Christof Böhm1, Sophia Kronthaler1, Maximilian N. Diefenbach1,2, Jakob Meineke3, and Dimitrios C. Karampinos1
1TUM, Munich, Germany, 2Division of Infectious Diseases and Tropical Medicine, University Hospital, LMU, Division, Munich, Germany, 3Philips Research, Hamburg, Germany
Synopsis
Body QSM relies on accurate magnetic field-mapping.
A well-established water–fat voxel
signal model with shared $$$R_2^*$$$ has successfully
been used for body QSM based on multi-echo
data at conventional echo times. However,
when UTE echoes are recorded to obtain
field-map information in previously unavailable
MR signal voids, such as trabecular bone,
the above water–fat model is no longer accurate.
Therefore a joint 2-signal-model fitting
using graph-cuts is proposed and applied. Further,
this work demonstrates the importance
of UTE echoes to obtain correct susceptibility
values of cortical bone and more importantly,
for bone marrow.
Purpose
The non-invasive measurement of bone density is
strongly relevant in the assessment of osteoporotic
fracture risk1. Quantitative susceptibility mapping (QSM) has been proposed for measuring bone density due to the diamagnetic
properties of the trabecular bone matrix2,3,4.
Previous reports on bone QSM include susceptibility
measurements for trabecularized bone marrow using conventional echo times (TE)2,3 and for cortical-bone
using ultra-short echo times (UTE). Not accounting
for the signal from the cortical-bone shell around the bone marrow might
affect the bone marrow susceptibility estimation, especially
next to cortical-bone surfaces perpendicular
to the main magnetic field $$$B_0$$$5. To recover the signal
from the cortical-bone UTE need to
be acquired. Using both UTE and conventional TE, the analysis of multiecho
gradient echo data requires the appropriate signal
modeling7 and should account for
different the T2* decay effects between cortical-bone
and other tissues6. Here, we develop a signal model for analyzing multiecho
data acquired at both UTE and conventional TE and characterize the importance
of recovering signal from cortical-bone regions using UTE for bone marrow QSM.Methods
Simulation
To investigate the importance of UTE in bone-QSM, a simulation of a numerical hollow-cylinder-phantom and a simulation based on an in-vivo cortical-bone structure were set-up. The cylinder was homogeniously
assigned with a diamagnetic susceptibility value of $$$-2\:$$$ppm. Within the hollow cylinder the susceptibility was set to $$$0.6\:$$$ppm to mimic bone
marrow susceptibility. The susceptibility of the hollow-cylinder was
forward-simulated for different angles with respect to $$$B_0$$$ to a field-map by convolution
with the dipole-kernel in $$$k$$$-space. The field-map
was inverted to a susceptibility-map using the closed-form $$$\ell_2$$$-regularized dipole inversion method. To
simulate the difference between UTE and non-UTE
field-map information, the inversion was
performed once with known field-map values on the
cylinder and once with these values
set to zero. A second more realistic simulation
was set-up by segmenting the cortical-bone structure
of the femur of an in-vivo scan and the above pipeline was similarly applied.
In-vivo measurements
One scan of a femur of a healthy volunteer was performed on a
3$$$\:$$$T scanner (Ingenia/Philips Healthcare/Best/Netherlands). A 3D-UTE
sequence was used with stack-of-stars center-out
radial acquisition and phase-encoding in the third
cartesian dimension. After the non-selective hard-pulse a
variable delay was introduced before the start of
the readout. All TEs of one spoke were acquired
before the spoke was rotated and the order of
the TEs was randomized9as depicted in Fig.1. The imaging parameters were set to TE$$$=0.19,0.24,0.34,0.54,0.74,1.29,2.39,3.49,4.59,5.69,6.79$$$ms, orientation=axial, FOV=$$$155\times{155}\times{210}\:$$$mm$$$^3$$$ and acquisition voxel size =$$$1.4\times{1.4}\times{1.5}\:$$$mm$$$^3$$$, SENSE-factor:R=2.
Signal Modeling
First, field-mapping was performed using a single-min-cut graph-cut algorithm10,11 and a voxelwise
method12. A non-UTE field-map was created
using the above mentioned graph-cut with only the later echoes of the acquisition (TE$$$=1.29,2.39,3.49,4.59,5.69,6.79\:$$$ms) and a fat spectrum
with 10 spectral peaks specific to bone marrow13.
Second, field-mapping was performed accounting for
the different signal behaviour of UTE echoes using the
signal model proposed in7 for UTE cortical-bone
imaging. Third, a VARPRO formulation is proposed to perform
the $$$w$$$-weighted voxel-wise fitting using different
signal models for different TE ranges, resulting
in a cost function depending on the field-map
term only. For cortical-bone regions a single component
with a $$$R_2^*$$$(cortical)
decay is fitted to the UTE data (TE$$$=0.19,0.24,0.34,0.54,0.74\:$$$ms), for the
rest of the volume a multi-compartment fat spectrum
with a spectrum specific to bone
marrow is fitted to the non-UTE TE (TE$$$=1.29,2.39,3.49,4.59,5.69,6.79\:$$$ms). All cost function
values are calculated over a range of $$$[-600, 600]\:$$$Hz. Local minima are extracted and put into
a global cost-function imposing spatial smoothness
on the field-map: This cost-function is solved using
graph-cuts similar to10,11,14. The pipeline of the
proposed UTE field-mapping method is depicted in
Fig.3.
In-vivo QSM processing
For the in-vivo QSM pipeline the background field removal
method Laplacian boundary value (LBV)15 was used. For the field-to-susceptibility inversion the
following $$$\ell_1$$$-regularized cost-function was minimized:$$\chi(\mathbf{r})=\underset{\chi'}{\arg\min}\big|\big|\text{w}(f_{B}-d*\chi')\big|\big|_2^2+\lambda\big|\big|\nabla\chi'\big|\big|_1,$$where the maximum intensity projection over TEs was set as the weighting factor w, $$$d$$$ is the dipole-kernel and the regularization factor $$$\lambda=0.003$$$ for
data-sets and field-maps.Results
Fig.1 shows the estimation the
susceptibility distribution within a perfect cylinder
up to a certain angulation with respect to $$$B_0$$$. However, in a realistic hollow-cylinder
cortical-bone model enclosing bone marrow it is not
possible to homogeniously estimate the bone marrow
susceptibility for any angulation with non-UTE field-map
information.
Only the proposed field-mapping method using
both the UTE and conventional TEs is able to correctly
pickup the diamagnetic nature of cortical-bone
and subsequently improve the susceptibility estimation
of the bone marrow, shown in Fig.4+5.Discussion & Conclusion
UTE is important to correctly estimate susceptibility values
of cortical-bone and the enclosed bone marrow.
The simulations of a realistic cortical-bone structure
emphasizes the need for UTE even when the
hollow cylinder structure is aligned with $$$B_0$$$ to correctly estimate the susceptibility
of the enclosed bone marrow.
In a in-vivo scan only the proposed field-mapping
method applied into a dataset including both UTE
and conventional TEs was able to reveal the true underlying
diamagnetic nature of cortical-bone. However,
the proposed method has the limitation
that regions of cortical-bone need to be identified in
a masking step to apply the simultaneous weighted
2-model voxel-wise fitting.Acknowledgements
The present work was supported by the European
Research Council (grant agreement No 677661, Pro-
FatMRI). This work reflects only the authors view
and the EU is not responsible for any use that may
be made of the information it contains. The authors
acknowledge finally research support from Philips
Healthcare.References
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