One of BioDynaMo's built-in biological processes is extracellular diffusion. It is the process of extracellular substances diffusing through space. The constants that govern the diffusion process can be set by the user. Let's go through an example where diffusion plays a role.

### Copy the demo code

`diffusion`

is one of many installed demos in BioDynaMo. It can be copied out
with `biodynamo demo`

.

`biodynamo demo diffusion .`

### Inspect the code

Go into the `diffusion`

directory and open the source file `src/diffusion_biology_modules.h`

in your favorite editor.
We can note the following things from its content:

#### 1. Substance list

`enum Substances { kKalium };`

The extracellular substances that will be used in the simulation are listed in
an `enum`

data structure. In this case it is just a single substance. According to our C++
coding style we will prepend the substance's name with the letter "k".

#### 2. Biology modules

In the same file you can find the definition of the biology modules `Chemotaxis`

and `KaliumSecretion`

. These are the modules that will govern the
behavior of the simulation objects (i.e. cells).

#### 3. Initial model

Open the `src/diffusion.h`

source file.

First, create a BioDynaMo simulation:

`Simulation simulation(argc, argv);`

Next up is creating the initial model of our simulation. Therefore, we have to create an initial set of simulation objects and set their attributes:

```
auto construct = [](const Double3& position) {
Cell* cell = new Cell(position);
cell->SetDiameter(30);
cell->SetMass(1.0);
cell->AddBiologyModule(new Chemotaxis());
Double3 secretion_position = {{50, 50, 50}};
if (position == secretion_position) {
cell->AddBiologyModule(new KaliumSecretion());
}
return cell;
};
std::vector<Double3> positions;
positions.push_back({0, 0, 0});
positions.push_back({100, 0, 0});
positions.push_back({0, 100, 0});
positions.push_back({0, 0, 100});
positions.push_back({0, 100, 100});
positions.push_back({100, 0, 100});
positions.push_back({100, 100, 0});
positions.push_back({100, 100, 100});
// the cell responsible for secretion
positions.push_back({50, 50, 50});
ModelInitializer::CreateCells(positions, construct);
```

The `construct`

lambda defines the properties of each cell that we create. These can be
physical properties (diameter, mass), but also biological properties and behaviors
(chemotaxis, substance secretion)

In this example, each cell is assigned the `Chemotaxis`

behavior. In `diffusion_biology_behaviors.h`

you can
check the source code of this module. Basically it makes cells move according to the gradient,
caused by a concentration difference of the substance. One of the cells
(the cell at position `{50, 50, 50}`

) will be the one secreting the substance;
it therefore gets assigned the `SubstanceSecretion`

behavior.

Furthermore, we define the initial positions of the cells. In this example it is done explicitly, but one could also generate a grid of cells, or a random distribution of cells.

### Simulation Parameters

Create a `bdm.toml`

file in the `diffusion`

directory, and copy the following lines
into it:

```
[visualization]
export = true
export_interval = 10
[[visualize_sim_object]]
name = "Cell"
additional_data_members = [ "diameter_" ]
[[visualize_diffusion]]
name = "Kalium"
gradient = true
```

This will enable exporting visualization files, so that we can visualize the simulation after it has finished. Furthermore, we enable the output of the diameter of our simulation objects (by default named "Cell"), and the gradient data of the extracellular diffusion

### Build and run the simulation

Run the following commands to build and run the simulation.

`biodynamo run`

### Visualize the simulation

Load the generated ParaView state file as described in Section Visualization.

From "View", select "Animation Panel". This will display some animation settings at the bottom of the screen. From the "Mode" select "Real Time". Then click the Play button at the top of the screen to run the simulation visualization.

### Diffusion parameter constraints

The differential equations that describe the diffusion are solved in an analytical way using the central difference method as shown in the figure below:

The diffusion coefficient dictates the speed of diffusing a substance through space, while with the decay constant one controls the speed at which a substance decays. Mathematically, the method would allow for unphysical behavior to occur, such as negative concentration values. In order to avoid such behavior from happening, we impose the following constraint on the parameters:

Since as a user, you are giving the resolution of the diffusion grid and not the
distance between the grid points, you can determine this value by dividing the
longest dimension of your space by the resolution, or by calling the corresponding
function `DiffusionGrid::GetBoxLength()`

.

For more information on the inner workings of the diffusion module, please refer to: https://repository.tudelft.nl/islandora/object/uuid%3A2fa2203b-ca26-4aa2-9861-1a4352391e09?collection=education

### Runge-Kutta method:

We have additionally implemented the 2nd order Runge-Kutta method within BioDynaMo. The Runge-Kutta method is an iterative method for solving ordinary differential equations (ODEs), both implicitly and explicitly. Often outperforming the Euler method for complex ODEs. Unlike the Euler method which estimates the next time step based on the rate of change of the defined ODE at the current point, the Runge-Kutta method is a family of schemes which involve slope calculations between the current and next time step, with the number of slope estimates depending on the order of the Runge-Kutta method being utilised.

In the case of the 2nd order Runge-Kutta method implemented here, a slope estimate is taken at the midpoint between the current and next time step, in addition to utilising the rate of change at the current time step.

The Runge-Kutta method solves ODEs of the form:

We estimate a solution explicitly using the following steps:

Here k1 is the slope at the beginning of the interval and k2 is the slope at the midpoint of the interval. With h determining interval length being solved for.

For example, with a h value of 1, we would be estimating between the current time step t to t+1 with a single midpoint slope estimate. For most ODEs increasing the number of intervals to be taken per time step increases overall accuracy, as we will be taking a greater number of midpoint slope estimates between t to t+1.

So, if we instead set h = 0.5, the method will first estimate over t to t + 0.5 with a midpoint slope estimate, repeating this for t + 0.5 to t + 1 with a second midpoint slope estimate. However, there is a trade-off taken here with increased computational time for increasing accuracy.

As stated, the higher order Runge-Kutta methods often outperform lower order solvers for ODEs, however this does not happen for the currently implemented version of chemical diffusion. This is due to the fact that when one breaks down the partial differential equations (PDEs) that define chemical diffusion into the set of ODEs that define equation 3.1, the time dependant variable is lost on the right hand side of the equation. This results in the extra steps being taken for the Runge-Kutta method having minimal impact as there is no time dependant variable to estimate the slope from.

Within BioDynaMo the number of intervals for the Runge-Kutta method to iterate over per time step can be set within the declaration of a diffusion grid itself as follows:

```
DiffusionGrid* d_grid = new DiffusionGrid(substance_id, "substance_name", diffusion_coefficient,
decay_constant, resolution, diffusion_step)
```

Note:

- The entered value for the diffusion_step is required to be a positive integer value of greater than 0.

To access the Runge-Kutta method for diffusion, one simply needs to update the bdm.toml file as follows :

```
[simulation]
diffusion_type_ = "RK"
[visualization]
export = true
export_interval = 10
diffusion_type = "RK"
[[visualize_sim_object]]
name = "Cell"
additional_data_members = [ "diameter_" ]
[[visualize_diffusion]]
name = "Kalium"
gradient = true
```

Note:

- This method requires the input of known initial boundary conditions for the ODE being solved.
- This method is also commonly referred to as the midpoint method or improved Euler.
- This method can additionally be used to solve partial differential equations (PDEs) but requires each component to be individually broken down into separate ODEs.