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Lecture 3: The Bloch Equations Solved & the MR Signal Equation Solve the Bloch equation –Precession –T2 relaxation –T1 relaxation MR signal equation –Understand.

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Presentation on theme: "Lecture 3: The Bloch Equations Solved & the MR Signal Equation Solve the Bloch equation –Precession –T2 relaxation –T1 relaxation MR signal equation –Understand."— Presentation transcript:

1 Lecture 3: The Bloch Equations Solved & the MR Signal Equation Solve the Bloch equation –Precession –T2 relaxation –T1 relaxation MR signal equation –Understand how magnetization changes phase due to gradients –Understand MR image formation or MR spatial encoding

2 Bloch Equations – Homogenous Material It’s important to visualize the components of the vector M at different times in the sequence. a)Let us solve the Bloch equation for some interesting cases. In the first case, let’s use an arbitrary M vector, a homogenous material, and consider only the static magnetic field. b)Ignoring T1 and T2 relaxation, consider the following case. Solve

3 The Solved Bloch Equations Solve

4 The Solved Bloch Equations A solution to the series of differential equations is: Next we allow relaxation. where M 0 refers to the initial conditions. M0 refers to the equilibrium magnetizataion. This solution shows that the vector M will precess about the B0 field.

5 Solution: Longitudinal Magnetization Component The greater the difference from equilibrium, the faster the change Solution: Initial Mz Return to Equilibrium

6 Solution: Longitudinal Magnetization Component initial conditions equilibrium Example: What happens with a 180° RF flip? t MoMo -M o Effect of T 1 on relaxation - 180° flip angle

7 Complex m m is complex. m =M x +iM y Re{m} =M x Im{m}=M y This notation is convenient: It allows us to represent a two element vector as a scalar. Re Im m MxMx MyMy

8 Transverse Magnetization Component The transverse magnetization relaxes in the Bloch equation according to This is a decaying sinusoid. t We continue to study the transverse magnetization. Why? Transverse magnetization gives rise to the signal we “readout”. Solution to this equation is :

9 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.

10 Transverse Magnetization Equation We can number the terms above 1-4 1. - variation in proton density 2. - spatial variation due to T 2 3.- rotating frame frequency - “carrier” frequency of signal 4. - spins will precess at differential frequency according to the gradient they experience (“see”).

11 Transverse Magnetization Equation Phase is the integral of frequency. - spins will precess at differential frequency according to the gradient they “see”. 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.

12 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

13 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

14 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.

15 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.

16 Receiving the signal (2) 3) Demodulate to baseband. i.e. zozo slice thickness  z Let’s simplify this: 1) Ignore T 2 for now; it will be easy to add later. 2) Assume 2D imaging. (Again, it will be easy to expand to 3 later.) S(t) is complex.

17 Receiving the signal (3) 3) Demodulate to baseband. i.e. S(t) is complex. Then, end goal

18 G x (t) and G y (t) Now consider G x (t) and G y (t) only. Deja vu strikes, but we push on! Let

19 k x and k y related to t Let As we move along in time (t) in the signal, we simply change where we are in k x, k y (dramatic pause as students inch to edge of seats...)

20 k x and k y related to t (2) x,y are in cm, k x,k y are in cycles/cm or cycles/mm kx,kx,k y are reciprocal variables.xy 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 G x (t), G y (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.

21 Spatial Encoding Summary Consider phase. Receiver detects signal What is ? Frequencyis time rate of change of phase. So

22 Spatial Encoding Summary So But Expanding, We control frequency with gradients. So,

23 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?

24 Complex Demodulation s r (t) is a complex signal, but our receiver voltage can only read a single voltage at a time. s r (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, s r (t)? Or the in-phase and quadrature components? Complex receiver signal ( mathematical concept) The quantity s(t) or another representation, is what we are after. We can write s(t) as an inphase and quadrature component, I(t) and Q(t)

25 Complex Demodulation An A/D converter reading the coil signal would read the real portion of s r (t), the physical signal s p (t)

26 Complex Demodulation s p (t) X X cos(   t) Inphase: I(t) Quadrature: Q(t) sin(   t) Low Pass Filter Let’s next look at the signal right after the multipliers. We can consider the modulation theorem or trig identities.

27 Complex Demodulation s p (t) X X cos(   t) Inphase: I(t) Quadrature: Q(t) sin(   t) Low Pass Filter

28 Complex Demodulation s p (t) X X cos(   t) Inphase: I(t) Quadrature: Q(t) sin(   t) Low Pass Filter

29 Complex Demodulation The low pass filters have an impulse response that removes the frequency component at 2   We can also consider them to have gain to compensate for the factor ½.


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