a set of discrete volume elements (voxels) that encompass the 2-D or 3-D a two-dimensional (2D) or 3D volume or object of interest in the 3D volume; and
b) developing a set of linear equations Ax=b relating a modeled response for the voxels to the nmr data; and the sampled signal arising from the unknown spin density within each individual voxel to each sample in the experimentally recorded data set comprising:
1) arranging the entire set of recorded nuclear magnetic resonance data samples as a vector b;
2) arranging the set of unknown voxel spin density values as a vector x;
3) computing each coefficient of the matrix A as a complex value describing the amplitude and phase of the recorded nmr signal that would result from the detection of a collection of precessing nuclear magnetic resonance spins, of unit spin density, contained within the hypothetical voxel corresponding to an unknown sample of x, using one particular combination of transmit coil or coils, receive coil, and pulse moment;
4) c) calculating the a set of localized nmr signals x as the a least squares solution to the system set of linear equations Ax=b, or as a regularized least squares solution to Ax=b the set of linear equations, using any mathematical algorithm that computes an estimate of the least squares solution or regularized least squares solution to the set of linear equations Ax=b.
6. The method according to claim 5, wherein the inverse or pseudo-inverse of the matrix A is computed once, and is applied sequentially to discrete time samples to obtain linear inverse/least-squares data processing method further comprises obtaining localized nmr signals on a time-sample-by-sample basis.
7. The method according to claim 5, wherein the least squares solution is calculated by one of the direct pseudo-inverse x=(AHA)−1AHb, or by the regularized direct pseudo-inverse, where small scalar values are added to the diagonal elements of A or AHA, prior to computing the inverse of(AHA) using one or more matrices describing amplitude and phase of a hypothetical nmr signal that would result from detection of a collection of precessing nmr spins, of unit spin density, contained within a hypothetical voxel.
8. The method according to claim 5, wherein the least squares solution or regularized least squares solution is calculated by a singular value decomposition method comprising:
a) calculating the singular value decomposition of the matrix A=USVH; and
b) one of calculating the least squares solution as x=V[diag (l/σj)]UHb, or calculating a weighted last squares solution, where the diagonal terms diag(l/σj) are each multiplied by a weighting factor prior to performing the matrix multiplication.
9. The method according to claim 5, wherein the least squares solution or regularized least squares solution is calculated using by a computer equipped with computer software, the software configured to use a linear iterative least squares solution algorithm comprising:
a) the gradient descent algorithm;
b) the steepest descent algorithm; or
c) the conjugate-gradient algorithm in order to process stored nmr data.
10. The method according to claim 1 wherein at least some of the nuclear magnetic resonance nmr signals result from the presence of groundwater in the 3D volume.
11. The method according to claim 1 wherein the static magnetic field is the Earth's magnetic field.
12. The method according to claim 1, wherein each recorded nuclear magnetic resonance signal is initially reduced further comprising reducing an acquired nmr signal to a single complex number by multiplying each data sample corresponding to an acquired nmr signal by the sampled an exponential function e(−j2πfnT) or the sampled exponential function e(−j2πfnT) and coherently summing the a resulting series of samples.
13. The method according to claim 1 wherein at least one of the transmitting magnetic field coils coil of the array and receiving magnetic field coils is the coil of the array are provided by a same coil, and this coil is used for the purposes of both transmitting and receiving.
14. The method according to claim 1 wherein a reduced number of transmittigg magnetic field coils and/or receiving magnetic field coils are further comprising physically displaced and additional nuclear magnetic resonance signals are recorded via the displaced coils, so as displacing a transmitting coil of the array between excitation pulses to generate a set of data equivalent to that obtained using a full set of multiple transmitting and receiving magnetic field coils.
15. The method according to claim 1, wherein each recorded nuclear magnetic resonance sample is a single sample of the discrete Fourier transform (DFT) of the sampled nuclear magnetic resonance signal further comprising applying a Discrete Fourier transform (DFT) on acquired nmr signals, and recording samples from the DFT output on a computer memory.
16. The method according to claim 1, wherein an image is computed over a 3-dimensional field of view further comprising computing a 3D image of the 3D volume.
17. The method according claim 1, wherein an image is computed over a 2-dimensional field of view further comprising computing a 2D image of the 3D volume.
18. The method according to claim 1, wherein an image is computed over a 1-dimensional field of view further comprising computing a one dimensional (1D) image of the 3D volume.
0. 19. The method according to claim 1, further comprising:
a) deploying one of more auxiliary devices to measure noise in the vicinity of the two or more magnetic field receiving coils of the array; and
b) subtracting noise from obtained nmr signals.
0. 20. The method according to claim 1, further comprising:
a) deploying one or more auxiliary devices to measure noise in the vicinity of the two or more magnetic field receiving coils of the array;
b) constructing a set of noise reference data samples {n(1)), . . . ,n(N)} from noise measurements;
c) constructing a linearly transformed surface nmr data sample X from data acquired from the two or more magnetic field receiving coils;
d) computing an estimate of a noise process on the linearly transformed surface nmr data sample X; and
e) subtracting an estimated noise sample from the linearly transformed surface nmr data sample X.
0. 22. An apparatus according to claim 21, wherein the plurality of coils comprises one or more combined transmit and receive coils.
0. 23. An apparatus according to claim 21, further comprising one or more switches configured to electronically isolate the AD data acquisition device during transmit pulses produced by the one or more signal generators and power amplifiers.
0. 24. An apparatus according to claim 21, further comprising one or more tuning circuits coupled to one or more of the coils in the array of coils.
0. 25. An apparatus according to claim 21, further comprising one or more pre-amplifiers configured to receive nmr signals via the coils configured to receive nmr signals, amplify the nmr signals, and output the amplified nmr signals to the AD data acquisition device.
0. 26. An apparatus according to claim 21, wherein the computer is configured to process recorded digital signals using a matched filtering data processing method.
0. 27. An apparatus according to claim 21, wherein the computer is configured to process recorded digital signals using an adaptive filtering data processing method.
0. 28. An apparatus according to claim 21, wherein the computer is configured to process recorded digital signals using a linear inverse/least-squares data processing method.
0. 29. An apparatus according to claim 21, wherein the computer is configured to process recorded digital signals using synthetic aperture processing.
0. 30. An apparatus according to claim 21, wherein the computer is configured to generate a one dimensional (1D), two dimensional (2D), or 3D image of at least a portion of the 3D volume.
0. 31. An apparatus according to claim 21, further comprising one or more auxiliary devices configured to measure noise in the vicinity of the coils of the array configured to receive nmr signals.
0. 32. An apparatus according to claim 31, wherein the one or more auxiliary devices comprise an auxiliary surface coil.
0. 33. An apparatus according to claim 31, wherein the apparatus is configured to subtract noise from obtained nmr signals.
0. 34. An apparatus according to claim 31, wherein the apparatus is configured to:
construct a set of noise reference data samples {n(1)), . . . ,n(N)} from noise measurements;
construct a linearly transformed surface nmr data sample X from data acquired from the coils of the array configured to receive nmr signals;
compute an estimate of a noise process on the linearly transformed surface nmr data sample X; and
subtract an estimated noise sample from the linearly transformed surface nmr data sample X.
0. 35. The method according to claim 1 further comprising physically displacing a receiving coil of the array of coils between measurements to synthesize a larger receive array.

This application is a continuation-in-part of International Application No. PCT/US2004/021911, filed Jul. 9, 2004, which designates the United States, and which claims the benefit of to provisional application No. 60/485,689, filed on Jul. 9, 2003.

Multicoil MRI has been used for many years to non-invasively examine the nuclear magnetic resonance (NMR) spin density distribution within three dimensional objects or volumes. Typically, using existing MRI data acquisition methods and data processing methods, the object under investigation is placed in a static magnetic field B0 and is energized by an alternating magnetic field B1. The frequency of the alternating magnetic field B1 is selected as the Larmor frequency (the natural nuclear magnetic resonant frequency) for the atomic species of interest. The Larmor frequency depends upon the magnitude of the static field B0, among other factors. A number of well-known MRI applications have detected the hydrogen proton spin density, although it is possible to image carbon, potassium and other atomic species with certain nuclear spin properties.

Typically, using existing MRI data acquisition methods and data processing methods, magnetic field gradients are applied across the object under investigation, either during or after the application of the alternating field B1. These magnetic field gradients cause the frequency of the NMR signal to vary in a predictable way along the various spatial dimensions of the object under investigation. Thus, in the prior state of the art of MRI, spatial localization is accomplished by frequency and/or phase encoding of the object through the application of controlled magnetic field gradients.

Some existing MRI devices are designed to use multiple coils during data acquisition, and some conventional MRI data processing methods exploit the differences between the individual coil fields to enhance the spatial resolution and quality of the NMR image. See for example U.S. Pat. No. 6,160,398. However, all existing MRI devices, MRI data acquisition methods and MRI data processing methods derive some or all of the spatial information required for imaging in three dimensions through the application of magnetic gradient fields.

While existing MRI devices, data acquisition methods and data processing methods may be suitable for the particular purpose to which they address, they are not as suitable for performing three dimensional magnetic resonance imaging in a static magnetic field without the application of controlled static magnetic field gradients.

A primary limitation of existing MRI devices and methods is the requirement to generate and control gradients in the static field B0. The generation and control of such gradients requires specially designed gradient field coils, and these coils are typically only effective when employed in certain constrained geometries. For example, in medical MRI, a great deal of research has been undertaken to design and construct the gradient coils for specific MRI scanner designs, and the gradient coil assemblies represent a significant portion of the scanner's expense. Most conventional MRI scanners use gradient coils that surround the object under investigation in order to produce approximately linear field gradients.

For many potential applications of three-dimensional MRI, the requirement to generate and control static field gradients is either impractical or prohibitively expensive. For example, in the investigation of subsurface groundwater distributions via surface coil NMR measurements, the generation of significant gradients in the Earth's magnetic field at operationally significant depths would require large amounts of power and complex arrays of magnetic field antennae. The imaging of other large fixed objects, such as bridge supports and building foundations, is similarly constrained by power requirements and the difficulty in generating and controlling static field gradients in three dimensions. Other potential applications of MRI, such as industrial non-destructive evaluation of raw materials, are not presently conunercially viable due to the expense and geometrical constraints associated with conventional gradient-based MRI scanners.

Surface NMR data acquisition methods and data processing methods have been used for many years to detect and localize subsurface groundwater. The existing state of the art in surface NMR utilizes a single surface coil to generate the alternating B1 field. The B1 field is transmitted with various levels of energy, and the measured NMR signals received on the same coil or a single separate coil are mathematically processed to estimate a profile for the groundwater distribution in one dimension only: depth. While existing surface NMR devices, data acquisition methods and data processing methods may be suitable for the particular purpose to which they address, they are not as suitable for performing three dimensional magnetic resonance imaging in a static magnetic field without the application of controlled static magnetic field gradients. Many surface NMR techniques can produce, at best, an estimate of the 1-dimensional groundwater density profile directly beneath the coil. These 1-D profile estimates are subject to a variety of errors stemming from the use of a single surface coil, and inaccurate 1-D models of the coil fields and water density profiles.

In recent years, single-coil surface NMR instruments have been developed and commercialized, and surface NMR data processing methods have been developed to characterize the distribution of groundwater in one or two dimensions. The first working surface NMR instrument was developed in the U.S.S.R. as described by Semenov et al. in USSR inventor's certificate 1,079,063, issued in 1988. The existing state of the art in surface NMR, epitomized by the commercial “Numis” brand instrument, utilizes a single surface coil to generate the alternating B1 field. The B1 field is transmitted with various levels of energy, and the measured NMR signals received on the same surface coil or a single separate surface coil are mathematically processed to estimate a profile for the groundwater distribution in one dimension only: depth. A commonly employed one-dimensional surface NMR profiling is described by Legchenko and Shoshakov in “Inversion of surface NMR data” appearing in Geophysics vol. 63: 75-84 (1998), incorporated hereinto by reference.

Presently available 1-D profile estimation techniques, which are based on single coil surface NMR systems, rely on a single measurement variable; the transmitted pulse energy and its relation to tip angle, to estimate a water density profile in depth. The NMR signal amplitude at a given point in space is a sinusoidal function of the flip angle at that location. Present 1-D inversion techniques measure the NMR signal using different transmit pulse energy levels, and then fit the set of NMR amplitudes to a simplified 1-D model. To make the inversion tractable, the coil vector field lines are assumed to be parallel and confined to a cylinder directly beneath the coil, and the water density profile is assumed to vary in one dimension only.

Reliance on one dimensional modeling according to the prior art therefore engenders certain deficiencies. A first fundamental problem is that the coil field lines are very different from the assumed cylindrical model over large portions of the investigation space. The generated signal depends upon the angle between the earth's vector field and the coil's vector field. A second fundamental problem is the assumption that the water density profile varies in one dimension only. Three-dimensionally variant aquifers, which are common in nature, cannot be adequately characterized using simple 1-D models. A third fundamental problem is that even if accurate coil field models were employed and 3-D water distributions were allowed, the resulting inversion would suffer from ambiguities. The integrated NMR signal depends on the 3-D distribution of water, the coil field lines, the Earth's field direction, and the transmitted pulse energy. Varying the pulse energy alone does not provide enough information to unambiguously solve the 3-D inversion problem.

In recognition of the limitations, ambiguities and potential errors imposed by the use of a single surface coil, other researchers have investigated the possibility of multi-dimensional surface NMR investigation using one or more laterally displaced surface coils. Hertrich and Yaramanci presented a three dimensional mathematical kernal function for the surface NMR signal source in “Surface-NMR with spatially separated loops—investigations on spatial resolution” appearing in the 2nd International Workshop on the Magnetic Resonance Sounding method applied to non-invasive groundwater investigations (19-21 Nov. 2003), incorporated herein by reference. Warsa, Mohnke and Yaramanci presented a discrete approximation of a 3-D model for the surface NMR signal source in “3-D modeling and assessment of 2-D inversion of surface NMR” appearing in the 2nd International Workshop on the Magnetic Resonance Sounding method applied to non-invasive groundwater investigations (19-21 Nov. 2003), also incorporated herein by reference. Although these references are useful in the development of the present invention, they do not describe a practical method for processing multi-coil surface NMR data into useful multi-dimensional estimates of the subsurface liquid distributions, and these references explicitly acknowledge the absence of such a method.

It is also recognized that electromagnetic field noise places another limitation on the utility and reliability of the prior state of the art in surface NMR. A variety of noise processes limit the ability to detect and localize groundwater using surface NMR measurements. Prior attempts to mitigate such noise have been limited to temporal processing of the raw data from a single coil. The existing prior art in this area is described by Legchenko in “Industrial noise and processing of the magnetic resonance signal” appearing in the 2nd International Workshop on the Magnetic Resonance Sounding method applied to non-invasive groundwater investigations (19-21 Nov. 2003), incorporated herein by reference. Temporal processing methods, such as narrowband filtering of the surface NMR signal, may distort the NMR signal itself and are ineffective when the frequency band of the noise process coincides with the desired surface NMR signal.

In view of the foregoing deficiencies inherent in the known types of multicoil NMR data acquisition methods and data processing methods now present in the prior art, the present invention provides new multicoil NMR data acquisition and processing methods wherein the same can be utilized for performing three dimensional magnetic resonance imaging in a static magnetic field without the application of controlled static magnetic field gradients.

The general purpose of the present invention, which will be described subsequently in greater detail, is to provide a new multicoil NMR data acquisition and processing method that has many of the advantages of the multicoil NMR data acquisition methods and data processing methods mentioned heretofore and many novel features that result in a new multicoil NMR data acquisition and processing method which is not anticipated, rendered obvious, suggested, or implied by any of the prior art multicoil NMR data acquisition methods and data processing methods, either alone or in any combination thereof.

To attain this, an embodiment of the present invention generally comprises a method for acquiring NMR data using an array of two or more transmit coils and two or more receive coils, and a method for processing such multicoil data to estimate the three-dimensional NMR spin density distribution within the object or volume under investigation. Features of the embodiment include a multicoil NMR data acquisition method, which utilizes multiple coil arrays in both transmit mode and receive mode, and which does not involve the generation or control of gradients in the static magnetic field; an imaging method for processing the data acquired via the multicoil surface NMR data acquisition method, which yields a three-dimensional estimate of the NMR spin density distribution; a noise cancellation method for processing the data acquired by the multi-coil surface NMR data acquisition method, which reduces undesired noise in the raw data and in the resulting three-dimensional estimate of the NMR spin density distribution.

The multicoil NMR data acquisition method uses an array of at least two transmit coils, and at least two receive coils. A single multi-coil FID measurement is recorded by driving the transmit coils with a current pulse at the Larmor frequency of the target, and after a short delay, recording the resulting NMR free induction decay signal for each of the receive coils. A series of independent measurements are obtained by using unique combinations of relative amplitudes and/or phases on the transmit coils, and unique total transmitted energy levels. The use of multi-coil arrays in both the transmit and receive modes introduces a unique dependence between the acquired set of signals generated by an isolated point source in space and the vector fields of the various coils relative to that point in space. The variance among the vector coil fields over the three-dimensional imaging volume makes it possible to isolate and locate signal sources in three dimensions.

The imaging method embodiment comprises specific data processing methods for processing NMR data acquired via the multicoil NMR data acquisition arrangement: a matched filtering data processing method, an adaptive filtering data processing method, and a linear inverse/least-squares data processing method. These data processing methods yield three-dimensional estimates of the NMR spin density distribution of the target. The data processing methods also yield estimates of the time-domain NMR signal processes emanating from discrete locations in the volume. These time-domain signal estimates can be further processed using previously developed analysis techniques to yield additional information on the physical properties of the materials under investigation.

The noise cancellation method embodiment comprises specific data processing methods for processing surface NMR data acquired via the multicoil surface NMR data acquisition arrangement: a noise cancellation data acquisition method which utilizes one or more reference measurements to estimate the unwanted noise process, and a noise cancellation data processing method which adaptively estimates and subtracts the noise process from surface NMR data.

The invention is not limited in its application to the details of construction and to the arrangements of the components set forth in the following description or illustrated in the drawings. The invention is capable of other embodiments and of being practiced and carried out in various ways. Also, it is to be understood that the phraseology and terminology employed herein are for the purpose of the description and should not be regarded as limiting.

Various other objects, features and attendant advantages of the present invention will become fully appreciated as the same becomes better understood when considered in conjunction with the accompanying drawings, in which like reference characters designate the same or similar parts throughout the several views, and wherein:

FIG. 1 is a block diagram of a multi-channel NMR data acquisition apparatus that uses separate coils for transmit and receive functions.

FIG. 2 is a block diagram of a multi-channel NMR data acquisition apparatus that uses the same array of coils for transmit and receive functions.

Referring for example to FIG. 3, coils which may be, e.g., combination transmit and receive coils, are arranged on a surface in the vicinity of a subsurface 3D volume.

  • 4. Subtract the estimated noise sample Q from the linearly transformed surface NMR data sample X:
    Y=X−Q
    Embodiments and Variations of the Noise Cancellation Method:
  • A first embodiment of the multicoil noise cancellation method uses one or more auxiliary surface coils to measure noise processes in the vicinity of the multicoil surface NMR data acquisition experiment.

    A second embodiment of the noise cancellation method uses correlation cancellation as the mathematical basis for estimating the linear coefficients {α(1), . . . , α(N)}. Correlation cancellation is well known to those versed in the arts of signal processing methods, and produces a set of coefficients {α(1), . . . , α(N)} that minimizes the mean squared value of the residual Y. There are a large number of direct, block-based, and iterative mathematical algorithms for estimating the linear coefficients {α(1), . . . , α(N)} and minimizing the mean squared value of the residual Y. Several implementations of such correlation cancellation algorithms are described by S. Haykin in “Adaptive Filter Theory” Prentice Hall, Upper Saddle River, N.J., 1996, and incorporated hereinto by reference.

    A preferred embodiment of the noise cancellation method constructs the NMR data sample X as a sample of the discrete Fourier transform of a raw surface NMR measurement sequence from a single surface coil. A modification of this embodiment also constructs noise reference data samples {n(1), . . . , n(N)} as samples of the discrete Fourier transform(s) of the raw data sequence(s) measured via the auxiliary electrical, magnetic, or electromagnetic measurement device(s).

    The present invention specifies three different methods for mathematically processing the multicoil NMR data, acquired according to the multicoil NMR data acquisition method, to isolate the NMR signals arising from different regions of the three-dimensional volume of investigation. The first method is an application of the principle of matched filtering (correlation) for multicoil NMR imaging. The second method is an application of adaptive filtering for multicoil NMR imaging. The third method is the application of linear inverse/least squares solution techniques for multicoil NMR imaging.

    In all three data processing methods, the data consists of a set of L×M×P sampled NMR signals, where L is the number of different transmit array combinations, M is the number of receive coils, and P is the number of different total energy levels transmitted for each transmit array combination. If each NMR signal consists of K time-domain data samples, then the entire data set consists of K×L×M×P data samples.

    Detailed Description of the Matched Filtering Data Processing Method:

    The generic method of mathematical correlation is familiar to those skilled in the arts of math and science. The embodiment described in the following paragraphs includes a specific formulation of the correlation method for estimating the three-dimensional NMR spin density distribution, given a set of NMR data acquired using the multicoil NMR data acquisition method.

    The relative NMR spin density is estimated on a point-by-point basis, throughout the three-dimensional volume of interest. The volume may be sampled uniformly or non-uniformly, depending on the requirements of the application. For each hypothetical sample location (a location in the volume of interest), the relative NMR spin density is estimated as follows:

      • 1. Compute the hypothetical initial amplitudes and phases, for the entire set of L×M×P sampled NMR signals, that would occur if a standardized unit volume of NMR spin density centered at the hypothetical sample location was subjected to the same multicoil NMR data acquisition procedure that is used to generate the data. For a single sampled NMR signal, this is accomplished by the following procedure, which will be understood by those who are skilled in the art of NMR processes and antenna field theory:
        • ii) Compute the phase of the precessing magnetic moment at the hypothetical sample location, relative to a fixed reference phase. The phase of the precessing magnetic moment is determined by the orientation of the transverse component of the transmitted B1 field at the hypothetical sample location. (In this discussion, the transverse component of any field is the component of the field that is perpendicular to the static field B0.)
        • iii) Compute the phase of the received NMR signal due to the assumed precessing magnetic moment at the hypothetical sample location. The phase of the received NMR signal is determined by the orientation of the transverse component of the receive coil at the hypothetical sample location, the phase of the precessing magnetic moment, and the fixed phase reference.
        • iv) Compute the tip angle of the precessing magnetic moment at the hypothetical sample location. The tip angle is determined by the total energy contained in the transverse field component of the transmitted pulse, at the hypothetical sample location. For a single transmit pulse, the tip angle is generally a linear function of the energy contained in the transverse component of the field at the sample location. If multiple transmit pulses are used, the tip angle depends on the entire pulse train.
        • v) Compute the initial amplitude of the received NMR signal. The initial amplitude of the received NMR signal depends on the magnitude of the transverse component of the receive coil field at the hypothetical sample location, as well as the tip angle of the precessing magnetic moment. The initial amplitude of the received NMR signal is a sinusoidal function of the tip angle, with maxima at +90 degrees and −90 degrees, and minima at 0 degrees and +180 degrees.
        • vi) The entire set of L×M×P initial received amplitude and phase values may be arranged as a L×M×P vector of complex numbers, where each complex number represents the hypothetical initial amplitude and phase of one of the NMR signals for the hypothetical sample location. This vector represents a filter vector that is matched to the expected set of initial amplitudes and phases for a unit volume of NMR spin density at the hypothetical sample location. This matched filter vector is referred to as h(x,y,z) where the subscript (x,y,z) denotes the hypothetical sample location in Cartesian coordinate space.
      • 2. Compute the 2-norm ∥h(x,y,z)∥ of the matched filter vector h(x,y,z).
      • 3. Normalize the matched filter vector h(x,y,z) to unit energy by dividing it, sample-by-sample, by its 2-norm:
        hn(x,y,z)=h(x,y,z)∥h(x,y,z)∥.
      • 4. Multiply each of the measured NMR signals by the associated initial amplitude sample from the normalized matched filter vector hn(x,y,z).
      • 5. Apply a constant phase shift to each of the measured NMR signals equal to the negative of the associated phase sample from the normalized matched filter vector hn(x,y,z).
      • 6. Coherently sum, on a time sample-by-sample basis, all of the amplitude-adjusted phase-shifted versions of the measured NMR signals. The resulting composite sampled NMR signal s(x,y,z) is the estimated NMR signal for the hypothetical sample location (x,y,z).
      • 7. The relative NMR spin density at the location (x,y,z) is estimated as the initial value of s(x,y,z) divided by ∥h(x,y,z)∥.

    Features of this technique are the construction of the matched filter h(x,y,z) and its application to isolate the NMR signal s(x,y,z) arising from a given location (x,y,z) within the volume. Other relevant sample properties, such as the decay constant at location (x,y,z), can be estimated from the composite NMR signal s(x,y,z) using existing signal processing methods, which are familiar to those skilled in the art of NMR.

    Embodiments Using the Matched Filtering Data Processing Method:

    In a preferred embodiment using the matched filtering data processing method, the phase shift is implemented by applying a time shift to each measured NMR signal such that the signal phase at the Larmor frequency is shifted by the specified amount. In another variation, the time shift is accomplished in the Fourier domain by computing the discrete Fourier transform of the measured NMR signal, then applying a linear phase shift in the Fourier domain, and then computing the inverse Fourier transform to produce the time-shifted version of the measured NMR signal.

    In another preferred embodiment using the matched filtering data processing method, the measured NMR signals are de-modulated by multiplication with the sampled exponential function e(−j2nfnT), where f is the Larmor frequency. In this embodiment, the measured NMR signals are transformed to complex valued sequences centered approximately at DC. In this variation, the phase shift of the matched filter is applied directly to each complex NMR signal by multiplying each time-domain sample by e(jφ) or e(−jφ), where φ is phase of a matched filter for that particular NMR signal.

    In yet another embodiment using the matched filtering data processing method, each measured NMR signal is initially reduced to a single complex number by multiplying it by the sampled exponential function e(−j2nfnT) and coherently summing the series of samples (or equivalently, computing the discrete Fourier transform of the series and selecting the DFT sample at the Larmor frequency). This complex number is an estimate of the amplitude and phase of the NMR signal content at the Larmar frequency. In this embodiment, the matched filter phase shift is applied by multiplying the single complex number representing each measured NMR signal by e(jφ) or e(−jφ), where φ is phase of a matched filter for that particular NMR signal.

    In still another embodiment using the matched filtering data processing method, the discrete sine transform is used to execute the portion of the matched filtering relating to the sinusoidally-dependent NMR tip angle response.

    Detailed Description of the Adaptive Filtering Data Processing Method:

    The generic method of adaptive filtering is familiar to those persons skilled in the art of math and signal processing. Embodiments of the invention use a specific formulation of the adaptive filtering method for estimating the three-dimensional NMR spin density distribution, given a set of NMR data acquired using the multicoil NMR data acquisition method.

    The relative NMR spin density is estimated on a point-by-point basis, throughout the three-dimensional volume of interest. The volume may be sampled uniformly or non-uniformly, depending on the requirements of the application. For each hypothetical sample location (a location in the volume of interest), the relative NMR spin density is estimated as follows:

      • 1. Arrange the entire set of measured NMR data as a matrix B with K columns and L×M×P rows. Each row is one measured, sampled NMR signal, corresponding to one particular combination of transmit array combination, receive coil(s) and transmit energy. The column indices correspond to time samples.
      • 2. Compute the data correlation matrix for the measured data matrix:
        RBB=BBH
      •  where the superscript H denotes conjugate transpose.
      • 3. If the correlation matrix RBB is less than full rank, preprocess RBB so that it becomes invertible (full rank). One method for making RBB invertible is to average the all the matrix elements along each diagonal.
      • 4. Compute the inverse RBB−1 of the full-rank data correlation matrix RBB.
      • 5. For each hypothetical sample location (x,y,z), compute the normalized matched filter vector hn(x,y,z) as previously described in the detailed description for the matched filtering method (1, i-v).
      • 6. Compute the adaptive filter m(x,y,z) as
        m(x,y,z)=hn(x,y,z)RBB−1l(hn(x,y,z)RBB−1 hn(x,y,z)H)1/2.
      • 7. Multiply each of the measured NMR signals by the associated initial amplitude sample from the adaptive filter vector m(x,y,z).
      • 8. Apply a constant phase shift to each of the measured NMR signals equal to the negative of the associated phase sample from the adaptive filter vector m(x,y,z).
      • 9. Coherently sum, on a time sample-by-sample basis, all of the amplitude-adjusted phase-shifted versions of the measured NMR signals. The resulting composite sampled NMR signal s(x,y,z) is the estimated NMR signal for the hypothetical sample location (x,y,z).

    Features of this technique are the construction of the adaptive filter m(x,y,z), and its application to isolate the NMR signal s(x,y,z) arising from a given location (x,y,z) within the volume. Other relevant sample properties, such as the decay constant at location (x,y,z), can be estimated from the composite NMR signal using existing signal processing methods, which are familiar to those skilled in the art of NMR.

    The difference between the normalized matched filter hn(x,y,z) and the adaptive filter m(x,y,z) is that the matched filter is optimized for detecting the NMR signal emanating from location (x,y,z) in a background of random white noise, while the adaptive filter is optimized for isolating the NMR signal emanating from location (x,y,z) when the interference signal exhibits a correlated structure in the measured data.

    Embodiments Using the Adaptive Filtering Data Processing Method:

    In a preferred embodiment using the adaptive filtering data processing method, the phase shift is implemented by applying a time shift to each measured NMR signal such that the sigual phase at the Larmor frequency is shifted by the specified amount. In another variation, the time shift is accomplished in the Fourier domain by computing the discrete Fourier transform of the measured NMR signal, then applying a linear phase shift in the Fourier domain, and then computing the inverse Fourier transform to produce the time-shifted version of the measured NMR signal.

    In another preferred embodiment using the adaptive filtering data processing method, the measured NMR signals are de-modulated by multiplication with the sampled exponential function e(−j2nfnT), where f is the Larmor frequency. In this embodiment, the measured NMR signals are transformed to complex valued sequences centered approximately at DC. In this variation, the phase shift of the adaptive filter is applied directly to each complex NMR signal by multiplying each time-domain sample by e(jφ) or e(−jφ), where φ is phase of adaptive filter for that particular NMR signal.

    In yet another embodiment using the adaptive filtering data processing method, each measured NMR signal is initially reduced to a single complex number by multiplying it by the sampled exponential function e(−f2πfnT) and coherently summing the series of samples (or equivalently, computing the discrete Fourier transform of the series and selecting the DFT sample at the Larmor frequency). This complex number is an estimate of amplitude and phase of the NMR signal content at the Larmor frequency. In this embodiment, any time-domain envelope information, such as the exponential decay rate, is lost. In this embodiment, the adaptive filter phase shift is applied by multiplying the single complex number representing each measured NMR signal by e(jφ) or e(−jφ), where φ is phase of adaptive filter for that particular NMR signal.

    Detailed Description of the Linear Inverse/Least-Squares Data Processing Method:

    The generic method of computing a solution to a set of linear equations is familiar to those persons skilled in the art of math and science. Embodiments of the invention employ a specific formulation of the linear inverse/least squares solution technique for estimating the three-dimensional NMR spin density distribution, given a set of NMR data acquired using the multi-channel data acquisition method.

    The linear inverse/least-squares data processing method for estimating the 3-D NMR spin density from a set of multichannel NMR data is implemented as follows:

      • 1. Select a set discrete volume elements (voxels) that encompass the 3-D volume or object of interest. The voxel sizes and shapes may be uniform (i.e. cubes of fixed dimension), variable, or arbitrary.
      • 2. Develop a set of linear equations Ax=b relating the unknown sampled NMR signal arising from the spin density within each voxel, to each sample in the measured data set. This may be accomplished as follows:
        • a. Model the sampled NMR signal source in each voxel as a set of time-domain samples. The NMR signal source in each voxel has an unknown initial amplitude that is dependent on the volume contained by the voxel and the NNW spin density within the voxel. The NMR signal source also has an unknown initial phase and unknown time-domain modulation. The phase and time domain modulation (including decay rates) are characteristic properties the material within each voxel.
        • b. Compute the coefficients for the set of linear equations relating the unknown NMR signal source samples for each voxel to the measured data samples. These coefficients depend on the amplitudes and phases of the transverse magnetic fields of the receive coils at each voxel, and the sequence of applied transverse B1 pulse energies at each voxel. The linear transform coefficients can be calculated using the description for the matched filtering method (1. i-v), along with a model for the absolute initial amplitude of the received signal based on the dimension of each voxel.
        • c. Organize the system of linear equations as a matrix equation:
          Ax=b
        •  where x is the vector of unknown NMR signal source samples (N time-domain samples for each voxel), b is the vector of measured NMR data samples, and A is the matrix of coefficients relating the unknown voxel-specific time-domain samples x to the measured NMR data samples b.
      • 3. Compute the least squares solution to Ax=b, or a regularized version of the least squares solution to Ax=b. There are many possible methods for computing the least squares solution or a regularized least squares solution to a set of linear equations. Thus, any mathematical algorithm that computes an estimate of the least squares solution or regularized least squares solution to the set of linear equations Ax=b is considered an appropriate means for solving the equation. Specific embodiments are described hereinafter.
        Embodiments Using the Linear Inverse/Least-Squares Data Processing Method:

    In a preferred embodiment using the linear inverse/least-squares data processing method, the least squares solution x is computed directly using via the least squares pseudo-inverse:
    x=(AHA)−1AHb
    where the superscriptH indicates conjugate transpose. In a preferred variation of this embodiment, the least squares solution is regularized by adding a constant scalar value to the diagonal elements of A or AHA, prior to computing the inverse of (AHA).

    In another preferred embodiment using the linear inverse/least-squares data processing method, the least squares solution is computed by first computing the singular value decomposition of A as
    A=USVH,
    where the columns of V are an orthonormal set of basis vectors for AHA and the elements wj of the e diagonal matrix S contains the positive square roots of the eigen values of AHA, and then computing the least squares solution as:
    x=V[diag(l/wj)]UHb.
    In a preferred variation of this embodiment, the least squares solution is regularized by weighting the orthogonal solution components such that the solution components generated from columns V with large associated singular values (wj) are emphasized more than the solution components generated from columns of V with small associated singular values.

    In yet another preferred embodiment using the linear inverse/least-squares data processing method, the least squares solution is computed using a linear iterative algorithm. Such linear iterative solution techniques include, but are not limited to: the Gradient Descent algorithm, the Steepest Descent algorithm, and the Conjugate Gradient algorithm. In a preferred variation of this embodiment, the least squares solution is regularized by terminating the iteration prior to its final convergence to the least squares solution.

    In still another embodiment using the linear inverse/least-squares data processing method, each measured NMR signal is initially reduced to a single complex number by multiplying it by the sampled exponential function e(−f2nfnT) and coherently summing the series of samples (or equivalently, computing the discrete Fourier transform of the series and selecting the DPT sample at the Larmor frequency). This complex number is an estimate of the amplitude and phase of the NMR signal content at the Larmor frequency. In this embodiment, any time-domain envelope information, such as the exponential decay rate, is lost. In this embodiment, the solution x consists of complex samples, where each sample represents the amplitude and phase of the NMR signal source for a given voxel.

    While the invention comprises at least some of the previously described features in various combinations, a better understanding of the invention can be ascertained by reviewing the field implementation of many of these features. Thus, the general procedure for acquiring and processing NMR data using this invention consists of: (1) hardware set-up, (2) data acquisition, (3) data processing.)

      • 1) Hardware set-up preferably comprises arranging the transmit coils and receive coils in a pattern near or around the object or volume of interest, and arranging the other acquisition hardware so as not to interfere with the data collection procedure. The coils may be arranged to maximize coverage of the object or volume of interest, and/or to maximize the diversity of coil field patterns incident across the object or volume of interest. Furthermore, the coil arrays may be arranged to minimize mutual coupling between coils. In addition, the layout of the coil arrays may be accomplished with the aid of numerical modeling software to optimize the resulting image quality for each application. Other acquisition devices should be arranged so as not to produce undue electrical or magnetic interference that would degrade the quality of the recorded NMR data.
      • 2) Data acquisition preferably comprises transmitting specified magnetic pulse trains at the Larmor frequency, using at least two transmit coils, and recording the subsequent NMR signals from at least two receive coils. Data are recorded, digitized and stored on appropriate media as the data acquisition progresses.
      • 3) Data processing preferably comprises executing computer software that retrieves the stored NMR data and processes it using one of the three data processing methods described herein so as to estimate the NMR spin density distribution and other material properties within the three-dimensional volume. Data processing may be performed entirely after all the NMR data for a given investigation have been acquired and stored. Alternately, data processing may be performed intermittently, in parallel with the data acquisition procedure, as partial NMR data becomes available.

    With respect to the above description then, it is to be realized that the optimum dimensional relationships for the parts of the invention, to include variations in size, materials, shape, form, function and manner of operation, assembly and use, are deemed design and optimization considerations readily apparent and obvious to a person skilled in the art, and all equivalent relationships to those illustrated in the drawings and described in the specification are intended to be encompassed by the present invention.

    Therefore, the foregoing is considered as illustrative only of the principles of the invention. Further, since numerous modifications and changes will readily occur to those skilled in the art, it is not desired to limit the invention to the exact construction and operation shown and described, and accordingly, all suitable modifications and equivalents may be resorted to, falling within the scope of the invention.

    Walsh, David O.

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