Calculating Tree Amplitude for Spin J Exchange

In summary, tree amplitude is a mathematical quantity that represents the probability amplitude for a particular spin exchange process in a tree-level Feynman diagram. It is calculated using perturbation theory and is affected by factors such as coupling strength, spin, energy, and momentum. It is important because it allows us to calculate the cross section for a given spin exchange process and make predictions about its likelihood of occurring. Additionally, tree amplitude is directly related to the scattering amplitude, which takes into account the initial and final states of the particles involved and any symmetry factors.
  • #1
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I am wondering something about the tree amplitude for exchange of a spin J resonance-- the basic calculation that exhibits the famous regge behavior. I see that one way to do the calculation is simply to note that the 4-point function for spin J exchange amongst massless particles arises from an interaction term with J derivatives, and hence J powers of momenta, from which we immediately infer that the t-channel amplitude is of the form
s^J/(t-M^2) + ... . However another method appears in the literature, which seems to be a partial wave expansion, noting that the spin J term of the expansion for the scattering amplitude is of the form (2J+1) f(t) P_J(cos \theta), where P_J (\cos(\theta) is the Legendre polynomial of spin J and \theta is the angle between the incoming t-channel particles. The asymptotic large s behavior can then be obtained by noting that cos(\theta) --> s/4m^2, and then that P_J (\cos (theta)) --> (cos \theta)^J --> s^J.

My question is why the two methods? Why does anyone use partial waves if it is so much simpler to get the result from field theory? And this is a very basic question, but what is the validity of a partial wave expansion in a field theory context?
 
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Thank you for your question regarding the calculation of the tree amplitude for exchange of a spin J resonance. I can explain the reasoning behind the two methods you mentioned and discuss the validity of a partial wave expansion in a field theory context.

The first method you mentioned, using field theory, is based on the interaction term with J derivatives in the 4-point function for spin J exchange. This method is commonly used because it is relatively straightforward and can provide a direct calculation of the amplitude. However, it is important to note that this method assumes that the particles involved are massless, and therefore may not be applicable in all scenarios.

The second method, using a partial wave expansion, is based on the idea that the scattering amplitude can be expressed as a sum of terms with different spin projections. This method is commonly used in the context of quantum field theory because it allows for a more general treatment of the problem, including cases where the particles involved have non-zero masses. It also provides a way to analyze the behavior of the amplitude at different angles, which can be useful in certain scenarios.

Now, why do some scientists choose to use the partial wave expansion method instead of the field theory method? This can depend on the specific problem they are trying to solve. In some cases, the field theory method may be more appropriate and simpler, as you noted. However, in other cases, the partial wave expansion method may provide a more general and flexible approach, allowing for a better understanding of the underlying physics.

Regarding the validity of a partial wave expansion in a field theory context, it is important to note that this method is based on the principles of quantum field theory. As such, it is a valid approach that has been widely used in many different contexts and has been shown to provide accurate results. However, as with any theoretical framework, it is important to consider the assumptions and limitations of the method and to use it appropriately.

In summary, both the field theory method and the partial wave expansion method have their strengths and limitations. Scientists may choose to use one or the other depending on the specific problem they are trying to solve. The validity of the partial wave expansion in a field theory context is supported by its use in many successful calculations and its consistency with the principles of quantum field theory. I hope this helps to answer your questions.
 

Related to Calculating Tree Amplitude for Spin J Exchange

1. How do you define tree amplitude in spin J exchange calculations?

Tree amplitude is a mathematical quantity that represents the probability amplitude for a particular spin exchange process in a tree-level Feynman diagram. It is calculated by summing over all possible intermediate states and integrating over the phase space variables.

2. Why is it important to calculate tree amplitude in spin J exchange?

Tree amplitude is important because it allows us to calculate the cross section for a given spin exchange process, which is a measure of how likely the process is to occur. This information is crucial for understanding and predicting the behavior of particles in high-energy collisions.

3. How is tree amplitude calculated in spin J exchange?

Tree amplitude is calculated using perturbation theory, which involves expanding the amplitude in a series of terms and calculating each term using Feynman rules. The tree-level amplitude is then obtained by summing over all possible intermediate states and integrating over the phase space variables.

4. What factors affect the value of tree amplitude in spin J exchange?

The value of tree amplitude is affected by several factors, including the coupling strength of the interaction, the spin of the particles involved, and the energy and momentum of the incoming particles. Higher order corrections and loop diagrams can also affect the value of tree amplitude.

5. How is tree amplitude related to scattering amplitudes in spin J exchange calculations?

Tree amplitude is directly related to the scattering amplitude for a given spin exchange process. The scattering amplitude is obtained by multiplying the tree amplitude with a factor that takes into account the initial and final states of the particles involved, as well as any symmetry factors. This allows us to calculate the cross section for the process and make predictions about its likelihood of occurring.

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