xiaoyu jiang1, sean p devan1, john c. gore1, and junzhong xu1
1Vanderbilt University Institute of Imaging Science, nashville, TN, United States
Synopsis
There is an increasing interest in characterizing tissue
microstructure using multi-compartment diffusion MRI models involving multiple
b values and diffusion times ($$$t_{diff}$$$s).
However, previous models usually ignore water exchange
between intra- and extracellular compartments, which limits the accuracy of
the fitted model parameters and potentially their interpretation as indicators
of disease progression or treatment response. Here, we propose a simplified
biophysical model of solid tissues that allows derivation of the mean intracellular
water lifetime ($$$\tau_{i}$$$) and other microstructural parameters (e.g., cell
size d) simultaneously from the $$$t_{diff}$$$ dependence of
diffusion MRI signals.
Introduction
Transcytolemmal water exchange plays a fundamental role in
cell physiology (1). The intracellular water
lifetime, $$$\tau_{i}$$$, is a key biophysical parameter that describes
transcytolemmal water exchange and which has been suggested as an indicator of
disease progression and treatment response (2).
In vivo measurements of $$$\tau_{i}$$$ are usually achieved using paramagnetic contrast
agent methods (3,4),
while diffusion-based methods such as the constant-gradient (5) and FEXI (filtered exchange
imaging) (6) are either limited by SNR or influenced
by other confounding effects. We propose a simplified model that incorporates
transcytolemmal water exchange in a multi-compartment diffusion-based IMPULSED method (7-9) that has been developed
previously to extract microstructural parameters (e.g., mean cell size d,
and intracellular volume fraction vin assuming no water exchange. Using simulations, we show that not only can the
proposed method estimate $$$\tau_{i}$$$ and d accurately,
but also it reduces the underestimation of IMPULSED-derived vin. Theory
The influence of cell membrane permeability (a function of
and
) on MR diffusion measurements depends on $$$t_{diff}$$$ (10):
it is negligible when $$$t_{diff}$$$ is relatively
short while it impacts diffusion signals significantly when t_{diff} is relatively
long. Therefore, a combination of acquisitions of both oscillating gradients as
in OGSE (oscillating gradient spin echo) for short $$$t_{diff}$$$ (e.g., ≤ 5
ms) and bipolar gradients as in PGSE (pulsed gradient spin echo) or STEAM (stimulated
echo acquisition mode) for relatively long $$$t_{diff}$$$ (e.g., ≥30 ms) provides sufficient coverage for practical
characterizations of $$$\tau_{i}$$$ and d. Solid tissues are modeled as two-compartments in
which water diffuses and exchanges. Cells are approximated as permeable spheres
with mean diameter d, intracellular diffusion coefficient Din (fixed to 1.56 µm2/ms as suggested
in (9)), and intracellular water
lifetime $$$\tau_{i}$$$. The analytic expressions
describing hindered/restricted diffusion in extra/intra-cellullar spaces are
the same as in the previous IMPULSED method, but the effect of water diffusion is
incorporated differently in different $$$t_{diff}$$$ ranges:
1. For short $$$t_{diff}$$$ (e.g., 5 ms using 50 Hz of OGSE), the water
exchange is ignored and the signal model is the same as the IMPULSED analysis (7).
2. For
long $$$t_{diff}$$$ (e.g., ≥ 30 ms), we adapted the
modified $$$K\ddot{a}rger$$$ model (11) that includes both restricted
diffusion and exchange between pools. This model assumes short gradient pulses
(i.e., δ ≪ Δ) so that diffusion is considered only during two
short gradient pulses, while relaxation and exchange effects occur throughout
the pulse sequence.
Using this hybrid model, we are able to extract d, vin and $$$\tau_{i}$$$ from diffusion
signals acquired with different $$$t_{diff}$$$.Methods
Finite difference
simulations (12) were performed on modeled tissues consisting of
closely packed spherical cells with vin
= 61.8%, Dex = 1 µm2/ms, and Din = 1.56 µm2/ms, d from 10 to 20 µm with each
incorporated 15 different $$$\tau_{i}$$$’s: 50, 60, 70, 80, 90,
100, 125, 150, 200, 250, 300, 350, 400, 450, 500, and $$$\infty$$$ ms. Bipolar gradients with $$$t_{diff}$$$ =
30, 70, 100, 200 ms and oscillating gradients with 50 Hz ($$$t_{diff}$$$ = 5
ms) were used to generate diffusion MRI signals with a gradient rise time 0.9
ms as in clinics (9). Results
Figure 1 shows that the simulated 50 Hz OGSE signals for
different cell sizes (10, 15, and 20 µm) and $$$\tau_{i}$$$s are almost the same, confirming the negligible
influences of $$$\tau_{i}$$$ when $$$t_{diff}$$$ is short. By
contrast, fast water exchange (
$$$\tau_{i}$$$
=50 ms) significantly affects diffusion data
acquired with relatively long diffusion times.
The hybrid model-derived $$$\tau_{i}$$$ and cell
membrane permeability Pm (a function of $$$\tau_{i}$$$, d, and Din (12))
show good agreement with the preset values (Figure 2&3). The noise level
has a larger impact on the accuracy of the fitted $$$\tau_{i}$$$s than the fitted cell sizes (Figure 4), and this
impact reduces with decreasing cell size.
Expanding the range of diffusion times from 100 to 200 ms increases the
sensitivity for detecting slower water exchange for larger cells.
Figure 4 shows that the IMPULSED method overestimates cell
sizes when fast water exchange exists, and the hybrid model improves cell size estimates.
As shown in Figure 5, ignoring water exchange leads to an underestimation of
intracellular volume fraction (vin). The hybrid model corrects the
bias when water exchange is relatively slow (e.g., $$$\tau_{i}$$$
>200 ms).Discussion and Conclusion
We propose a simple biophysical model to provide
simultaneous assessment of intracellular water lifetime $$$\tau_{i}$$$ and cell size d in
physiologically relevant ranges using diffusion MRI with clinically achievable
diffusion times (5-100 ms). Because of the involvement of the modified $$$K\ddot{a}rger$$$ model for long $$$t_{diff}$$$ data, it is
challenging for this model to quantify fast water exchange ($$$\tau_{i}\gg\frac{cell\:radius^2 }{intrinsic intracellular diffusion coefficient (D)}$$$), e.g., $$$\tau_{i}$$$ < 10 ms
and 35 ms for cells with diameters of 10 and 20 µm, respectively, assuming D is
~ 3 µm2/ms (free water diffusion rate at body temperature).
Moreover, the assumption of short gradient pulses may not be valid for cases
that use long pulse durations. Efforts to develop a general approach that models
diffusion and water exchange under finite durations of gradients are ongoing. Acknowledgements
No acknowledgement found.References
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