Lecture 3 the mr signal equation
Download
1 / 23

Lecture 3: The MR Signal Equation - PowerPoint PPT Presentation


  • 155 Views
  • Uploaded on

Lecture 3: The MR Signal Equation. We have solved the Bloch equation and examined Precession T2 relaxation T1 relaxation MR signal equation Understand how magnetization changes phase due to gradients Understand MR image formation or MR spatial encoding. Complex transverse magnetization: m.

loader
I am the owner, or an agent authorized to act on behalf of the owner, of the copyrighted work described.
capcha
Download Presentation

PowerPoint Slideshow about 'Lecture 3: The MR Signal Equation' - wilkinson


An Image/Link below is provided (as is) to download presentation

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.


- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -
Presentation Transcript
Lecture 3 the mr signal equation l.jpg
Lecture 3: The MR Signal Equation

  • We have solved the Bloch equation and examined

    • Precession

    • T2 relaxation

    • T1 relaxation

  • MR signal equation

    • Understand how magnetization changes phase due to gradients

    • Understand MR image formation or MR spatial encoding


Complex transverse magnetization m l.jpg
Complex transverse magnetization: m

m is complex.

m =Mx+iMy

Re{m} =Mx Im{m}=My

This notation is convenient:

It allows us to represent a two element vector as a scalar.

Im

m

My

Re

Mx


Inhomogeneous object nonuniform field l.jpg
Inhomogeneous Object - Nonuniform field.

Now we get much more general.

Before, M(t) was constant in space and so no spatial variable was needed to describe it.

Now, we let it vary spatially.

We also let the z component of the B field vary in space.

This variation gives us a new phase term, or perhaps a more general one than we have seen before.


Transverse magnetization equation l.jpg
Transverse Magnetization Equation

We can number the terms above 1-4

1. - variation in proton density

2. - spatial variation due to T2

3. - rotating frame frequency

- “carrier” frequency of signal

4.

- spins will precess at differential frequency according to the gradient they experience (“see”).


Transverse magnetization equation5 l.jpg
Transverse Magnetization Equation

- spins will precess at differential frequency according to the gradient they “see”.

Phase is the integral of frequency.

Thus, gradient fields allow us to change the frequency and thus the phase of the signal as a function of its spatial location.

Let’s study this general situation under several cases, from the specific to the general.


The static gradient field l.jpg
The Static Gradient Field

In a static (non-time-varying) gradient field, for example in x,

Plugging into solution (from 2 slides ago)

and simplifying yields


The static gradient field7 l.jpg
The Static Gradient Field

Now, let the gradient field have an arbitrary direction. But the gradient strength won’t vary with time.

Using dot notation,

Takes into account the effects of both the static magnetic and gradient fields on the magnetization gives


Time varying gradient solution non static l.jpg
Time –Varying Gradient Solution (Non-static)

. We can make the previous expression more general by allowing the gradients to change in time. If we do, the integral of the gradient over time comes back into the above equation.


Receiving the signal l.jpg
Receiving the signal

Let’s assume we now use a receiver coil to “read” the transverse magnetization signal

We will use a coil that has a flat sensitivity pattern in space.

Is this a good assumption?

- Yes, it is a good assumption, particularly for the head and body coils.

Then the signal we receive is an integration of

over the three spatial dimensions.


Receiving the signal 2 l.jpg
Receiving the signal (2)

Let’s simplify this:

1) Ignore T2 for now; it will be easy to add later.

2) Assume 2D imaging. (Again, it will be easy to expand to 3 later.)

3) Demodulate to baseband.

i.e.

zo

slice thickness z

S(t) is complex.


Receiving the signal 3 l.jpg
Receiving the signal (3)

S(t) is complex.

Then,

3) Demodulate to baseband.

i.e.

end goal


G x t and g y t l.jpg
Gx(t) and Gy(t)

Now consider Gx(t) and Gy(t) only.

Deja vu strikes, but we push on!

Let


K x and k y related to t l.jpg
kxand ky related to t

Let

As we move along in time (t) in the signal, we simply change where we are in kx, ky

(dramatic pause as students inch to edge of seats...)


K x and k y related to t 2 l.jpg
kxand ky related to t (2)

x

kx,

y

kyare reciprocal variables.

x,y are in cm, kx,kyare in cycles/cm or cycles/mm

Remarks:

1) S(t), our signal, are values of M along a trajectory in F.T. space.

- (called k-space in MR literature)

2) Integral of Gx(t), Gy(t), controls the k-space trajectory.

3) To image m(x,y), acquire set of S(t) to cover k-space and apply inverse Fourier Transform.


Spatial encoding summary l.jpg

What is ?

Spatial Encoding Summary

Receiver detects signal

Consider phase.

Frequency

is time rate of change of phase.

So


Spatial encoding summary16 l.jpg
Spatial Encoding Summary

But

So

Expanding,

We control frequency with gradients.

So,


Complex demodulation l.jpg
Complex Demodulation

  • The signal is complex. How do we realize this?

  • In ultrasound, like A.M. radio, we use envelope detection, which is phase-insensitive.

  • In MR, phase is crucial to detecting position. Thus the signal is complex. We must receive a complex signal. How do we do this when voltage is a real signal?


Complex demodulation18 l.jpg
Complex Demodulation

sr(t) is a complex signal, but our receiver voltage can only read a single

voltage at a time. sr(t) is a useful concept, but in the real world, we

can only read a real signal. How do we read off the real and imaginary

components of the signal, sr(t)?

Complex receiver signal

( mathematical concept)

The quantity s(t) or another representation,

is what we are after. We can write s(t) as a real and imaginary component, I(t) and Q(t)


Complex demodulation19 l.jpg
Complex Demodulation

An A/D converter reading the coil signal would read the real

portion of sr(t), the physical signal sp(t)


Complex demodulation20 l.jpg
Complex Demodulation

Inphase: I(t)

X

Low Pass Filter

sp(t)

cos(w0t)

X

Low Pass Filter

Quadrature: Q(t)

sin(w0t)

Let’s next look at the signal right after the multipliers. We can

consider the modulation theorem or trig identities.


Complex demodulation21 l.jpg
Complex Demodulation

Inphase: I(t)

X

Low Pass Filter

sp(t)

cos(w0t)

X

Low Pass Filter

Quadrature: Q(t)

sin(w0t)


Complex demodulation22 l.jpg
Complex Demodulation

Inphase: I(t)

X

Low Pass Filter

sp(t)

cos(w0t)

X

Low Pass Filter

Quadrature: Q(t)

sin(w0t)


Complex demodulation23 l.jpg
Complex Demodulation

The low pass filters have an impulse response that removes the

frequency component at 2w0 We can also consider them to have

gain to compensate for the factor ½.