Chapter 4: Soil Water Properties Flashcards

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1
Q

Molecules like little magnets, have generally “+” and “-“ charged sides.

A

Polar

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2
Q

Molecules stick slightly to each other

A

Cohesion

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3
Q

Molecules stick to other charged molecules.

A

Adhesion

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4
Q

Forces holding or moving water in the soil.

A

Soil Water Potential

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5
Q

Water held to soil particles by hydrogen bonds.

A

Matric Potential

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6
Q

Water held to dissolved salts in soil solution.

A

Solute Potential

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7
Q

Gravity “pulling” water through the soil.

A

Gravitational Potential

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8
Q

Water that drains “freely” from soil, usually about 3 days after irrigation.

A

Gravitational Water

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9
Q

Amount of water (usually inches per foot of soil) held by soil after gravitational water drains off.

A

Field Capacity

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10
Q

Amount of water held in soil when plants are permanently damaged from water stress.

A

Permanent Wilting Point

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11
Q

Amount of water held in soil between field capacity and permanent wilting point.

A

Available Water Capacity

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12
Q

Many soils in __________ County are affected by salt.

A

Kern

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13
Q

The more negative the charge, the ____________ the bond.

A

Stronger

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14
Q

Clay is a “sponge” because of ____________.

A

Oxygen

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15
Q

Solute Potential is generally a ________ thing.

A

Bad

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16
Q

Solute Potential is very important to _________________.

A

Agriculture

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17
Q

All ________ __________ have a lot of oxygen radicals sticking out.

A

Living Things

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18
Q

Most crops can remove __________ of the water (on average).

A

Half

19
Q

Soil is __________ charged, so it sticks to water.

A

Negative

20
Q

Water is ____________ charged.

A

Positive

21
Q

High heat Capacity can ___________ crop production.

A

Extend

22
Q

Ice has a lot of _______ in it that insulates and protects lakes and other bodies of water.

A

Air

23
Q

Hydrogen parts of water __________ to soil.

A

Attach

24
Q

Sand has _______ negative charge.

A

Low

25
Q

Silt has a higher ____________ charge.

A

Negative

26
Q

Clay has a ________ negative charge.

A

High

27
Q

Field Capacity in an “average” AG soil = ______ Water of saturated soil.

A

1/2

28
Q

Available Water Capacity in an “average” AG soil = _____ field capacity.

A

1/2

29
Q

__________ ___________ have low field capacities, but may have moderate available Water holding capacity, because all water that is left after drainage is available.

A

Sandy soils

30
Q

__________ have highest field capacity, but low available water capacity, because waster held very tightly to clay particles.

A

Clays

31
Q

Best all around soil is the _________ soils with high field capacity and high available Water Capacity.

A

Loamy

32
Q

Weigh, dry, weigh again

  • slow, labor intensive
  • Good for lab samples that must be dried anyway
A

Gravimetric

33
Q

Air pressure pushes water out of soil

  • Pressure needed related to water content
  • Good for quick results in lab
A

Pressure Bomb

34
Q

2 electrodes, 1 cm apart, inside porous block. Conductivity related to water content of block; more water = more conductance.

  • Blocks can be buried in soil
  • Relatively cheap and fast and reliable
  • Inaccurate in salty soils
A

Porous Blocks

35
Q

Method where you will squeeze the soils with your hand to see if water drips from it or if it forms a ball. You can also roll the soil and see if it falls apart.

A

Soil feel method

36
Q

Device put down hole that emits fast neutrons. Neutrons that hit water are reflected, returned and are measured.

  • Proportion of slow to fast related to water content
  • Immediate results and 100% accurate
  • radioactive
  • you need to be licensed to do this method
A

Neutron Probe

37
Q

Water reflects radio waves (radar), much more that soil particles

  • Proportion of received to emitted waves estimates soil water
  • Very expensive equipment
  • Certain wave frequencies will penetrate the soil, and the frequency coming back will indicate the water content.
A

Radio Waves

38
Q

Tubes filled with water with a porous cup on the end. As water pulled out into dry soil from cup, water level in tube drops and measured by suction on meter

  • Relatively cheap
  • Not very accurate in dry soils
A

Tensiometers

39
Q

Moves by the force of gravity

  • Before the three days are over
  • Starts with infiltration and can end with deep percolation
A

“Free” or Saturated Flow

40
Q

___________ textured soils have much more saturated flow than ___________ textured soils.

A

Coarser; Finer

41
Q

_________ _________ increases saturated flow by keeping soil pores open.

A

Organic Matter

42
Q

Flow in soil pores from field capacity to permanent wilting point

A

Unsaturated Flow

43
Q

Unsaturated flow will flow from wetter to drier areas and can flow against gravity to bring up _________.

A

Salts