Soil Moisture, Groundwater Occurrence Flashcards

1
Q

Layers in Vadose Zone (From upper to lower)

A
  • Soil Water Belt
  • Intermediate Belt
  • Capillary Fringe
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2
Q

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

A

Capillarity

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3
Q

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

A

Capillary Fringe

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4
Q

Capillarity results from 2 forces

A
  • mutual attraction (Cohesion) between water molecules
  • molecular attraction (Adhesion) between water and different soil materials
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5
Q
  • 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
A

Tensiometer

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6
Q

Soil moisture at a location varies with changes in the

A

amount of precipitation and evapotranspiration

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7
Q

H2O in the vadose zone available to growing plants, found in belt of soil water

A

Soil Water

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8
Q

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.

A

Field capacity

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9
Q

the remaining moisture is too tightly bound the soil particles

A

Wilting point

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10
Q
A
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