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Validating DECOMPOSE QSM with temperature variant ex vivo brainstem imaging experiments
Jingjia Chen1, Khallil Taverna Chaim2, Maria Concepción García Otaduy2, and Chunlei Liu1,3
1Department of Electrical Engineering and Computer Sciences, University of California, Berkeley, Berkeley, CA, United States, 2LIM44, Instituto e Departamento de Radiologia, Faculdade de Medicina, Universidade de Sao Paulo, Sao Paulo, Brazil, 3Helen Wills Neuroscience Institute, University of California, Berkeley, Berkeley, CA, United States

Synopsis

A model and corresponding solver for estimating sub-voxel paramagnetic and diamagnetic susceptibility components are validated based on the temperature dependence of magnetic susceptibility. Two pieces of brainstem sample were scanned under various temperature conditions to test the properties of the separated paramagnetic and diamagnetic components.

INTRODUCTION

Quantitative susceptibility mapping (QSM) is sensitive to tissue’s molecular composition1. QSM has been applied in multiple clinical and research settings, from developing diagnostic biomarker of dementia 2,3,4,5,6 to understanding cerebral structures7,8 and to monitoring disease treatment9. However, colocalization of species with opposing susceptibility confounds the quantification of magnetic susceptibility. For instance, colocalization of iron with Amyloid beta in Alzheimer’s disease patients is known and QSM has been applied to study such.6,10–12 A couple of models have been proposed to decompose QSM.13,14 Among those, qualitative histological staining is the most common in vivo validation. Here, we use temperature-dependent GRE data to validate the separation of a newly proposed DECOMPOSE QSM.

THEORY

Paramagnetism and diamagnetism are the two most commonly found magnetic properties of biologic tissues. Following Curie’s Law, at a certain range of temperature and field strength, paramagnetic susceptibility is approximately inversely proportional to temperature, $$\begin{align} \chi (T\rightarrow \infty) = \frac{C}{T} \end{align} \tag{1}$$ where C is the material’s specific Curie constant. We propose to use this relationship to validating algorithms for decomposing QSM sources. Specifically, the paramagnetic component should be temperature dependent while the diamagnetic component should remain stable across temperature changes. There has been study shown that such an effect is visible through QSM15.'

The model we are validating here is the DiamagnEtic-COMponent-and-Paramagnetic-cOmponent-SEparation (DECOMPOSE) QSM based on a three-pool signal model as$$\begin{align}S(t;C_+,C_-,C_0,\chi_+,\chi_-,R^*_{2,0})=&C_+e^{-(a\chi_++R^*_{2,0}+i\frac{2}{3}\chi_+\gamma B_0)t}\\&+C_-e^{-(-a\chi_-+R^*_{2,0}+i\frac{2}{3}\chi_-\gamma B_0)t}\\&+ C_0e^{-R^*_{2,0}t}\end{align}\tag{2}$$
where paramagnetic, diamagnetic and neutral-susceptibility components contribute one term each of complex exponential to the total signal of a voxel. The estimated parameters are used to form Paramagnetic Component Susceptibility (PCS) and Diamagnetic Component Susceptibility (DCS) defined as below,
$$\text{PCS (or DCS)}=\frac{\sum_t\measuredangle(C_{+or-}e^{-(a|\chi_{+or-}|+R^*_{2,0}+i\frac{2}{3}\chi_{+or-}\gamma B_0)t}+(C_0+C_{-,or +})e^{-R^*_{2,0}t})}{\frac{2}{3}\gamma B_0\sum t}\tag{3}$$.

METHODS

Two human brainstems were fixed in a non-buffered 4%-formalin for over 12 months, washed out in distilled water and placed into a proton-free fluid (Fomblin) prior to MRI scanning. Fomblin produces no MRI signal and has a similar susceptibility to tissue16. Sample tube was heated up using water bath for 3 hours at 40oC before the acquisition on 7T Magnetom (SIEMENS, Erlangen, Germany) using an in-house built solenoid.

QSM acquisition was repeated sequentially while the brainstem was cooling down naturally until reaching thermal equilibrium (20°C). A 3D muilti-echo FLASH GRE was used with the following parameters:FOV=120mm, voxelsize=0.25x0.25x0.4mm3. Two sets of data were acquired: one with five echoes of TE1/deltaTE/TE5 = 4/3/16ms, and the other with 16 echoes of TE1/deltaTE/TE16=4/3/49ms. Due to low SNR of later echoes, only the first 12 echoes were adopted for further analysis.

Before every GRE acquisition, a single-shot water unsuppressed spectrum was acquired with semiLASER sequence, with TE/TM/TR=7/26/9000 ms, voxelsize = 30x20x20 mm3 to estimate temperature through chemical shift from the spectrum.

Phase is unwrapped by Laplacian-based method17,18 followed by V-SHARP19 background removal. Lastly, QSM of each echo was computed using STAR-QSM20 in STI Suite21. The resulting QSM maps are re-referenced to the region where $$$R_2^*$$$ value has lower than 4 Hz2 variance over time.

RESULTS

Figure 1 shows a plot of the indirect measurement of temperature through analyzing water proton chemical shift as a function of time. The DECOMPOSE results of each set of data are presented as line graphs and corresponding parameter maps. The resulting paramagnetic component susceptibility (PCS) (Figure 2,4) showed more visible increases as the temperature decreases. The diamagnetic component susceptibility (DCS) showed minimal changes across the scans. Detailed parameter maps of one sagittal slice are shown in Figure 3,5. With either 5 or 12 echoes, the resulting PCS visibly increase as the temperature decreases. Further, it appears that decomposing with the 12-echo data results in more temperature-stable DCS maps.

DISCUSSION

The method we are validating is based on multi-echo GRE data. Generally, more echoes are beneficial since the model relies on the temporal behavior of the signal progression. Here we show that, in practice, with as minimal as 5 echoes, the algorithm is able to separate para-/dia-magnetism with reasonable results.

One big challenge in performing the analysis was the lack of an absolute reference for QSM. As temperature changes, the absolute bulk susceptibility of the whole sample changes. Larmor frequency shift and phase pre-processing employed in QSM reconstruction methods remove the zero and first-order information of the phase, which leads to the QSM being referenced to the mean of the whole sample with STAR-QSM. As the temperature decreases, total bulk susceptibility increases with paramagnetic susceptibility's increase, which will then lead to an apparent decrease of the diamagnetic part whereas the physical diamagnetic susceptibility ought to remain stable with temperature changes. To address this, we used regions with minimum $$$R_2^*$$$ temporal variation as QSM reference. Even so, changes in DCS may still be observed but less dramatic than that of PCS.

The volume fractions ($$$C_{+,-,0}$$$) also showed a slight temperature dependance. We estimated that the thermal expansion resulting from a 20-degree-Celsius range will lead to approximately 0.5% of volume change if extracellular fluid is considered to have volume thermal expansion coefficient close to water22 and up to 1.5% if proteins/lipids and other biomolecules are considered23. This is comparable to what we have observed. Nonetheless, the estimation of parameters may be corrupted by noise and QSM inaccuracies, thus caution is warranted in interpreting the results.

Acknowledgements

No acknowledgement found.

References

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Figures

Figure1. Temperature profile estimated from water proton spectrum before each QSM scan. The blue circles are the estimated temperature from calculating chemical shift. The orange circles indicate each QSM acquisition.

Figure 2. DECOMPOSE QSM results for 16 echoes data set. Mean value of each parameters of all 10 scans are shown. Temperatures range from 37 °C to 21 °C. Mean value is calculated from the non-zero mean of one representative slice. Note the paramagnetic component susceptibility is increasing with decreasing temperature as expected.

Figure 3. Parameter maps, paramagnetic component susceptibility (PCS) and diamagnetic component susceptibility (DCS) compared to thresholding QSM. The line artifact in the third column is due to a dicom file error of two slices in the magnitude images. The increasing trend of PCS is visible, while the temperature related change in DCS is minimal.

Figure 4. DECOMPOSE QSM results from data with only 5 echoes. Temperature range from 37 °C to 20 °C Each parameter’s non-zero mean value of a representative slice is displayed vs. temperature changes. The paramagnetic component susceptibility (PCS) shows increasing trend particularly for the first 5 temperature points.

Figure 5. DECOMPOSE QSM parameter maps of the first 10 scans comparison to the QSM thresholding at zero. While DCS maps remain mostly stable, PCS maps show an increasing trend especially for the first 5 scans where temperature was changing the most drastically.

Proc. Intl. Soc. Mag. Reson. Med. 29 (2021)
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