This process calculates the salt load and salinity of the water flowing out
of a particular channe as done in PCalcOldAcruCELRUN for the hydrological component.
This process is responsible to distribute salt load from an impervious area
into the adjacent river in the case of adjunct impervious areas or onto the
surrounding land segment in the case of disjunct impervious areas.
This process is responsible to transport salt carried along with the runoff water
from an irrigated area to either a reservoir or an out let of the catchment
depending on the location of the reservoir if one exists.
calculates the quantity of salt load added to an irrigated area based on the
volume of rain falling on the irrigated land and applied
irrigation water as well as their associated salinity.
This class is responsible to determine the quick flow salinity from
irrigated areas which is assumed to have the same value of TDS concentration as storm flow salinity.
This process is responsible to transport salt carried along with the percolating water
from one horizon to another and finaly to groundwater as well as to conduct subsurface salt balance computations in an irrigated area.
this process is responsible to determine the upward transport of salts from
the bottom horizon to the topsoil and finally to quick flow depending on the
occurence of saturated upward flow of water.
This process is responsible for distributing runoff salt load from
a land segment to the appropriate outflow components, such as a channel
and dam reaches, as is done with the hydrological process.
calculates the quantity of salt load added to a reservoir based on
the volume of rain falling on the reservoir surface as well as its associated salinity.
This class determines current reservoir storage salinity and outflow salinity
based on the two cell plug-flow (salt stacking) model as used by Herold (1980)
This process is responsible to determine the updated salinity level of a soil
layer or ground water after salt uptake took place according to first order
rate kinetics.
This process is responsible to determine quickflow salinity in non-irrigated lands based on the actual
quick flow salinity which is assumed as having same value as rainfall salinity
and the delayed stormflow salt load.
This process is responsible to transport salt carried along with the percolating
water from one horizon to another and finaly to groundwater in non irrigated area.
this process is responsible to determine the upward transport of salts from
groundwater through the subsoil and topsoil to quickflow depending on the
existence of saturated upward flow of water in non-irrigated lands.