Chapter 6 Soil water Flashcards

(77 cards)

1
Q

When dry soil is crushed in the hand, it can be seen that it is composed of

A

all kinds of particles of different sizes.

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2
Q

When dry soil is crushed in the hand, it can be seen that it is composed of all kinds of particles of different sizes.

Most of these particles originate from

A

degradation of rocks; they are called mineral particles.

Some originate from residues of plants or animals (rotting leaves, pieces of bone, etc.), these are called organic particles (or organic matter).

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3
Q

The soil particles seem to touch each other, but in reality have

A

spaces in between.

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4
Q

The soil particles seem to touch each other, but in reality have spaces in between. These spaces are called

A

pores

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5
Q

When the soil is “dry”, the pores are mainly filled with

A

air

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6
Q

After……………………………………….., the pores are mainly filled with water

A

irrigation or rainfall

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7
Q

Living material is found in the soil. It can be …………………………………………………………..

A

live roots as well as beetles, worms, larvae etc.

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8
Q

living materials help to…………………….. and thus……………………………………………..

A

aerate the soil and thus create favourable growing conditions for the plant roots

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9
Q

The following image represents

A

The composition of the soil

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10
Q

A represents

A

Soil Particles

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11
Q

B represents

A

water

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12
Q

C represents

A

air

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13
Q

D represents

A

root

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14
Q

If a pit is dug in the soil,………………………………………………………………………….. can be seen.

A
  1. At least 1 m deep,
  2. Various layers,
  3. Different in colour and composition
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15
Q

If a pit is dug in the soil, at least 1 m deep, various layers, different in colour and composition can be seen. These layers are called

A

horizons

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16
Q

the profile of the soil:

A

succession of horizons

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17
Q

soil profile:

A
  1. The plough layer
  2. The deep plough layer
  3. The subsoil layer
  4. The parent rock layer
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18
Q

The following image represent the

A

Soil profile

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19
Q

A represent

A

Plough layer

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20
Q

B represents

A

Deep plough layer

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21
Q

C represents

A

Subsoil layer

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22
Q

D represents

A

The parent rock layer

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23
Q

Name of the particles:

gravel

Size limits in mm:

A

larger than 1

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24
Q

Name of the particles

gravel

distinguishable with the naked eye:

A

Obviously

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25
**Name of the particles:** sand **size** **limit** **in mm:**
1 to 0.5
26
**Name of the particles:** sand **Distinguishable with naked eye:**
easily
27
**Name of the particles:** silt **Size limits in mm:**
0.5 to 0.002
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**Name of the particles:** silt **Distinguishable with naked eye**
barely
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**Name of the particles:** clay **Size limits in mm:**
less than 0.002
30
**Name of the particles:** clay **Distinguishable with the naked eye:**
impossible
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......................................determines the soil texture.
The amount of sand, silt and clay present in the soil
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In ............................textured soils: .............................. is predominant (sandy soils).
coarse sand
33
In ......................... textured soils: ...................is predominant (loamy soils).
medium silt
34
In .......................textured soils: .......................is predominant (clayey soils).
fine clay
35
In the field, soil texture can be determined by
rubbing the soil between the fingers
36
Soil structure refers to or soil structure refers to
the grouping of soil particles (sand, silt, clay, organic matter and fertilizers) into porous compounds. These are called aggregates or Soil structure also refers to the arrangement of these aggregates separated by pores and cracks
37
When present in the topsoil, a massive structure
blocks the entrance of water
38
When present in the topsoil, a massive structure blocks the entrance of water; seed germination is difficult due to
poor aeration
39
if the topsoil is ....................................., the water enters easily and the seed germination is better
granular
40
The following soil structure is
Grangular
41
The following soil structure is
Blocky
42
The following soil structure is
Prismatic
43
The following soil structure is
Massive
44
In Granular soil structure the flow is ..........................
rapid
45
In Blocky soil structure the flow is ..........................
moderate
46
In Prismatic soil structure the flow is ..........................
moderate
47
In Massive soil structure the flow is ..........................
Slow
48
The depth of the ..........................................varies greatly from place to place, mainly due to changes in ......................................
groundwater table topography of the area
49
In one particular place or field, the depth of the groundwater table may vary in ............
time
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A perched groundwater layer can be found
on top of an impermeable layer rather close to the surface (20 to 100 cm)
51
A perched groundwater layer can be found on top of an impermeable layer rather close to the surface (20 to 100 cm). It covers usually a .......................area.
limited
52
The top of the perched water layer is called the
perched groundwater table
53
A represents
Soil surface
54
B represents
Perched water layer
55
C represents
Compacted layer
56
D represents
ground water table
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Infiltration:
The movement of water from the soil surface into the soil
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Redistribution:
The subsequent movement of infiltrated water in the unsaturated zone of a soil.
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Redistribution involve:
1. Exfiltration 2. Capillary rise 3. Recharge 4. Interflow
60
exfiltration
evaporation from the upper layer of the soil
61
capillary rise
movement upward from the saturated zone to the unsaturated zone due to surface tension
62
recharge
movement of water from the unsaturated zone to the saturated zone
63
interflow
flow that moves downslope
64
Infiltration and redistribution depend critically on.......................................................
the material and hydraulic properties of soils
65
The groundwater can be sucked ..............................by the soil through ................................... that are called ..............................
upward very small pores that are called capillars .
66
The groundwater can be sucked upward by the soil through very small pores that are called capillars. This process is called ..........................
capillary rise
67
Soil texture: Coarse (sans) Capillary rise (in cm):
20 to 50 cm
68
Soil texture: medium Capillary rise(in cm):
50 to 80 cm
69
Soil texture: fine (clay) Capillary rise (in cm):
more than 80 cm up to several meters
70
Darcy’s Law states that the flow rate in the horizontal depends on
(1) the ability of the soil to “conduct” water; (2) the magnitude and direction of the slope, which is the gravitational potential energy gradient per unit weight of flowing water (soil water wants to flow downhill, towards lower gravitational potential energy), and (3) the magnitude and direction of the horizontal gradient in soil water pressure (if soil water pressure decreases in the x direction, the water wants to flow in that direction).
71
hydraulic conductivity
the vertical flow rate depends on the sum of the gravitational potential energy gradient per unit weight of water (dz/dz =1) and the vertical gradient in soil water pressure.
72
In a steady state (qz equals ...............)
zero
73
there is a balance between ................................. and ....................................
the effect of gravity an upward decrease in soil water pressure
74
the effect of gravity (which always wants to .......................................of ...................................., .towards...............)
pull the water “down the gradient” gravitational potential energy lower z
75
an upward decrease in soil water pressure (“................. the gradient” is in the .......................... z direction).
down positive
76
if the effect of gravity and an upward decrease in soil water pressure don't balance there is
a vertical water flow (up or down, depending on which term “wins”), the magnitude of which depends of the size of the imbalance and the value of the hydraulic conductivity coefficient.
77