vertebrae (T4-L5) from one normal and one scoliotic magnetic resonance (MR) spine image using six manual and two computerized measurements. Manual measurements were performed by superior and inferior tangents, anterior and posterior tangents, and mid-endplate and mid-wall lines. Computerized measurements were performed by automatically evaluating the symmetry of vertebral anatomy in sagittal cross-sections and volumetric images. The mid-wall lines were the manual measurements with the lowest intra- and inter-observer variability (
and
standard deviation, SD). The strongest inter-method agreement was found between the mid-wall lines and posterior tangents (
SD). Computerized measurements did not yield intra- and inter-observer variability (
and
SD) as low as the mid-wall lines, but were still comparable to the intra- and inter-observer variability of the superior (
and
SD) and inferior (
and
SD) tangents.
1 Introduction
radiographs of L4/L5 and L5/S1 segments. The manual and computer-assisted measurements proved to be equivalent in terms of variability, the Cobb angle and posterior tangents were the least variable, and the anterior tangents were the most reliable measurements. Street et al. [15] evaluated the reliability of measuring kyphosis manually from different imaging modalities in the case of thoracolumbar fractures. For the Cobb angle measurements, they concluded that plain radiographs were the most reliable measurement modality, followed by computed tomography (CT) and finally by magnetic resonance (MR) imaging.2 Methodology
2.1 Manual Measurements
of SVI, measured against reference horizontal or vertical lines that are parallel to the coordinate system of the 3D image.
2.2 Computerized Measurements
of rotation of the local vertebral coordinate system
(defined by Cartesian unit vectors
,
and
) around the axes of the global image coordinate system
(defined by Cartesian unit vectors
,
and
). Both
and
are right-hand Cartesian coordinate systems, representing left-to-right (
-axis), anterior-to-posterior (
-axis) and cranial-to-caudal (
-axis) direction. The angles
(i.e. SVI),
(i.e. coronal vertebral inclination) and
(i.e. axial vertebral rotation) then represent the rotation of the vertebral coordinate system
around vectors
(pitch),
(roll) and
(yaw), respectively. If the origin of
is located at the vertebral centroid and
is rotationally aligned with the vertebra in
, anatomically corresponding symmetrical parts of the vertebra can be observed within volumes of interest (VOIs) along positive/negative directions of each axis
,
. The angles
of vertebral rotation can be therefore determined by finding the planes of maximal symmetry, which divide the whole vertebra into symmetrical left/right (
) halves, and the vertebral body into symmetrical anterior/posterior (
) and cranial/caudal (
) halves. For each axis
,
, the symmetrical correspondences of the two halves (
and
) of a VOI are measured by
:

), shown for a symmetrical pair of points
and
inside
. b The vertebral coordinate system
and the observed volumes of interest (
encompasses the whole vertebra,
encompasses the vertebral body)
is the weighting function, and
and
are the projections of the intensity gradient vectors
and
in the coordinate system
to the unit vector
,
, of the coordinate system
at symmetrical pair of points
and
, respectively, and
is the number of point pairs inside each VOI (Fig. 2a). By projecting the gradient vectors to
,
, and by applying the weighting function
, we retain the gradient components
and
that are relevant for defining the vertebral symmetry in the direction of
. Two variations of the computerized method were applied for each vertebra. The measurements in 3D automatically evaluated the vertebral rotation in 3D images by maximizing symmetrical correspondences:
, and the VOI that encompasses the vertebral body is denoted by
(Fig. 2b). On the other hand, the measurements in 2D automatically evaluated SVI in the same 2D oblique sagittal cross-sections that were used for manual measurements (Fig. 3) by considering only
that encompasses the vertebral body and reducing its dimensionality to the area of interest (AOI), and maximizing the remaining symmetrical correspondences:

mm in size to encompass the whole vertebral body of thoracic and lumbar segments. By rotating these planes in 3D, the rotation angles
are obtained from the inclination of the planes, and the current symmetrical correspondences are evaluated by mirroring the edges of vertebral anatomical structures (obtained from image intensity gradients) over each plane and comparing them to the edges on the opposite side of that plane in an optimization procedure.3 Experiments and Results
3.1 Images and Observers
vertebrae between segments T4 and L5 from one normal (
-year male,
frontal Cobb angle) and one scoliotic (
-year male,
frontal Cobb angle) spine image were included in this study. The T2-weighted MR scans (mean repetition and echo time TR
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