roam
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Thank you very much for your input.
I see. I guess we used z=0 because at short times the heat hasn't really traveled much into the stem.
If water is substituted for tissue (a zero-order approximation), do you know for what sort of timescales each of the equations in post #25 are valid?
So ##\theta_{\infty}(t,z)## is valid for long times t, and also for long z (far removed from heat source ##q##)?
So, when we write ##Q=I \alpha## doesn't that already account for the attenuation? Isn't this what you mean by the attenuation of I?
The attenuation coefficient of a sample is related to the absorption coefficient through:
$$\gamma=\underbrace{\alpha}_{\text{absorption coefficient}}+\underbrace{\beta}_{\text{scattering coefficient}}$$
Chestermiller said:The equation in post #22 is just what this equation predicts at z = 0.
I see. I guess we used z=0 because at short times the heat hasn't really traveled much into the stem.
If water is substituted for tissue (a zero-order approximation), do you know for what sort of timescales each of the equations in post #25 are valid?
Chestermiller said:No. It is the spatial part of the asymptotic temperature variation at long times.
So ##\theta_{\infty}(t,z)## is valid for long times t, and also for long z (far removed from heat source ##q##)?
Chestermiller said:q is the integral of Q over the length of the stem. That is ##q=\int_0^L{Qdz}## (Don't forget to include the attenuation of I)
So, when we write ##Q=I \alpha## doesn't that already account for the attenuation? Isn't this what you mean by the attenuation of I?
The attenuation coefficient of a sample is related to the absorption coefficient through:
$$\gamma=\underbrace{\alpha}_{\text{absorption coefficient}}+\underbrace{\beta}_{\text{scattering coefficient}}$$