Sergey Magnitsky1
1CHOP, Philadelphia, PA, United States
Synopsis
Diffusion-weighted
imaging is instrumental in the evaluation of bone quality. However, an interpretation
of the data obtained from porous material is complex due to the effects of
restricted diffusion. In this study, we are presenting a new restriction
diffusion phantom, which was developed for an optimization of acquisition
protocols for bone studies. The phantom consists of microscopic-slides
separated by glass spheres (~10 μm). The space between slides was
filled with water. NMR data were collected and diffusion-properties of the
phantom were documented. The proposed phantom can be easily replicated in any
laboratory and will assist in investigations of restriction diffusion.
Introduction
Different patterns of restricted diffusion were
detected in various bone conditions. To model restricted diffusion,
investigators used phantoms made of natural products like celery stems. These
phantoms are not stable and not reproducible. No commercially available
restricted diffusion phantoms are available at present. The goal of this study
was the development of a simple restricted diffusion phantom to detect:1) the effect
of the impermeable boundary on diffusion data, 2) determine b/q-values when the free and restricted
water becomes different, 3) probe angular properties of restricted diffusion. This phantom will be utilized for an optimization of
acquisition parameters of MRI experiments to study restricted diffusion of
water and fat in bones.Methods
Hollow
glass spheres with a diameter of 9-13 μm (Sigma-Aldrich)
were spread with a painting brush evenly on a surface of 10 microscope glass
slides (75 x 38 mm, Fisher Scientific). The slides were put on each other and
tighten together with a string. The stuck was immersed in a container with tap
water. After 60 min, the phantom was removed from the water and wax was applied
on the edges of the phantom to prevent drying.
Experiments were conducted at 4.7 T horizontal bore magnet interfaced
with Varian console. A two cm surface transmit-received coil was utilized for the
acquisition of NMR data. The phantom was placed into the magnet and the
diffusion-weighted stimulated echo experiment was performed with the following
parameters: TR=10 s, TE = 10 ms, diffusion gradient was varied 0-24 G/cm, the
angel of the diffusion gradient was varied 0-900, d = 20 ms, D = 450 ms.
Results
Figure 1 shows the normalized
q-plot (q=(1/2p)gGd) of the NMR signal intensity of free water and water
in the phantom. The Green symbols depict free water diffusion. The Blue symbols
present the water signals in the phantom with the diffusion gradient applied
parallel to the surface of the glass slides. The Red symbols show water
diffusion in the phantom with the diffusion gradient applied perpendicular to
the surface of the glass slides. The NMR signal intensity of water molecules
inside of the glass phantom is following the free diffusion pattern only in the
parallel orientation of the diffusion gradient and the surface of glass slides.
Rotation of the diffusion gradient by 90-degree to the surface of the slides
revealed the significant deviation from the free diffusion pattern and the
presence of local minimums (Figure 1 red symbols). These phenomena were
described by Callaghan [1] and reflected the presence of impermeable
boundaries. In our experiments, the minimums were detected at q(min1) = 70534
and q(min2) = 160305 1/m. A calculation of characteristic dimension based on
this q-values yields a distance of 13.3 and 12.3 mm, which are in a good agreement with dimensions of the
spheres used in our phantom as spacers.
The orientation of diffusion boundaries in the
human bones has a convoluted orientation. To simulate this situation, we
conducted a series of experiments with different orientations of the diffusion
gradient. Figure 2 shows the q-plots of the NMR signal intensity at different
angles between the diffusion gradient and the surfaces of the glass slides. The
minimums, typical for the restricted-diffusion, gradually disappeared from the
curves, and the shape of the line transforms into the free diffusion pattern
with the decrease of the diffusion gradient angle.Discussion and conclusions
In this study, we developed a phantom to simulate diffusion data in
porous compartments of human bone. This simple phantom with known geometry
allowed us: 1) to detect effects of the impermeable boundary on diffusion data,
2) determine parameters of the diffusion experiments when the free and
restricted water exhibit different behavior, 3) probe angular properties of
restricted diffusion.
Characterization of bone porosity plays an important role in the
diagnosis of bone degenerative disorders. The developed phantom permitted us to
model the restricted diffusion in human bones and measure the characteristic
dimension of the compartment. The red curve on Figure 1 is an example of
restricted diffusion, while the green and blue symbols are illustrations of free
diffusion. A significant deviation of free and restricted diffusion curves was detected
at q value more than 25000. The
calculation of the compartment dimensions based on water diffusivity (D = 2.3
x10-5cm2/sec) and the theory developed by Callaghan
revealed ~12.8 μm, which
is in good agreement with the design of our phantom. A variation of the orientation
of the diffusion gradient allowed us to test the effect of un-parallel
boundaries on the diffusion pattern.
The
proposed phantom can be easily replicated in any lab and further modified to mimic
any size of restriction compartments since the hollow spheres of different
sizes are commercially available. We built several copies of the phantom and the
measurements of the distance in different copies were the same with <5%
variation. The similar results obtained from a different copy indicate about good
reproducibility of the proposed phantomAcknowledgements
I would like to thank Dr. S Pickup from the
University of Pennsylvania for the help with MRI acquisition and useful
discussions.References
1. Callaghan,
P.T., NMR imaging, NMR diffraction and
applications of pulsed gradient spin echoes in porous media. Magnetic
Resonance Imaging, 1996. 14(7-8): p.
701-9.