Chapter 4: Soil Water Properties Flashcards

(43 cards)

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).

19
Q

Soil is __________ charged, so it sticks to water.

20
Q

Water is ____________ charged.

21
Q

High heat Capacity can ___________ crop production.

22
Q

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

23
Q

Hydrogen parts of water __________ to soil.

24
Q

Sand has _______ negative charge.

25
Silt has a higher ____________ charge.
Negative
26
Clay has a ________ negative charge.
High
27
Field Capacity in an "average" AG soil = ______ Water of saturated soil.
1/2
28
Available Water Capacity in an "average" AG soil = _____ field capacity.
1/2
29
__________ ___________ have low field capacities, but may have moderate available Water holding capacity, because all water that is left after drainage is available.
Sandy soils
30
__________ have highest field capacity, but low available water capacity, because waster held very tightly to clay particles.
Clays
31
Best all around soil is the _________ soils with high field capacity and high available Water Capacity.
Loamy
32
Weigh, dry, weigh again - slow, labor intensive - Good for lab samples that must be dried anyway
Gravimetric
33
Air pressure pushes water out of soil - Pressure needed related to water content - Good for quick results in lab
Pressure Bomb
34
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
Porous Blocks
35
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.
Soil feel method
36
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
Neutron Probe
37
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.
Radio Waves
38
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
Tensiometers
39
Moves by the force of gravity - Before the three days are over - Starts with infiltration and can end with deep percolation
"Free" or Saturated Flow
40
___________ textured soils have much more saturated flow than ___________ textured soils.
Coarser; Finer
41
_________ _________ increases saturated flow by keeping soil pores open.
Organic Matter
42
Flow in soil pores from field capacity to permanent wilting point
Unsaturated Flow
43
Unsaturated flow will flow from wetter to drier areas and can flow against gravity to bring up _________.
Salts