Accurate measures of fibre dispersion might improve tractography through voxels with bending and/or fanning configurations and also provide more accurate tissue microstructure indices. When estimated from regular diffusion MRI, however, the accuracy of the dispersion estimate depends on the accuracy of the underlying microstructural model. In this work, we find that encoding water diffusion using multiple shapes of the b-tensor leads to an accurate measurement of fibre dispersion within a single b-shell. We show that this holds for complicated sub-voxel geometries using both simulations and in vivo data.
The diffusion MRI (dMRI) signal can be modelled as the convolution of a fibre orientation distribution function (fODF) with a fibre response function. Therefore, measuring the fODF width (fibre dispersion) requires knowing the response function (diffusion anisotropy). This is usually done by either estimating it from the most anisotropic voxels1 or by assuming an explicit microstructural model2-4, whereby if the assumptions break down, estimates of fibre dispersion can be biased (Figure 1B) due to model degeneracy5,6.
These models generally only consider data acquired using the Stejskal-Tanner sequence, which is sensitive to diffusion along a single direction (linear tensor encoding). By varying the gradient waveform more generally one can create sequences sensitive to diffusion in a plane (planar encoding) or to diffusion in all directions (spherical encoding)7,8. Combining these sequences in a single b-shell allows the measurement of anisotropy experienced by water at the microscopic scale independently of the fODF (micro-anisotropy)8,9. Because micro-anisotropy determines the width of the response function, this combination of sequences should allow us to measure fibre dispersion accurately using a single b-shell (Figure 1C)11 Here we show that this is indeed the case even for voxels with complicated microstructure.
The linear, planar and spherical tensor encoding can be characterized by a b-tensor12,13:
$$\mathbf{B}_{\rm linear}=b\hat{\mathbf{g}}\cdot\hat{\mathbf{g}}^T,$$
$$\mathbf{B}_{\rm planar}=\frac{b}{2}(\mathbf{I}-\hat{\mathbf{n}}\cdot\hat{\mathbf{n}}^T),$$
$$\mathbf{B}_{\rm spherical}=\frac{b}{3}\mathbf{I},$$
where $$$b$$$ is the b-value, $$$\hat{\mathbf{g}}$$$ the diffusion gradient direction in the linear encoding, $$$\hat{\mathbf{n}}$$$ is the normal of the plane in planar encoding, and $$$\mathbf{I}$$$ is the 3x3 identity matrix. For a voxel containing multiple compartments (indexed with i) with axisymmetric Gaussian diffusion tensors the attenuation is given by13:
$$S(\mathbf{B})=\sum_{i}S_{0, i}e^{-\mathbf{B}\cdot\mathbf{D}_i}=\sum_i S_{0, i} e^{-b d_{\bot, i}} e^{-b(d_{\parallel,i}-d_{\bot,i})\hat{\mathbf{\nu}}_i\cdot \mathbf{B} \cdot \hat{\mathbf{\nu}}_i^T}$$
where $$$d_{\parallel, i}$$$/$$$d_{\bot, i}$$$ is the diffusivity along/across $$$\hat{\mathbf{\nu}}_i$$$. We assume all tensors have the same fODF described by the Bingham distribution:
$$f(\hat{\mathbf{\nu}})=\frac{1}{4\pi{}_1F_1(1/2;3/2;\mathbf{Z})}e^{-\hat{\mathbf{\nu}} \cdot \mathbf{Z} \cdot \hat{\mathbf{\nu}}^T}$$
where the Bingham matrix $$$\mathbf{Z}$$$ describes the orientation, extent, and anisotropy of the fODF and $$${}_1 F_1$$$ is a confluent hypergeometric function. The convolution of the Bingham distribution with the signal attenuation gives2:
$$S(\mathbf{B})=\sum_{i}S_{0,i}e^{-bd_{\bot,i}}\frac{{}_1F_1(1/2;3/2;\mathbf{Z}-b(d_{\parallel,i}-d_{\bot,i})\mathbf{B})}{{}_1F_1(1/2;3/2;\mathbf{Z})}$$
To achieve convergence in a single b-shell we can only fit a single compartment, which gives us an effective amplitude ($$$\overline{S_{0}e^{-bd_{\bot}}}$$$) and anisotropy ($$$\overline{d_{\parallel}-d_{\bot}}$$$) for all compartments:
$$S(\mathbf{B})=\overline{S_{0}e^{-bd_{\bot}}}\frac{{}_1F_1(1/2;3/2;\mathbf{Z}-b(\overline{d_{\parallel}-d_{\bot}})\mathbf{B})}{{}_1F_1(1/2;3/2;\mathbf{Z})}$$
Changing the b-value would alter the relative contributions ($$$S_{0,i}e^{-bd_{\bot,i}}$$$) of the various compartments and hence the effective anisotropy ($$$\overline{d_{\parallel}-d_{\bot}}$$$). We can avoid making assumptions about how anisotropy changes with b-value by fixing the b-value and only varying the shape and orientation of the b-tensor B, to probe the fODF (encoded in $$$\mathbf{Z}$$$). This allows us to measure the fODF even without an accurate model of how the contribution of multiple water compartments changes with b-value.
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