Biomagnetic studies of slow CNS disturbances. Gardner-Medwin AR (1993) In: Migraine: Basic Mechanisms and Treatment. ed. Lehmenkühler A. et al.. Urban & Schwarzenberg, Munchen, pp. 229-238
Biomagnetic studies of slow CNS disturbances
A.R. Gardner-Medwin
Department of Physiology,
University College London,
London WC1E 6BT,
UK
Running Head: MEG studies of slow CNS disturbances
INTRODUCTION
Measurement of the magnetic fields produced by electrical events
in the brain (magneto-encephalography: MEG) offers a non-invasive technique
for study that has a number of advantages over the direct measurement of
surface voltage changes (EEG). The advantage that has received the most
study is its potential for localising the origin of a signal accurately.
MEG signals are relatively little affected by the high resistance (bone
and dura) encasing of the brain and the low resistance (scalp) outer tissue,
which attenuates and distorts electric current flow to the sites of non-invasive
electrodes. Much interest has centred round the localisation of epileptic
foci, event related signals, and rhythmic activity. These signals mostly
lie in the frequency band 1Hz-1kHz, for which MEG techniques nowadays tend
to be best adapted.
Migraine, particularly the aura of classical migraine, is known
to be associated with some sort of pathophysiology of the brain, often
specifically of parts of the cerebral cortex. The disturbances usually
have a time course of minutes or hours. The visual aura in classical migraine
has components (scintillating patterns at the region of onset of a scotoma)
that suggest abnormal physiological activity at frequencies well above
1Hz, but the profound loss of function that spreads across the visual cortex
in this form of migraine itself has a duration at any one site of several
tens of seconds or minutes (e.g. Lashley, 1941). It is potentially of interest
to look for MEG signals with this kind of time course under such conditions.
Preliminary biomagnetic studies have been carried out in migraine
patients, some of them using DC recording techniques (Barkley et al., 1990).
There are formidable technical problems in such studies, due to the level
of magnetic interference that is picked up at low frequencies even inside
a shielded room, and the problems of artefact identification. This makes
it difficult to establish what signals may be consistently related to specific
aspects of the migraine syndrome, let alone where (in the brain or elsewhere)
these signals may originate.
One of the problems in migraine is that one is looking for magnetic
signals that are not necessarily time locked in a consistent way to any
other identifiable characteristic of the syndrome. They may also differ
radically, because of different tissue geometry and structures involved,
in different patients. They are therefore not amenable to averaging across
episodes or across subjects, which can improve the signal-to-noise ratio
in experimentally triggered disturbances such as spreading depression in
animals (Gardner-Medwin et al. 1991, & Fig. 1). Satisfactory study
of one-off slow signals requires a considerable technical improvement in
signal-to-noise ratio and artefact identification.
A particular reason for interest in slow magnetic signals in
neurological conditions is that both ischemia and spreading depression
are associated with very large and prolonged electro-physiological changes
in affected regions: large negative extracellular potential changes, high
potassium concentration, and large currents through glial cells involved
in homeostasis (see Gardner-Medwin, 1981 for a discussion of these phenomena
in relation to migraine). Spreading depression offers a good experimental
model for studying the effects of such changes. The magnetic signals seen
in anaesthetised rabbits during spreading depression consist of slow field
shifts with a peak amplitude of about 1.5 pT approximately 400 s after
induction of the disturbance with KCl application. The average inferred
current dipole sources (Fig. 1B) have a similar time course, with variable
rapid components at the onset and termination of KCl application. These
signals were close to the limits of what could reliably be detected with
conventional biomagnetic techniques using second order gradiometers (see
below) in a screened room.
TECHNIQUES
This paper sets out a novel approach to the improvement of biomagnetic
signal-to-noise ratios at ultra low frequencies (0.001-0.1Hz). It is well
known that to measure DC sources one must move the source relative to the
magnetometer. Various approaches have been used, including comparison of
fields with the subject under the magnetometer and at a remote distance
either horizontally (Cohen & Kaufman, 1975) or vertically (Elbert,
1991) or with repeated scanning across the source with the subject on a
moveable bed (Freake et al., 1988) or with an animal on a swing (Trontelj
et al., 1989). The procedure employed here is to impose on the subject
a constant horizontal circular motion under the magnetometer, with a radius
of 12 mm and a period of normally 2-4 s for human subjects (Fig. 2). This
is referred to as rotatory scanning (Gardner-Medwin, 1991). The subject
is barely aware of this motion, provided it is smoothly executed.
The rotatory scanning has the effect that any DC magnetic source
on the moving plate produces an AC field at the frequency of rotation (Fig.
3). This AC field is proportional to the horizontal gradient of field due
to the source, and is in a region of the spectrum where the noise amplitude
in the critical units (pT/?Hz) is much less than at frequencies below 0.1Hz.
The DC sources and fields can be inferred from measurements of the AC signals,
rejecting completely the effects of DC field shifts from environmental
interference.
Automatic computer analysis of the signals allows measurements
of the field gradients in two perpendicular directions to be derived in
each cycle of the rotation. The directly measured fields can also of course
be observed, and are usually averaged throughout each cycle. This provides
significant data compaction, with still quite adequate time resolution
for study of phenonena varying over tens of seconds or more. This gives
a technique for essentially continuous high stability monitoring of DC
fields, simultaneously on as many channels as the hardware and software
will handle. Fig. 4 shows the simultaneous monitoring on 6 magnetic channels
of a slowly changing current in a calibration dipole (period 20s, maximum
peak to peak amplitude 24?A.mm, approximately as for the sources during
spreading depression in Fig. 1). Substantial background field shifts took
place during this 10min stretch of recording, larger than the directly
measured sinusoidal signals (middle traces). These had only a transient
and small effect on the gradient traces extracted from the rotatory scanning
analysis and shown at the top (for one direction only). The data obtained
wth the rotatory scanning techniques monitors faithfully the slow time
course of the changes in the source.
There are two incidental additional advantages that derive from
the rotatory scanning technique:
1. Most commercial magnetometers measure vertical or near vertical
fields, which are zero directly over an active current dipole source. They
have positive and negative maxima on either side of the dipole, as can
be seen in Fig. 4 by noting the opposite phase of the large signals at
the top and bottom of the mean directly measured fields. The field gradient
on the other hand has a maximum directly over the dipole (as seen in the
top traces in Fig. 4). This makes for somewhat more direct interpretation
of the records in relation to dipole sources.
2. Since the rotatory scanning derives horizontal gradients
of the measured fields, it improves the relative sensitivity of the magnetometer
to nearby sources rather than distant sources. Fields due to distant sources
that are not on the moving table are totally rejected unless they happen
to have a component of variation at the frequency of movement. Magnetic
sources on the moving table, such as ferromagnetic contamination in the
nose, teeth, lungs or abdomen, are however also sources of significant
interference, especially if body movements occur. These contamination sources,
though they may be very large, are mostly much more distant than the sources
of interest in the brain. The signals they induce fall off as r-4 for an
instrument designed as what is called a 1st order gradiometer and as r-5
for a 2nd order gradiometer (where r is the distance of the source, assumed
to be a magnetic (not a current) dipole, of constant orientation). With
these same instruments the field gradients measured with rotatory scanning
fall off as r-5 and r-6 respectively. This can give a significant benefit.
For the same reasons, a 2nd order gradiometer is generally better than
a 1st order gradiometer at rejecting the effects of contamination.
VALIDATION
Assessment of the rotatory scanning technique ideally requires
a slowly changing physiological signal that is reproducible in man, with
similar temporal characteristics to the signals of potential interest during
brain pathologies. In collaboration with S. Swithenby and K. Fiaschi we
are studying the field changes associated with the corneo-retinal current
through the eye. This current rises slowly to about double its baseline
level in the dark, reaching a peak approximately 8 minutes after the onset
of light. The usual technique for monitoring these changes does not even
involve DC electrical recording, but measures the rapid potential shift
between the two sides of an eye (electro-oculogram) when a standard eye
movement is made (Arden & Kelsey, 1962). Parallel measurements of magnetic
shifts have also been made using standard eye movements (Katila et al.,
1980). With care, the corneo-scleral DC potential differences can be measured
directly (Nielsen XX, 1991). We are essentially carrying out the equivalent
DC magnetic study, measuring directly the steady magnetic fields in the
vicinity of the eye and their changes following a change in light level.
Fig. 5 shows records obtained with a single channel magnetometer
using rotatory, showing the field gradients on exposure to light after
dark adaptation and also the simultaneous conventional measurements of
the mean field over each cycle period. The sensor was positioned over the
left temple. The gradients measured with the rotatory scanning analysis
exhibit the characteristic time course of the changes in corneo-retinal
current. Similar time courses following the onset of light were seen in
the modulus of the gradient on each of 4 runs (with various sensor positions)
on 2 subjects. Although these observations are very preliminary and
the changes have yet to be mapped satisfactorily, they demonstrate the
advantage to be gained from the scanning technique. Note that the simultaneous
direct field measurements in Fig. 5 show too many erratic DC shifts to
be interpretable at all.
CONCLUSION
Complete and confident characterisation of slow magnetic signals
from a neurological patient necessarily requires that a great many factors
combine at one time. Some of the trickiest of these are clinical factors:
the patient must be able to produce the phenomena of interest within an
acceptable time in the magnetic laboratory. He must also be sufficiently
cooperative and comfortable to lie still for the time required. The kinds
of improvement of signal to noise ratio described here should go a long
way in improving the technical reliability of the records and reducing
the stringency of the requirements that a good subject must be relatively
free of magnetic contamination.
ACKNOWLEDGEMENT
This work is supported by the Wellcome Trust, and has in part depended
on the collaboration and advice of S. Swithenby, K. Fiaschi, C. Guy, T.
Elbert and their colleagues. Much of the equipment was made by D. Farquharson
and P. Stukas.
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Fig. 1. Biomagnetic changes recorded from anaesthetised rabbits following initiation of Spreading Depression (SD) with 150mM KCl applied at the cortical surface in a cup on the left hemisphere. A. Means and s.e.m. from the indicated numbers of recordings (N), of vertical field shifts at various recording sites above the heads of the rabbits at 400s after KCl application. B. Inferred net dipole source strength (mean ± s.e.m.) in the anterior posterior direction (0o) and rightward direction (90o) from ten recordings. Bar shows the time of KCl application. Data from Gardner-Medwin et al. (1991).
Fig. 2. Apparatus used for constant rotatory scanning of a subject under a magnetometer. The subject stays in a constant orientation while each point moves in a 12mm diameter circle with a period of usually 2-4s. The drive is conveyed to the upper plate by a system of cords, pulleys, etc. engineered in non-magnetic materials. The (1st or 2nd order) magnetometer measures vertical or near vertical fields on any number of channels.
Fig. 3. Fourier transform data with a steady calibration source of different strengths at a distance of 15mm below the magnetometer sensor coil. A signal at the frequency of rotatory scanning (ca. 0.9Hz) is superimposed on the background noise and is proportional to the source strength. Measurement of the Fourier components at the scanning frequency gives the horizontal gradients of the vertical field produced by DC sources that move with the table. Most of the background noise is excluded, as are gradients due to magnetic sources that do not move with the upper plate in Fig. 2. Data obtained with a 2nd order gradiometer in an unshielded room, in collaboration with S. Swithenby & K. Fiaschi (Open University, UK).
Fig. 4. Measurements of the field gradient in the X direction (upper traces) obtained with the rotatory scanning technique from 6 magnetometer channels ca. 48mm above a calibration dipole in the Y direction. Direct field measurements averaged over each scanning cycle are shown below (middle traces). Current in the dipole was varied as shown in the bottom trace (at ca. 0.05 Hz). The 6 channels were spaced by 20mm in the X direction, approximately symmetrically over the dipole. Note the shifts in field measurements due to DC shifts in external interference; these have only slight transient effects on gradients derived from rotatory scanning. Data obtained with 1st order gradiometers in a shielded room, in collaboration with T. Elbert (Munster, Germany).
Fig. 5. Measurements of DC field changes following the onset of
light adaptation in a human subject. The subject had been dark adapted
for ca. 20min and was then exposed to ordinary room light. The head lay
on its right side, with the left temporal aspect of the skull horizontal.
The vertical field was measured ca. 22 mm above the temple and 40mm from
the corner of the eye in the X direction (toe to head). Gradients in the
X direction and Y direction (front to back) are shown, derived from rotatory
scanning at 0.3 Hz. Simultaneous recording of the directly measured mean
field (top trace) shows marked field shifts not reflected in the gradient
measurements. The X and Y gradients show the characteristic slow transient
time course of changes in the corneo-retinal current due to light adaptation,
with a maximum about 10min after light onset. A single channel 2nd order
gradiometer was used in an unshielded environment with active cancellation
of the earth's field. Data obtained in collaboration with S. Swithenby
& K. Fiaschi (Open University, UK).