Soil-water budgets Considers all forms of soil moisture for a given region Indicates for plants how much moisture is available Components of soil-water budget Precipitation input (PRECIP) Actual evapotranspiration (ACTET) Potential evapotranspiration (POTET) Deficit (DEFIC) Surplus (SURPL) Soil-moisture storage (ΔSTRGE) Evapotranspiration Evaporation The change of liquid water into water vapor Transpiration A cooling mechanism in plants Evapotranspiration is therefore the release of water vapor from plants in order to cool them Evapotranspiration is highest on hot and sunny days Potential Evapotranspiration The amount of water that would be evapotranspired under specific temperature and moisture conditions This measurement ignores whether water is available for transpiration or not It is the DEMAND! INPUTS OUTPUTS Deficit Will occur if the requirements for potential evapotranspiration are not met Surplus Will occur if the requirements for potential evapotranspiration are met and there is extra moisture available Soil moisture storage Amount of moisture available to plants Change storage = amount of water taken from ST to help meet PE when P is lacking Water balance technique Precipitation (P) vs potential evapotranspiration (PE) P = AE + S + ST PE = AE + D AE = amount of water actually used by plants so if water is in good supply AE = PE…. IF WATER IS LACKING THEN AE = P + ST POTET Determining water budgets For each month the following can be plotted PRECIP POTET ACTET Water Balance Plants Once ST will not use more than PE PE is used up plants will take it from 1952 Mississippi 1952 IS IT A WET OR A DRY YEAR? J PE F M A M J JL A S O N D 1 1 1.2 2.3 4.6 7.1 7.3 6.2 4.3 1.5 1 0.5 P 3.5 3.1 5.5 2.3 3.2 0.3 2.1 2.7 1.2 0.3 2.7 4.6 P-PE 2.5 2.1 4.3 0 -1.4 -6.8 -5.2 -3.5 -3.1 -1.2 1.7 4.1 ST 6 6 6 6 4.6 0 0 0 0 0 1.7 5.8 ∆ST 0 0 0 0 -1.4 -4.6 0 0 0 0 1.7 4.1 AE 1 1 1.2 2.3 4.6 4.9 2.1 2.7 1.2 0.3 1 0.5 D 0 0 0 0 0 2.2 5.2 3.5 3.1 1.2 0 0 S 2.5 2.1 4.3 0 0 0 0 0 0 0 0 0