Explanation of water-budget equation | Derivation of water-budget equation
Water- Budget Equation
The water- budget equation is nothing but the continuity equation
of water in its various phase at time Δt. For the given problem area, there can
be the various phases of water incoming and outgoing and the water-budget the equation simply balances the inflow and outflow of water in the equation.
For the given problem area at time Δt, continuity equation
for water in various phase is given by:
Mass inflow –
Mass outflow= change in Mass storage
This equation resembles with continuity equation because in
the continuity equation we assumed that mass accumulated is zero. And because
of that reason, the mass inflow was equal to mass outflow. But in this case, the mass
inflow and mass outflow are different and that difference is the mass storage.
However, the point is water-budget equation is the continuity equation and follows
the principle of conservation of mass.
If the density of the water inflow, water outflow and the
storage mass is the same, then the equation can be written as:
Volume inflow- Volume outflow = change in Volume
storage
Vi-Vo=
ΔS
Since the inflow and outflow occurs in different forms or
phase so, more precisely water-budget equation can be written as:
P-R-G-E-T=
ΔS
Where,
P=Precipitation
R=Surface Runoff
G= groundwater flow
E= evaporation
T= transpiration
So, in different phases or forms of loss and gain of water,
water budget equation is changed into
P-R-G-E-T= ΔS
Also, storage occurs in 3 forms they are stored as soil moisture,
storage as groundwater and storage as surface water storage.
So, ΔS=ΔSs+ΔSg+ΔSm
Where,
ΔSs= storage as surface water storage
ΔSg = storage as groundwater
ΔSm= storage as soil moisture
In terms of the rainfall-runoff relationship, the water-budget
equation can be written as
R=P-L
Where,
R= Runoff (storage)
P= Precipitation
L= All kind of losses due to evaporation, transpiration,
groundwater flow, etc.
So, the required water-budget equation is R=P-L
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