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Surface Balance = Supply – Demand ± Surplus/Deficit
The balance between how much of something is available (supply) and how much is needed or used (demand).
Effects of Water Surpluses
Recharge soil moisture
Recharge deeper groundwater
Become runoff
Supply: Precipitation
atmosphere to oceans/land
Demand: Evaporation
oceans/land to atmosphere
Demand: Transpiration
plants to atmosphere
Surplus: Runoff
land to oceans
Potential Evapotranspiration (PET)
Maximum amount of water that could evaporate from the ground and be released by plants
Actual Evapotranspiration (AET)
Amount of water that actually evaporates from the ground and is released by plants
Precipitation (P)
Water that falls from the atmosphere
Evapotranspiration (ET)
Water that returns to atmosphere
→ Evaporation from surfaces, Transpiration from plants
Percolation
Gravitational pull of water downwards through pore space in soil and rock
Porosity
Amount of pore space in rock or sediments
Permeability
Degree of connectedness among pores
Groundwater Mining
Removing water faster than nature can replace it