Soil Moisture, Groundwater Occurrence Flashcards
Layers in Vadose Zone (From upper to lower)
- Soil Water Belt
- Intermediate Belt
- Capillary Fringe
is the depression or the rise of a liquid in a small capillary passage tube having small cross sectional area such as openings in the porous materials
Capillarity
is the subsurface layer in which groundwater seeps up from a water table by capillary action to fill pores. Pores at the base of the capillary fringe are filled with water due too tension saturation
Capillary Fringe
Capillarity results from 2 forces
- mutual attraction (Cohesion) between water molecules
- molecular attraction (Adhesion) between water and different soil materials
- measuring instrument used to determine water potential (soil moisture tension) in the vadose zone
- Device typically consists of glass or plastic tube with porous ceramic cup and filled with water
Tensiometer
Soil moisture at a location varies with changes in the
amount of precipitation and evapotranspiration
H2O in the vadose zone available to growing plants, found in belt of soil water
Soil Water
when soil-moisture content of a layer reaches to the points at which the force of gravity acting on the water = the surface tension, gravity drainage cease.
Field capacity
the remaining moisture is too tightly bound the soil particles
Wilting point