Team:Paris Saclay/Modeling

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We use the following phenomenological law suggest by Adolphe Fick in 1855:
We use the following phenomenological law suggest by Adolphe Fick in 1855:
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'' In an homogeneous and isotropic environment, containing particles distributed inhomogeneously,appears spontaneously a volumetric flow density vector particle $\overrightarrow{J}(M,t) $. In any point $M$ in space, this vector is proportional to the gradient of the particle density $n(M,t)$. Mathematicaly, this relationship take the form:  \[  \overrightarrow{J}(M,t) = - D  \times \overrightarrow{grad}  n(M,t) \]  where $D$ is the diffusion coefficient.''
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'' In an homogeneous and isotropic environment, containing particles distributed inhomogeneously,appears spontaneously a volumetric flow density vector particle $\overrightarrow{J}(M,t) $. In any point $M$ in space, this vector is proportional to the gradient of the particle density $n(M,t)$. Mathematicaly, this relationship take the form:  \[  \overrightarrow{J}(M,t) = - D  \times \overrightarrow{grad}  n(M,t) \qquad (1) \]  where $D$ is the diffusion coefficient.''
article ----> case of agarose $ D = 0{,}256 \times 10^{-8} m^2 s^{-1} $  
article ----> case of agarose $ D = 0{,}256 \times 10^{-8} m^2 s^{-1} $  
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* To simplify the problem, we consider that the diffusion of oxygen particle occurs only in one direction. So $\overrightarrow{J}(M,t) = J(x,t) \overrightarrow{e}_x $.
* To simplify the problem, we consider that the diffusion of oxygen particle occurs only in one direction. So $\overrightarrow{J}(M,t) = J(x,t) \overrightarrow{e}_x $.
* The material's equation of conservation in lack of source:  
* The material's equation of conservation in lack of source:  
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\[ \frac{\partial n}{\partial t} (x,t) = - \frac{\partial J}{\partial x} (x,t) \]
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\[ \frac{\partial n}{\partial t} (x,t) = - \frac{\partial J}{\partial x} (x,t) \qquad (2) \]
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By replacing (2) in (1), we obtain the following '''equation of diffusion'''
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By replacing $(2)$ in $(1)$, we obtain the following '''equation of diffusion'''
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\[ \bigg(  \frac{\partial}{\partial t} - D \frac{\partial^2}{\partial x^2} \bigg) n(x,t) = 0 \]
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\[ \bigg(  \frac{\partial}{\partial t} - D \frac{\partial^2}{\partial x^2} \bigg) n(x,t) = 0 \qquad (3) \]
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Revision as of 16:18, 8 August 2014

Modeling

To realise our artwork, we use an agarose gel to obtain the shape of a lemon. To push the resemblance to the extreme, we wish to have a crust in the edge of the lemon when we seperate it. In fact, we build bacteria who produce yellow/green color in presence of oxygen. Thus we must evaluate the penetration of the oxygen in the gel !

We use the following phenomenological law suggest by Adolphe Fick in 1855:

In an homogeneous and isotropic environment, containing particles distributed inhomogeneously,appears spontaneously a volumetric flow density vector particle $\overrightarrow{J}(M,t) $. In any point $M$ in space, this vector is proportional to the gradient of the particle density $n(M,t)$. Mathematicaly, this relationship take the form: \[ \overrightarrow{J}(M,t) = - D \times \overrightarrow{grad} n(M,t) \qquad (1) \] where $D$ is the diffusion coefficient.

article ----> case of agarose $ D = 0{,}256 \times 10^{-8} m^2 s^{-1} $

  • To simplify the problem, we consider that the diffusion of oxygen particle occurs only in one direction. So $\overrightarrow{J}(M,t) = J(x,t) \overrightarrow{e}_x $.
  • The material's equation of conservation in lack of source:

\[ \frac{\partial n}{\partial t} (x,t) = - \frac{\partial J}{\partial x} (x,t) \qquad (2) \]

By replacing $(2)$ in $(1)$, we obtain the following equation of diffusion \[ \bigg( \frac{\partial}{\partial t} - D \frac{\partial^2}{\partial x^2} \bigg) n(x,t) = 0 \qquad (3) \]