Non-homogenous convection equation

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In summary, the conversation discusses potential solutions to the PDE $$u_t + u_x = f(x,t)$$ with a specific focus on the case where ##f(x,t) = \delta(x-at)/(x-at)##. The method of characteristics is suggested as a possible approach, with a proposed substitution of ##\dfrac{x-at}{\varepsilon} =:y##. However, there are still challenges in dealing with the inhomogeneous RHS, and solving all ODEs explicitly is necessary.
  • #1
member 428835
Does anyone know if there are solutions to the following PDE

$$u_t + u_x = f(x,t)$$

If not in a general context, what if ##f(x,t) = \delta(x-at)/(x-at)##? Please let me know if you have any information.

Method of characteristics?
 
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  • #2
I would substitute ##\dfrac{x-at}{\varepsilon} =:y## and with ##\dfrac{dy}{dx}\; , \;\dfrac{dy}{dt}## known, there should be a way to solve it. Just an idea.
 
  • #3
fresh_42 said:
I would substitute ##\dfrac{x-at}{\varepsilon} =:y## and with ##\dfrac{dy}{dx}\; , \;\dfrac{dy}{dt}## known, there should be a way to solve it. Just an idea.
A good idea, but this just implies any function of the form ##g(x-at)## is a homogenous solution. How do you deal with the inhomogenous RHS?
 
  • #4
Well the method of characteristics gives you
$$ \frac{dt}{ds}=1 \rightarrow t(r,s)=s+C_1(r)$$
$$\frac{dx}{ds}=1 \rightarrow x(r,s)=s+ C_2(r)$$
$$\frac{du}{ds}=f(x,t) \rightarrow u(r,s)=\int f(s+C_2(r),s+C_1(r)) ds + C_3(r)$$

So if you know the boundary conditions you can substitute them and try to solve all ode's explicitly. If the BC is $$u(x,0)=\phi(x)$$ your BC's can be written as
$$x(r,0) = r \rightarrow C_2(r) = r $$
$$t(r,0) = 0 \rightarrow C_1(r) = 0$$
$$u(r,0) = \phi(r) \rightarrow C_3(r) = \phi(r) - \int f(r,0)ds$$

and you can substitute ##s=t## and ##r=x-t## in the equation for ##u##. Hope this helps. I have used the notation from:
https://web.stanford.edu/class/math220a/handouts/firstorder.pdf
 

What is the non-homogenous convection equation?

The non-homogenous convection equation is a mathematical equation used to describe the transport of a quantity (such as heat or mass) in a fluid medium that is undergoing convection. It takes into account both the convection of the fluid and any sources or sinks of the quantity being transported.

How is the non-homogenous convection equation different from the homogenous convection equation?

The non-homogenous convection equation includes additional terms to account for the sources or sinks of the transported quantity, while the homogenous convection equation assumes a constant source or sink term. This makes the non-homogenous convection equation more versatile and applicable to a wider range of scenarios.

What is the significance of the non-homogenous term in the convection equation?

The non-homogenous term represents the sources or sinks of the transported quantity, which can have a significant impact on the overall transport process. It allows for a more accurate and realistic representation of the system being studied.

What are some applications of the non-homogenous convection equation?

The non-homogenous convection equation has numerous applications in various fields, including fluid dynamics, heat transfer, atmospheric science, and chemical engineering. It is commonly used to model the transport of pollutants in the environment, the cooling of electronic devices, and the mixing of fluids in industrial processes.

How is the non-homogenous convection equation solved?

The non-homogenous convection equation can be solved using various numerical methods, such as finite difference, finite volume, or finite element methods. These methods involve discretizing the equation into a system of equations that can be solved iteratively to obtain a numerical solution. Analytical solutions are also possible for simplified cases of the equation.

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