2.0.0b10
catchment modelling framework
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A generic node-to-node gradient based connection. More...
A generic node-to-node gradient based connection.
This connection is similar to the Darcy-connection, but there are no restrictions concerning the type of nodes. However, the left side needs to be a water storage
\[ q = Q_1 \nabla \Psi \]
where:
Public Member Functions | |
LinearGradientFlux (cmf::water::flux_node::ptr left, cmf::water::flux_node::ptr right, real Q1, real d=-1.0) | |
Creates a generic gradient based flux, if enough water is present in the source. | |
real | conc (cmf::math::Time t, const cmf::water::solute &_Solute) |
Returns the concentration of the flux. | |
flux_node::ptr | get_target (const flux_node &inquirer) |
Returns the other end of a connection than the asking end. | |
flux_node::ptr | get_target (int index) const |
With index 0, the left node is returned, with index 1 the right node of the connection. | |
real | get_tracer_filter () |
A value ranging from 0 to 1 to filter tracers out of the water flux. | |
real | get_tracer_filter (solute S) |
A value ranging from 0 to 1 to filter tracers out of the water flux. | |
bool | kill_me () |
Deregisters this connection from its nodes. Returns true if only one reference is left. | |
flux_node::ptr | left_node () const |
Returns the left node of this connection. | |
real | q (const flux_node &inquirer, cmf::math::Time t) |
Returns the current flux through a connection. Negative signs mean out of the inquirer, positive are inflows to the inquirer. | |
void | refresh (cmf::math::Time t) |
Performes a new calculation of the flux. | |
flux_node::ptr | right_node () const |
returns the right node of this connection | |
void | set_tracer_filter (real value) |
A value ranging from 0 to 1 to filter tracers out of the water flux. | |
LinearGradientFlux | ( | cmf::water::flux_node::ptr | left, |
cmf::water::flux_node::ptr | right, | ||
real | Q1, | ||
real | d = -1.0 ) |
Creates a generic gradient based flux, if enough water is present in the source.
left | The left node of the connection |
right | The right node of the connection |
Q1 | Flux over the connection for a unity gradient ( \(\nabla \Psi = 1\)) in \(\frac{m^3}{day}\) |
d | the topographic lenght of the connection in m |
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inherited |
Returns the concentration of the flux.
If not overridden, it returns the concentration of the source of the flux (direction depending)
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inherited |
A value ranging from 0 to 1 to filter tracers out of the water flux.
1.0 is no filter and 0.0 means no solute is crossing this connection
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inherited |
A value ranging from 0 to 1 to filter tracers out of the water flux.
1.0 is no filter and 0.0 means no solute is crossing this connection