MODULE 1 Flashcards

1
Q

Irrigation – application of water into the soil; in some areas,
irrigation means to supplement rainfall and serves to
increase production

A

Irrigation –

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2
Q

– removal of excess water within or on the soil; it can be

natural or artificial

A

Drainage

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3
Q

Advantages of Irrigation and Drainage:

A

-increase cropping efficiency
-increase crop productivity and yield
-increase cropping intensity

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4
Q

Agriculture consumes ——-of our total water consumption, and the
majority of this consumption is accounted for by irrigation.
Moreover, roughly half of all harvested rice area and ——-of the
total rice output are irrigated rice.

A

82% , 70%

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5
Q

the largest irrigation scheme,
servicing about 44 % of the total irrigated land

A

National Irrigation System (NIS) -

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6
Q
  • relative proportion
    of variously sized
    groups of mineral
    particles in a
    particular soil or
    horizon
A

Soil Texture

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7
Q

– represents the soil which is made up of air, water and
solids.

A

Soil System

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8
Q

TOTAL VOLUME

A

VT = Va + Vw + Vs
Vv = Va + Vw

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9
Q

determines the amount of pore spaces within the soil
- amount of water a soil can hold in a saturated condition

A

c. Porosity (n)

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10
Q
  • the ratio of the volume of
    voids in a soil to volume of
    solids
A

Void Ratio (e)

e = Vv / Vs = n / 1-n

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11
Q

Degree of Saturation (DOS)

A

DOS =( Vw-Vv) x 100

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12
Q

lateral movement of water in the ground surface

A

surface runoff -

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13
Q

lateral movement of water below water table

A

seepage -

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14
Q

flow of water from the ground surface into the soil

A

infiltration -

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15
Q

further downward movement of water into the soil

A

percolation -

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16
Q

3 types of Moisture Content Measurement

A

Direct Method
b. Feel and Appearance
c. Bouyoucos Method
d. Tensiometers

17
Q
  • uses the electrical properties of the soil to determine its
    moisture content
A

. Bouyoucos Method

18
Q

Soil water content and matric potential are not uniquely
related and depend on the path of saturation or desaturation
- Difference in mc readings even same tensiometer readings

A

Hysteresis

19
Q
  • amount of water the soil profile will hold when all its pore
    spaces are filled up
A

Saturation Point

20
Q
  • soil is allowed to drain 2-3 days
  • amount of water the soil profile will hold against the soil
    moisture tension of 1/3 bar
A

Field Capacity

21
Q
  • amount of water the soil profile will hold against the soil
    moisture tension of 15 bar
A

Permanent Wilting Point

22
Q
  • amount of water the soil profile will hold against the soil
    moisture tension of 10,000 bar
A

Hygroscopic Point

23
Q

causes the dissimilar particles and/or surfaces to

cling to one another

A

Adhesive force -

24
Q

similar or identical particles/ surfaces

to cling to one another

A

Cohesive force -

25
Q

due to the effect of gravity

A

Gravitational force -

26
Q

caused by salt or ion concentration differences or
gradients

A

Osmotic forces -

27
Q

water on the soil grains that is not capable
of significant movement by the action of gravity or capillary
forces

A

Hygroscopic water -

28
Q

*water that exists in the pore spaces of the soil
and is retained against the force of gravity in a soil that permits
unobstructed drainage

A

Capillary water -

29
Q

water that will readily move out of the soil
if favorable drainage is provided

A
  • Gravitational water -
30
Q

*held too tightly by capillary forces and is
generally not accessible to plant roots

A

Unavailable water -

31
Q

difference between gravitational and
unavailable water

A
  • Available water -
32
Q

drains quickly from the root zone under
normal drainage conditions

A
  • Gravitational water -
33
Q

drains quickly from the root zone under
normal drainage conditions

A
  • Gravitational water -