This work presents a new method for quantifying multiple-TE/two-dimensional spectroscopy data, characterized by the use of spectral priors obtained by quantum mechanical simulations and an experimentally measured lineshape distortion function derived from a set of multi-TE water spectroscopic data. Results from in vivo J-resolved spectroscopy data demonstrated the excellent fitting produced by the proposed method, and improved robustness over a standard parametric-model-based method. With further developments, such as extensions to different sequences and Cramer-Rao bound analysis, the proposed method should prove useful for a range of 2D spectroscopy experiments.
Signal Model
To address the key issues of modeling the spectral variations of individual molecules at different TEs and accounting for signal distortion for multi-TE quantification, we propose to use the following model (also considering sampling before echoes)
$$s(t,TE_i) = \sum_{m=1}^{M}a_m\phi_{m,i}(t,\tau_i)e^{-(TE_i-TE_1)/T_{2,m}}e^{-(t-\tau_i)/T_{2,m}}e^{i2\pi\delta f_m(t-\tau_i)}e^{-i\theta_{m,i}+i2\pi\Delta f_{i}t}h_i(t) + \sum_{b=1}^{B}c_b\phi_b(t,TE_i)e^{-\beta_bt}, \quad [1]$$
where $$$TE_i$$$ denotes the $$$i$$$th echo time, $$$t$$$ the free-precession time, $$$a_m$$$ the molecular concentration, and $$$\{\tau_i\}$$$ the sampling periods before echoes. Spectral priors are incorporated through the resonance structures $$$\{\phi_{m,i}(t)\}$$$ (from quantum mechanical simulations) and exponential lineshapes only dependent on molecular-specific parameters, i.e., relaxation parameters $$$T_{2,m}$$$ and frequency shifts $$$\delta f_m$$$. The additional terms $$$\theta_{m,i}$$$ and $$$\Delta f_{i}$$$ account for phase discrepancy and field shifts across TE. Finally, the time-domain envelope function $$$h(t)$$$ is used to model the experiment-dependent lineshape distortions (e.g., due to intra-voxel B0 inhomogeneity and/or eddy currents). The last summation captures the baseline with basis $$$\{\phi_b(t)\}$$$ and damping factors $$$\{\beta_b\}$$$.
Distortion Estimation
A key component in the proposed method is the determination of $$$h(t)$$$. Existing methods typically model $$$h(t)$$$ by Gaussian functions with additional phase terms, and try to jointly determine the associated nonlinear parameters from the data, increasing the number of unknowns for fitting. We propose here a different approach to address this, by acquiring a set of water spectroscopic signals with selected TEs from the same voxel (this can be done quickly since only one average per TE is needed). Specifically, we model the water data as
$$s_w(t,TE_i) = e(TE_i; T_{2,w})e^{-t/T_{2}'+i2\pi f_0t}\sum_{l=-L/2+1}^{L/2}\alpha_le^{i2\pi l\Delta ft}, \qquad\qquad\qquad\qquad\qquad\qquad [2]$$
where $$$e(TE_i; T_{2,w})$$$ captures pure $$$T_2$$$-dependent signal decay, $$$e^{-t/T_2'}$$$ and $$$f_0$$$ the exponential decay and frequency shift caused by intra-voxel B0 inhomogeneity, respectively, and the last term models the non-exponential distortion. While separating $$$e(TE_i; T_{2,w})$$$ from $$$e^{-t/T_2'}$$$ from a single FID is highly ill-posed, the problem becomes simpler with the multi-TE water data available. More specifically, the samples at echo times from the water FIDs (denoted as $$$\{s_w(t=0,TE_i)\}$$$) can be used to extract the $$$T_2$$$-decay, by interpolating $$$\{s_w(0,TE_i)\}$$$ to the FID sampling grids (e.g., using a spline kernel). This interpolation is accurate given a sufficient number of TEs and more robust than a multi-$$$T_2$$$ parametric fitting which suffers from poor-conditioning.
With $$$e(.)$$$ determined, it is incorporated into Eq. [2] for the fitting of $$$s_w(t,TE_i)$$$ to determine $$$T_2'$$$, $$$f_0$$$ and $$$\{\alpha_l\}$$$. TE-dependent $$$h(t)$$$'s were synthesized in the form of $$$e^{-t/T_{2}'}\sum\alpha_le^{i2\pi l\Delta ft}$$$ and averaged to generate the final estimate, which was then incorporated into Eq. [1] for the proposed multi-TE quantification. The fitting was done by solving a least-squares problem using a variable-projection-based algorithm.
In vivo localized J-resolved data were acquired to evaluate the proposed method. Data were acquired on a 3T scanner (Siemens Prisma) using a PRESS sequence. Water-suppressed data were acquired from 20x20x20mm3 voxels with TE=30,80,160ms1, TR=2500ms, 100 averages, 2kHz bandwidth, and 512 FID samples. The voxel location is illustrated in Fig. 1. Water data were acquired at 16 TEs ranging from 30 to 350ms (optimized by simulations of sampling a signal with 3 TE components) and TR=4s.
Figure 2 shows the processing results for the water data, particularly the successful estimation of $$$e(TE_i;T_{2,w})$$$ and $$$h(t)$$$. Figure 3(a)-(b) show the fitting results for different TEs from a representative dataset. Small residuals are observed. Separated individual metabolite components are shown in Fig. 3(d). Figure 4 compares the estimated parameters from two repeated experiments on the same subject. As can be seen, the parameters produced by the proposed method are clearly more reproducible than a standard parametric model which uses the Voigt lineshapes1.
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