QUIZ # 10- ABE-1-MODULE 6 Flashcards

1
Q

are those activities which maintain or enhance the productive capacity of the soil, water and vegetation in areas prone to degradation through
* prevention or reduction of soil erosion,
compaction, salinity;
* conservation or drainage of water and
* maintenance or improvement of soil fertility

A

Soil and water conservation (SWC)

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2
Q

are agronomic, vegetative, structural and management measures that control soil degradation and enhance productivity in the field

A

SWC technologies

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3
Q

are ways and means of support
that help to introduce, implement, adapt and apply SWC technologies in the field.

A

SWC approaches

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4
Q

are those farming operations and management strategies conducted
with the goal to control soil erosion by preventing or limiting soil particle detachment and transport in water or air (Baumhardt et al., 2014)

A

Soil conservation practices

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5
Q
  • the detachment of soil materials (gravel, sand, silt, and clay) and subsequent transport by an agent to an area of deposition
A

SOIL EROSION

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6
Q

comes from erodere, a Latin verb meaning “to gnaw”

___________ gnaws away at the earth like a dog at a bone

A

“Erosion”

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7
Q

most important agent of erosion in humid tropical areas

A

water

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8
Q

important agent in many parts of the world (in areas with arid climates)

A

wind

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9
Q

important agent during landslides, mudflows and bankfalls

A

gravity (mass wasting)

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10
Q

Over a short period, the process of erosion is almost ___________.

A

invisible

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11
Q

Erosion arises from two types of problem:

A

◼ Geological problem
◼ Social and economic problem

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12
Q

◼ weathering of surface layers of rock by water and biosphere
◼ Normal geologic erosion - 0.1 t/ha/yr

A

◼ Geological problem

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13
Q

◼ Urbanization and population growth
◼ Accelerated erosion - 10 to 700 t/ha/yr

A

◼ Social and economic problem

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14
Q

Erosion events are very _____________.

A

irregular

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15
Q

Factors affecting Soil Erosion

A
  1. Climate ( rainfall, wind )
  2. Soil erodibility
    ◼ Soil texture
    ◼ Soil structure
  3. Vegetation or plant cover
  4. Relief (Slope)
  5. Man’s activities
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16
Q

Soil erosion by water depends on:

A

(1) the slope
(2) the soil structure
(3) the volume or rate of flow of surface
runoff water

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17
Q

steep, sloping fields are more exposed to erosion;

A

slope:

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18
Q

_____ soils are more sensitive to erosion

A

light

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19
Q

_________ or ___________ flows induce more erosion

A

larger or rapid

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20
Q

usually heaviest during the early part
of irrigation, especially when irrigating on slopes.

A

Erosion

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21
Q

The dry surface soil, sometimes loosened by cultivation, is easily removed by flowing water. After the first irrigation, the soil is moist
and settles down, so erosion is _____________.

A

reduced

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22
Q

__________ areas are more sensitive to erosion, especially in their early stages.

A

Newly irrigated

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23
Q

Forms of Erosion by Water

A

◼ Raindrop splash erosion
◼ Sheet erosion
◼ Rill Erosion
◼ Gully erosion
◼ Stream channel erosion

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24
Q

◼ The first step in the erosion
process begins as raindrops
impact the soil surface.
◼ Raindrops typically fall with a
velocity of 20-30 feet per second.
The energy of these impacts are
sufficient to displace soil particles
as high as two feet vertically.
◼ The impact of a rainfall on a bare
soil can compact the upper layer of
soil, creating a hard crust that
inhibits plant establishment.

A

Raindrop splash erosion

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25
is the even removal of a very thin layer or "sheet" of topsoil from sloping land. occurs as runoff travels over disturbed ground, picking up and transporting particles dislodged by splash erosion. The process of _______________ is uniform, gradual and difficult to detect until it develops into rill erosion.
Sheet erosion
26
The potential for _____________ is dependent on the soil type, velocity, and quantity of flow over the surface. Long slopes, steep slopes, and slopes that carry higher volumes of runoff are more susceptible to _______________
sheet erosion
27
◼ only a thin layer of topsoil; or the subsoil is partly exposed; sometimes even parent rock is exposed ◼ quite large amounts of coarse sand, gravel and pebbles in the arable layer, the finer material has been removed ◼ exposure of the roots ◼ deposit of eroded material at the foot of the slope
Sheet erosion
28
occurs as runoff begins to form small concentrated channels. As __________begins, erosion rates increase dramatically due to the resulting concentrated higher velocity flows.
rill erosion
29
◼ Construction sites that show signs of ________________ need to be re-evaluated and additional erosion control techniques employed. Rilling can be repaired by tilling and should be repaired as soon as possible in order to prevent gullies from forming.
rill erosion
30
is the removal of soil by a concentrated water flow, large enough to form channels or gullies; results from water moving in rills, which concentrate to form larger channels (when rill erosion can no longer be must typically be repaired utilizing earthmoving equipment. _______________ can be prevented by quickly repairing rill erosion and addressing the cause
Gully erosion
31
The signs of _____________ on an irrigated field are: ◼ irregular changes in the shape and length of the furrows ◼ accumulation of eroded material at the bottom of the furrows ◼ exposure of plant roots
gully erosion
32
-consists of both stream bed and stream bank erosion. ◼ Stream bed erosion occurs as flows cut into the bottom of the channel, making it deeper and reaches a stable slope. - The resulting slope is dependent on the channel materials, and flow properties.
Stream channel erosion
33
◼ Stream bank erosion can also occur as soft materials are eroded from the stream bank or at bends in the channel. This type of stream bank erosion results in meandering waterways. ◼ One significant cause of both steam bed and stream bank erosion is due to the increased frequency and duration of runoff events that are a result of urban development.
Stream channel erosion
34
Mechanics of Soil Erosion Process
1. Soil detachment by rain fall 2. Entrainment of Sediment 3. Sediment Deposition
35
process by which raindrops splash sediment from the soil surface into the water of overland flow or runoff water.
Soil detachment by rain fall
36
the process whereby overland flow picks up sediments from the soil surface, whether in rills, between rills and in sheet flow.
Entrainment of Sediment
37
the process which is the result of sediment settling out under the action of gravity. The rate depends on sediment size, being very rapid for coarse (sand) and very slow for fine ( silts and clay) particles, thus the silts and clays are transported and deposited farther away from where they
3. Sediment Deposition
38
occurs when eroded material that is being transported by water, settles out of the water column onto the surface, as the water flow slows
SEDIMENTATION
39
◼ Kinetic energy ◼ Slope of the land ◼ Cover ◼ Resistance of the soil to detachment and transport based on chemical and physical properties of soil ◼ Conservation factors
IMPORTANT FACTORS TO SOIL EROSION
40
◼ predicts the long term average annual rate of erosion on a field slope based on rainfall pattern, soil type, topography, crop system and management practices A = R x K x LS x C x P Threshold level of soil loss - 8-12 tons/ha/yr - 4 tons/ha/yr (thin topsoil) Limitations: can be used for splash erosion only cannot be used in other country unless you modify R
Universal Soil Loss Equation (USLE)
41
was developed using the English system of units. Its equivalent form in the metric unit system is presented by Kent Mitchell and Bubenzer (1981) as E = 0.224 R K L S C P where: E = sheet erosion loss in kg/m2 R = rainfall erosivity factor K = soil erodibility factor L = slope length factor S = slope gradient factor C = cropping management factor P = erosion control practice/conservation factor
The UNIVERSAL SOIL LOSS EQUATION
42
has gained wide acceptance in the United States. It has recently been adapted by soil conservationists in many other countries.
The UNIVERSAL SOIL LOSS EQUATION
43
was developed from agricultural plots with certain ranges of variations in soil, climatological and slope conditions.
The UNIVERSAL SOIL LOSS EQUATION
44
Very simple to use, however, the validity of the _______ depends on how close the conditions to which it is being applied at are to the range of conditions from which it was developed. It is best suited to small areas with low to moderately intense rainfall.
The UNIVERSAL SOIL LOSS EQUATION
45
◼ 72.6 ft long ◼ 6 ft wide ◼ 9% slope ◼ Bare ◼ plowed up and down the slope ◼ no conservation measure
STANDARD EROSION PLOTS
46
The control of soil erosion and sedimentation needs to be based on the correct identification of source areas of sediment, a knowledge of the processes by which water and sediment are moved over the land surface, and an understanding of how these processes are affected by the physical environment and socio-economic factors.
Erosion Control Principles
47
◼ use land according to its capability ◼ protect the soil surface with some form of cover ◼ control runoff before it develops into an erosive force
Three main principles
48
◼ The method used to prevent erosion from raindrop splash and sheet erosion is _____________.
stabilization
49
-temporary and permanent vegetation -mulching -compost blankets -erosion control products that absorb the impact of raindrops
Examples of stabilizing techniques
50
Under erosion control practices 1. Mulching 2. Cover cropping 3. Strip-cropping 4. Crop Rotation 5. Relay Cropping 6. High Density Planting 7. Multiple Cropping 8. Alley Cropping (Sloping Agricultural Land Technology ) 9. Agroforestry
Agronomic Measures
51
Under erosion control practices 1. Contouring 2. Minimum Tillage 3. Strip of Zone Tillage (Precision Tillage) 4. Mulch Tillage 5. Subsoiling 6. Ridge-tying
Soil Management (Conservation Tillage)
52
Soil Management (Conservation Tillage) 1. Terracing bench Zingg or conservation bench terraces broad-based 2. Grassed Waterways 3. Structures (Farm ponds and check dams) 4. Toward Soil Conservation – oriented Farming Systems
Mechanical Methods
53
is an earth embankment or a ridge and channel constructed across the slope at an acceptable grade.
terrace
54
1. reduce sheet and rill erosion 2. prevent gully formation 3. moisture conservation 4. moderate flood or overland flows
Functions of a terrace
55
TYPES OF A TERRACE
-BENCH -ZINGG -broad-based terrace
56
e.g. Banaue Rice Terraces ➢ used for maximum moisture conservation ➢ used where land is at a premium ➢ conventional
BENCH
57
e.g. Banaue Rice Terraces ➢ used for maximum moisture conservation ➢ used where land is at a premium ➢ conventional
BENCH
58
◼ easier to farm than conventional ◼ used for maximum soil and water conservation
ZINGG
59
may either be graded or level. ◼ grade – fall in channel ◼ slope – fall in natural land surface
broad-based terrace
60
◼ Terrace location ◼ Factors that influence terrace location (e.g. land slope, soil condition) Criteria for terrace location ◼ Minimum maintenance ◼ Ease of farming ◼ Erosion control
Planning the terrace system
61
1. The allowable soil loss should be first estimated using relevant information on soil depth, fertility, land value, siltation damage downstream, etc. 2. In the absence of soil loss information, the spacing may also be estimated from appropriate erosion equations such as the universal soil loss equation. 3. No hard and fast rules can be laid down to follow in terrace layout because every field has its own individual problems. 4. Good judgment and consideration of all factors are required to obtain the best possible layout terraces on each field.
Terrace Design