2.0.0b10
catchment modelling framework
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A class to represent large groundwater storages, not bounded to the usual horizontal discretization scheme, the Cell. More...
A class to represent large groundwater storages, not bounded to the usual horizontal discretization scheme, the Cell.
Naturally aquifers are connected with aquifer_Darcy or kinematic_wave connections. As a boundary condition for a cell based soil water system, aquifers are used as a right hand side node of percolation connections.
Basic head ( \(\Psi\)) / volume ( \(V\)) relation:
\[ \Psi = z_{base} + \frac {V}{A \Phi} \]
Public Member Functions | |
aquifer (cmf::project &p, cmf::geometry::point position, real area, real thickness, real porosity, real K=1e-4) | |
Creates an aquifer at a certain position. | |
aquifer (cmf::upslope::cell_vector &cells, real thickness, real porosity, real K=1e-4) | |
Creates an aquifer below a collection of cells. | |
real | conc (cmf::math::Time t, const cmf::water::solute &_Solute) const override |
Returns the current WaterQuality (concentration of all solutes) | |
real | conc (const cmf::water::solute &_Solute) const |
Returns the concentration of the given solute. | |
void | conc (const cmf::water::solute &_Solute, real NewConcetration) |
Sets a new concentration. | |
cmf::water::flux_connection * | connection_to (const cmf::water::flux_node &target) |
Returns the connection between this and target. | |
virtual real | dxdt (const cmf::math::Time &time) |
Returns the derivate of the state variable at time time . | |
real | flux_to (const cmf::water::flux_node &target, cmf::math::Time t) |
Returns the actual flux between this and target (positive sign means "from this into target") | |
cmf::geometry::point | get_3d_flux (cmf::math::Time t) |
Returns the sum of all flux vectors. | |
real | get_base_height () const |
Returns the base height of the aquifer in m a.s.l. | |
virtual real | get_K (cmf::geometry::point direction) const |
Returns the conductivity in m/day for a specific direction. | |
real | get_potential (cmf::math::Time t=cmf::math::never) const override |
Returns the water potential of the node in m waterhead. | |
cmf::project & | get_project () const |
Returns the project, this node is part of. | |
real | get_state () const |
Returns the current state of the variable. | |
char | get_state_variable_content () const |
A character indicating the integrated variable (either 'V' for Volume or 'h' for head) | |
real | get_top_height () const |
Returns the top height of the aquifer in m a.s.l. | |
virtual real | get_volume () const |
Returns the volume of water in this storage in m3 | |
virtual bool | is_connected (const cmf::math::StateVariable &other) const |
Returns True if this waterstorage is effected by another state. | |
bool | is_storage () const override |
Returns true, since this is a storage. | |
real | operator() (cmf::math::Time t) const |
returns the waterblance | |
bool | remove_connection (cmf::water::flux_node::ptr To) |
Remove the connection. | |
virtual void | set_potential (real new_potential) |
Sets the potential of this flux node. | |
void | set_state (real newState) |
Gives access to the state variable. | |
void | set_state_variable_content (char content) |
A character indicating the integrated variable (either 'V' for Volume or 'h' for head) | |
virtual void | set_volume (real newwatercontent) |
Sets the volume of water in this storage in m3 | |
SoluteStorage & | Solute (const cmf::water::solute _Solute) |
Returns the water quality of the water storage. | |
real | waterbalance (cmf::math::Time t, const flux_connection *Without=0) const |
Returns the sum of all fluxes (positive and negative) at time t. | |
Static Public Member Functions | |
static aquifer::ptr | cast (cmf::water::flux_node::ptr for_cast) |
Casts a flux_node to an aquifer, if the flux_node is an aquifer. | |
Public Attributes | |
real | area |
The horizontal area of the aquifer. | |
cmf::geometry::point | K |
The conductivity in m/day for the three spatial dimensions. | |
std::string | Name |
The Name of this node. | |
const int | node_id |
The Id of the node. | |
real | porosity |
The porosity of the aquifer in m3/m3. | |
cmf::geometry::point | position |
The spatial position of the node. | |
real | thickness |
The thickness of the aquifer in m. | |
Protected Member Functions | |
void | MarkStateChangeHandled () |
Sets the updated flag (m_StateIsNew) to false. | |
bool | StateIsChanged () |
Returns if the state was currently updated. | |
Overrides of flux_node | |
virtual bool | RecalcFluxes (cmf::math::Time t) |
Pure flux_nodes do not influence fluxes, therefore no recalculation of fluxes is required by flux_node. | |
virtual double | is_empty () const |
Returns true if the node has no water. | |
aquifer | ( | cmf::project & | p, |
cmf::geometry::point | position, | ||
real | area, | ||
real | thickness, | ||
real | porosity, | ||
real | K = 1e-4 ) |
Creates an aquifer at a certain position.
p | Project, this aquifer belongs to |
position | Position of the aquifer center (x and y) and the aquifer top (z) |
area | Area of the aquifer |
thickness | Mean thickness of the aquifer in m |
porosity | Mean porositiy of the aquifer |
K | Conductivity of the aquifer in m/day. If the conductivity should be anisotropic, change the x,y and z values of the member K |
aquifer | ( | cmf::upslope::cell_vector & | cells, |
real | thickness, | ||
real | porosity, | ||
real | K = 1e-4 ) |
Creates an aquifer below a collection of cells.
cells | The cells above the aquifer. The area of the aquifer equals the area of the cells, and the upper boundary equals the soildepth of the lowest cell |
thickness | The thickness of the aquifer in m |
porosity | Porosity of the aquifer |
K | Conductivity of the aquifer in m/day. If the conductivity should be anisotropic, change the x,y and z values of the member K |
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virtual |
Returns the conductivity in m/day for a specific direction.
Takes account for anisotropy
\[ \|K\|(d) = \frac{d}{\|d\|} \bullet K\]
Implements conductable.
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overridevirtualinherited |
Returns the water potential of the node in m waterhead.
The base class water storage always returns the height of the location
Reimplemented from flux_node.
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virtualinherited |
Pure flux_nodes do not influence fluxes, therefore no recalculation of fluxes is required by flux_node.
WaterStorage overrides this, since state changes require an update of the fluxes
Reimplemented from flux_node.
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inherited |
Returns the sum of all fluxes (positive and negative) at time t.
Single fluxes can be excluded from the calculation
t | Time of the query |
Without | A flux_connection that is excluded from the waterbalance (e.g. to prevent closed circuits) |