Water Storage and Movement Flashcards
water storage is affected by
unique chemical structure of water, neg charge of clay, combination of adhesion and cohesion
stauration
point where water fills all pore spaces leaving no room for air. water moves through soil profile due to gravity
field capacity
max amount of water that can be held in the soil against the force of gravity
permanent wilting point
air takes up most of the pores and the water is held to soil so tightly that plants can’t access it
plant available water
difference between field capacity and permanent wilting point
gravitational/saturated flow
rapid movement through macropores only flowing down
capillary/unsaturated flow
water movement through adhesion and cohesion through micropores can flow in any direction