Evalutation of methods for removal for background field inhomogenities in susceptibility weighted phase imaging

Journal article

F. Schweser, A. Deistung, B. W. Lehr, J. Reichenbach

Semantic Scholar


APA   Click to copy
Schweser, F., Deistung, A., Lehr, B. W., & Reichenbach, J. (2008). Evalutation of methods for removal for background field inhomogenities in susceptibility weighted phase imaging.

Chicago/Turabian   Click to copy
Schweser, F., A. Deistung, B. W. Lehr, and J. Reichenbach. “Evalutation of Methods for Removal for Background Field Inhomogenities in Susceptibility Weighted Phase Imaging” (2008).

MLA   Click to copy
Schweser, F., et al. Evalutation of Methods for Removal for Background Field Inhomogenities in Susceptibility Weighted Phase Imaging. 2008.

BibTeX   Click to copy

  title = {Evalutation of methods for removal for background field inhomogenities in susceptibility weighted phase imaging},
  year = {2008},
  author = {Schweser, F. and Deistung, A. and Lehr, B. W. and Reichenbach, J.}


Introduction Susceptibility weighted phase images (SWI) provide anatomical contrast complementary to the magnitude [1, 2] by directly reflecting local magnetic field changes induced by the distribution of magnetic susceptibilities of the measured object. Therefore, phase images can be adducted as marker for deposits of iron [3] which was used to estimate brain iron levels in vivo as a function of age [4]. However, phase images are only defined in the range [-π,π) which produces ambiguities (phase wraps) and thus requires correction of these 2π-wraps. In SWI two methods have been established for phase correction: homodyne filtering [5] and phase unwrapping [6]. In contrast to homodyne filtering phase unwrapping preserves all spatial frequencies and reduces the number of phase wraps especially in the vicinity of air/tissue boundaries. However, unwrapped phase images are superposed with a low spatially varying magnetic field due to background field inhomogeneities. Accurate removing of these background field inhomogeneities from unwrapped phase images is required for quantification of phase images or magnetic susceptibility. Typically, these background fields are estimated by low pass filtering using a Gaussian [7] or box kernel [8], as well as polynomial fitting [2]. In this work, we compare these methods for background field removal with a technique based on spherical mean value estimation (SMVE) [9]. Materials and Methods Volunteer data were acquired with a high-resolution 3D fully flow compensated gradient-echo sequence (TE/TR/FA = 20ms/30ms/15°, voxel size = 0.6×0.6×0.6mm3, 75% partial Fourier along phase and slice encoding direction) on a 3T MR-scanner (Tim Trio, Siemens Medical Solutions) using a 12channel head-matrix coil. The multi-channel phase images were combined using uniform sensitivity reconstruction [10]. Phase wraps were eliminated using homodyne filtering and phase unwrapping using the Phun-package [6] resulting in two sets of corrected images. Three sets of images were obtained from the set of phase-unwrapped images by further correcting them with respect to background field inhomogeneity using low pass filtering (Gaussian kernel), fitting by 2nd order polynomials, and SMVE, respectively. Gaussian filtering was performed with kernel widths ranging from 0.3 to 15 FOV and SMVE was evaluated for sphere radii ranging from 0.6 to 30mm. The resulting images were analyzed with respect to maintenance of absolute phase differences within adjacent regions of the image and inhomogeneity suppression performance. Examination of absolute phase differences was motivated by the assumption that a slowly varying additive background field has a small impact on the difference between adjacent pixel values. Thus, it was assumed that a modification of the gradient map is an appropriate measure of the quality of the background field suppression. As a quality measure for phase differences the RMSE of the corrected images and the original phase-unwrapped image were calculated and normalized with the RMS of the original image. The amount of inhomogeneity suppression was a measured by averaging pixel values of two ROIs in a region of high and low background field magnitude, respectively. The difference of these values was assumed to be closed to zero in case of proper inhomogeneity correction. Results and Discussion Fig. 1 depicts the homogenization measure over the normalized RMSE for all methods and filter parameters. Low homogenization measure and low normalized RMSE means well inhomogeneity suppression and low error in absolute phase differences, respectively. The original image is depicted by a pale blue star at zero RMSE. The SMVE seems to clearly outperform the other approaches for a certain range of sphere radii (3.6 to 10.8 voxels). This is actually misleading as the standard deviations of the ROIs were in the dimension of 10 for these images. The elimination of the background field in these images was performed equally well. Furthermore, it is striking that no images could be extracted that have both proper background field elimination and an RMSE below 0.1. This border likely results from the small background field component that is still present in the gradient field. The region of well reconstructed phase images is highlighted in green. These values were achieved by polynomial fitting, low pass filtering (kernel width of 7 to 9 FOV), and SMVE (radius of sphere 6 to 18mm). However, the results of low pass filtering and SMVE depended on the chosen filter parameters. The homodyne filter sufficiently removed the background inhomogeneities but significantly modified the absolute phase differences in all cases. The measured phase map containing both phase wraps and background field inhomogeneity is shown in Fig. 2a. A homodyne filtered image and the phase unwrapped image are shown in Fig 2b and c, respectively. Background field inhomogeneities are directly removed using homodyne filtering while inhomogeneities are still depicted in the phase unwrapped image. Significant artefacts at the edges of the phase maps in Gaussian and SMVE may be attributed to incomplete removal of localized inhomogeneities and incomplete averaging at the edges, respectively.

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