1. Erosion is the process where soil particles are
b b b b b b b or
b and put in motion. (Unit 1): Ans- Dislodged; detached
b b b b b b bb b
2. Sedimentation is the process whereby detached particles are b b b b b b b
b elsewhere. (Unit 1): Ans- Deposited b b b bb
3. Sediment is solid b b or
particulate matterthat has been removed from its site of origin by
b b b b b b b b b b b
, ,or b
and deposited elsewhere. (Unit 1): Ans- Mineral; organic; water;wind; gravity
b b b b b bb b b b b
4. Accelerated erosion is a speeding up of erosion due to
b b b b b b b b b
activity.(Unit 1): Ans- Human
b b b bb
5. Major erosive forces are water and
b b b b b . (Unit 1): Wind
b b b
6. In some areas, more soil is lost from
b b b b b b b
erosion than fromwater erosion. (Unit 1): Ans- Wind
b b b b b b b bb
7. The effects of
b b erosion are usually more visible than b b b b b
b erosion. (Unit 1): Ans- Water; wind b b b bb b
8. The three categories of overland erosion are: (Unit 1): Ans- Sheet, rill, gully
b b b b b b b b b bb b b
9. b
erosion is the removal of a uniform layer of soil fromrain-
b b b b b b b b b b b
splash and storm water runoff. (Unit 1): Ans- Sheet
b b b b b b b bb
10. The
1b/b12
, of erosion defines the difference between rills andgullies. (Unit 1): Ans-
b b b b b b b b b b b
bbb Depth
11. The physical factors affecting erosion are: (Unit 1): Climate, vegetative cover,so
b b b b b b b b b b b
ils, slope.
b
12. Erosion and sedimentation may cause:
b b b b
-Loss of b bb b
- b damage to roads, buildings or bridges.
b b b b b
- b , resulting in reduction of fish
b b b b b bb
b , reduced
b or bb b
b capacity, and b costs to maintain b b .
- b loading. (Unit 1): - fertile topsoil
b b b b b
- Structural
- Deposition; spawning areas; channel; storm drain; increased; turbidity
b b b b b b b
- Pollutant
13. The climatic factors that strongly influence erosion and runoff are
b b b b b b b b b
b amount, , and
b
. (Unit1): Rainfall, frequency, intensity.
b b b b b
14. Soil properties influencing erodibility include: (Unit 1): Texture, structure,c
b b b b b b b b b
ohesion, natural drainage class
b b b
15. Texture refers to the b b b or of
b of soil particles in soil. (Unit 1): Size; combination of sizes
b b b b b b b b b b
2b/b12
, 16. Structure refers to the degree to which individual soil particles
b b b b b b b b b
b to each other. (Unit 1): Adhere
b b b b b
17. Slope , , and
b
b affect erodibility. (Unit 1): Steepness, length, and rough-
b b b b b b b
ness.
b
18. Sediment deposition occurs when soil-laden wind or water
b b b b b b b bb
b enough to allow the soil particles to settle out. (Unit 1): Slows
b b b b b b b b b b b
19. The , , and
b of the trans-
b b
ported particles influence the rate at which they settle out. (Unit 1): Size, shape,an
b b b b b b b b b b b b b b b
d density. b
20. Smaller, lighter particles such as b b b b
particles are easilytransported and are
b b b b b to settle out. (Unit 1): Clay-
b b b b b
sized;slow/difficult b
21. The Five Principles of Erosion and Sedimentation Control are:
b b b b b b b b
- the development to fit the natural site conditions
b b b b b b b
-Expose the b practical area for the b b b pos-
sible time
b b
-Apply bb b
prevention practices as first life ofdefense
b b b b b b
-Apply control practices to prevent off-site sedimenta-
b b b b b
tion
b
-Implement a thorough b b , , and
b
b program. (Unit 1): - Plan b b b b
- Smallest; shortest b
- Soil erosion b
3b/b12