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: | ||
- | '' 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.'' | + | '' 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: | ||
- | \[ \frac{\partial n}{\partial t} (x,t) = - \frac{\partial J}{\partial x} (x,t) | + | \[ \frac{\partial n}{\partial t} (x,t) = - \frac{\partial J}{\partial x} (x,t) \qquad (2) \] |
- | By replacing (2) in (1), we obtain the following '''equation of diffusion''' | + | By replacing $(2)$ in $(1)$, we obtain the following '''equation of diffusion''' |
- | \[ \bigg( \frac{\partial}{\partial t} - D \frac{\partial^2}{\partial x^2} \bigg) n(x,t) = 0 \] | + | \[ \bigg( \frac{\partial}{\partial t} - D \frac{\partial^2}{\partial x^2} \bigg) n(x,t) = 0 \qquad (3) \] |
{{Team:Paris_Saclay/default_footer}} | {{Team:Paris_Saclay/default_footer}} |
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 \[ \bigg( \frac{\partial}{\partial t} - D \frac{\partial^2}{\partial x^2} \bigg) n(x,t) = 0 \qquad (3) \]